-3.
GC
856
.0735
of
OCEANOGRAPHY
Progress Report
The Development of Methods for Studying
Physical and Biological Processes in the
Nearshore Zone on the Pacific Coast of the
United States.
Reference 73-3
March 1973
OREGON STATE UNIVERSITY
THE DEVELOPMENT OF METHODS FOR STUDYING PHYSICAL AND
BIOLOGICAL PROCESSES IN THE NEARSHORE ZONE
ON THE PACIFIC COAST OF THE UNITED STATES
Principal Investigator:
Co-Principal Investigator:
Robert L. Holton
William P. Elliott
L School of Oceanography,
Oregon State University,
Corvallis, Oregon
97331
PROGRESS REPORT
1 June 1972 through 28 February 1973
Submitted to
Eugene Water and Electric Board,
Portland general Electric
Pacific Power & Light
Reference 73 - 3
March 1973
STAFF
Robert L. Holton, Ph.D.
Principal Investigator
William
Co-Principal Investigator
P. Elliott, Ph.D.
Janice Crawford, B.S.
Kenneth Johnson, B.S.
Carolyn Mullikin, B.S.
Walter Pearson, M.S.
Graduate Students
Linda Smith, B.S.
Leo Kowalski, Boat Operator
In addition to the above the following assisted at various times in
the conduct of the field work and data analysis but did not receive financial
support from this project. Their assistance is gratefully acknowledged here.
Norman Farrow
William Gilbert
Vernon Johnson
Donald Keene
Jan Naidu
PROGRESS REPORT
Introduction
The following progress report presents a summary of the work conducted
through January of 1973 as specified in our proposal, "The Development of
Methods for Studying Physical and Biological Processes in the Nearshore
Zone on the Pacific Coast of the United States,"
supported by the Eugene
Water and Electric Board, Portland General Electric Company and the Pacific
Power and Light Company.
Although we started this program in the early summer of 1978 without
adequate lead time to order equipment and hire personnel we have been able
to make a meaningful start at achieving the goal of developing study
methods for the nearshore zone.
However, the progress is spotty.
In the
areas of sampling fish and benthic organisms a limitation on boats available,
equipment on hand, and number of personnel hired resulted in little effort
being expended in this area.
The studies
of surface currents and of phytoplankton
and zooplankton
distribution have been initiated and significant progress has been made.
In these cases the studies have been adequate to enable us to do a more
effective job of planning for future needs in these study areas. We
anticipate having significant programs in all areas during the 1973 working
season.
The logistic problem was difficult during the first year's operation.
We plan to reduce this problem greatly during 1973 by shifting our operations to Newport and
basing most of our personnel there for the summer.
This will increase our efficiency by allowing us to utilize both the
existing weather and the time of our personnel more effectively.
We feel that in general the only way to develop adequate methods is
to take a particular method, use it to gather data under field conditions,
and evaluate the adequacy of the method by a careful examination of the
data collected.
This approach is reflected in the following discussion
of the individual subprojects.
2
Working Vessels
The experience that we had during the 1972 working season indicates
that the Pacific City-style dory is a satisfactory vessel for working in
this zone.
It allows us to come through the surf and to the shore during
many of the working days during the summer.
It does not, however, allow
us this ability on days when the swell is running high.
It also is capable
of handling the various types of sampling rigs that we need for this pro-
gram.
Although the dory itself is capable of doing the type of work that
we desire, we find that the dory as equipped last summer did not give us
as full and versatile a range of operation as we desire. In particular,
we find two areas.in the dory operation that were less than completely
satisfactory. The use of a conventional outboard engine, in a well, necessitates the use of an extra man for handling the dory as we are coming
through the surf to the beach. This extra man is necessary to lift the
motor to keep it from hitting on the sand as we are coming to the beach.
This type of motor also leaves us without power when we are inside the
surf zone and this requires extra manpower to hold the dory in place. The
second area of deficiency was the lack of navigational equipment. This
proved to be a safety problem on days when we were caught in a fog.
We
also find that we were unable to locate and replicate a station with any
degree of accuracy without the help of a triangulation from shore.
To remedy this situation and to reduce the man power requirement
imposed by such triangulation we feel that a radar and fathometer system
will aid us greatly in making the best use of the dory. We will also propose the use of a jet powered dory to increase the efficiency of our operation.
Although we did not have any large effort directed toward large animal
sampling last summer, we did do enough work with the dory in the surf to deter-
mine that it would be
set a beach seine with the dory and then
move the dory out of the way and pull the beach seine from the shore. We
will use the dory for this type of operation during the coming summer. We
will also use the dory to pull conventional otter trawls and bottom sampling
devices through the surf zone under favorable conditions.
possible to
3
Phytoplankton
The data presented in Appendix I are representative of the phytoplankton
data that were collected during the 1972 period.
The procedure for the
collection of these data is as follows: An NIO water sampling bottle
is
used for collection of one liter water samples.
The use of this bottle
allows sampling
to occur at any depth from the surface to the bottom within
the nearshore zone.
The bottle is an adaption of the Nansen type reversing
water sampler, which reverses and locks in place at
a particular depth to
take the desired sample.
The water sample so obtained is then processed in the following
way.
The water from the NIO bottle is placed in a one liter plastic bottle and
the one liter plastic bottle is submerged in a water bath
on the boat to
maintain it at its correct temperature.
The water bath is also designed
to reproduce the approximate light intensity that the phytoplankton
would
be encountering at their depth of collection. This light intensity is
reduced for lower samples by the successive addition
of screens to the top
of the water sampling container.
The phytoplankton samples are then transferred to a shore-based station for filtering.
Only six to eight samples
are collected at one time before the trip to the shore-based facility.
The
samples typically spend about one hour between the time
of collection and
the time of filtration.
On the shore the water samples are processed in
a tent, where we are
able to filter them through a specially developed one liter filtering
apparatus using a 0.8 micron filter.
This filter will remove essentially
all of the larger diatoms, which appear to make
up the majority of the
plankton in this area.
The filtering device is a pressure filter and in
the work last summer nitrogen gas was used to develop
the pressure to push
the liter of material through the filter.
The filter, thus attained, is
then frozen using dry ice in the field and retained in
this frozen condition
until time for analysis.
The processing of the frozen filters in the laboratory is started by
grinding them in a mixer in a solution of 90% double distilled acetone.
The solution is then placed in a refrigerated centrifuge and spun down
for 20 minutes.
During this processing, care is taken to keep the samples
constantly refrigerated and in the dark.
This is necessary since both
4
light and heat will tend to alter the pigments.
The supernatant liquid
is then read in a spectrophotoneter at six different wave lengths.
This
raw data is then analyzed by a computer program to determine the pigment
values as presented in Appendix I.
The program calculates chlorophyll
values based on two different methods that have been used by other investi-
gators.
The values given in Appendix I after the analysis are values for the
chlorophyll content of the particular sample.
Although, the chlorophyll
content is not a direct measure of primary production in a marine ecosystem,
it is in fact, a measure of the potential production for a system and is
widely used in this way.
The advantage to using this type of measurement
lies in the fact that one is able to get a great number of measurements in
a relatively short period of time.
If a person is measuring the actual
production by the various light bottle-dark bottle techniques it will be
much more difficult to obtain a survey of a broad area over a short period
of time, since each sample requires a considerable incubation time and requires a longer time for analysis than the samples measured in the way we
are measuring.
Therefore, we propose to test the validity of this method as a survey
method for primary production in a given region and to validate this method
against measurements of primary productivity by a carbon-14 method during
future years.
The data that we have at this time illustrate some difficulties encountered with this type of measurement.
The greatest difficulty at this
stage is our inability to obtain replicate samples that are showing a
consistent value.
At this time we blame this on the fact that we have not
had enough development time to standardize our methods to allow us to
operate more accurately in this area.
Therefore, a first effort in the
future year's work will be to use this method and to develop greater precision in its use so that we can get the variations between replicate
samples taken at the same time and the same place down to a much lower
level.
Since we did not make measurements of productivity, we will plan to
develop the techniques for making such measurements during the coming work
period.
We will also develop counting abilities to determine population
sizes for various major species during this season as well.
5
Zooplankton Sampling
The data collected during the past working year on zooplankton are pre-
sented in Appendix II.
method.
All of these data were collected by the following
A Clark-Bumpus zooplankton sampling device with a five inch dia-
meter mouth and a number 6 mesh net was used to collect all samples.
This sampler has a rotor on the front that allows water to turn the
blades of a meter.
This meter has been calibrated in a known environment
(such as a swimming pool) and with this calibration it allows calculation
of the number
device.
of cubic meters of water that flowed through your sampling
Therefore, it is possible to count the
animals and knowing the
number of cubic meters that have passed through the device, it is then pos-
sible to determine
the number of organisms in each cubic meter of water.
A sample thus collected is diluted down to permit taking 3-4 aliquots
which, when combined, comprise a subsample containing 400-500 individuals.
sample is then carefully counted and identified
sex, and stage in the life cycle. The raw data so collected
This defined
by species,
are then pro-
means of a computer program to give the results as demonstrated
in Appendix II. The use of this computer program saves a great deal of
cessed by
time in the calculation
of densities of organisms in this nearshore zone.
Our studies for the last summer have allowed us to develop the
techniques for collecting and processing this type of data.
necessary
We have learned that the dory is in fact an excellent platform for the
collection of zooplankton data.
The dory used last summer was limited in
no power winch for the precise and rapid lowering and recovery
that it had
of the zooplankton net.
Future work in this area will be greatly facili-
tated by the use of a dory that has the power winch available for these
studies.
Although this area of the coastal ecosystem has not been previously
studied or
sampled, we have confirmed the species distribution with respect
distance
to time and
studies both
indicate the
are larger
to shore could have been predicted from previous
within the Yaquina Bay and from farther offshore.
occurrence of sampling errors on the replicate
than we are
willing to accept at this time.
The data
samples that
Therefore, it will
6
be necessary for us to devote a great deal of attention to methods of
reducing error between replicate samoles and secondly to providing reliable
estimates of the amount of error that is inherent in this sampling method.
Only by having information that indicates the size of the expected error
will we be able to set confidence limits on future samples that are associated with a particular location.
One component of the observed variability is undoubtedly the result
of patchiness in distribution of the organisms.
Future efforts must include
a sizable effort to determine the nature of such patchiness.
Sampling
methods must then be developed which will take this patchiness into account
and which will reduce the replicate sample variation due to patchiness.
This effort will have a high priority for the 1973 working year.
A summary of the data showed that we noted a total of 50 different
species in the plankton samples during this study's period.
The number
of species and the species of maximum abundance varied both with distance
from shore and with the time of sampling.
Dominant in this analysis were
Acartia clausi, Acatia lo ngiremis, various species of Pseudocalanus, Podon
leuckarti, and various barnacle life stages.
Acartia clausi was most abundant near shore and increased in numbers
from July to mid-August and then decreased to mid-September in our sampling.
Acartia longiremis was most abundant farther offshore with a rather sizable
fluctuation in abundance during the time of the study.
Pseudocalanus
species were consistently of a higher abundance near shore
and relatively
stable at all near shore stations with a slight decrease in August.
Podon
and the barnacle stages became abundant at erratic intervals and especially
abundant in September. They are found in all stations from August on and
were in the largest numbers on the days of the roughest seas.
Studies of zooplankton abundance with depth, indicated that we were
finding a maximum in abundance and diversity of species about 15 meters
in depth.
Therefore, this depth was used as a standard depth for towing
our sampling device for the remainder of the sampling period.
There is
some variation with the abundance of individual species with depth. This
variation which has been noted requires further evaluation.
This type of
7
information will, of course, become extremely important in the planning for
any possible cooling water intake in the marine environment.
The specific
design of such an intake should take into account the death distribution
of all of the various nearshore marine species to trv to select an intake
depth that minimizes the pumping of such organisms through the industrial
operation of interest.
The distribution of species and abundance of species in the direction
parallel
as yet
to the shore was noted.
Since the meaning of this variation is
undetermined, it obviously must be studied in greater detail.
variation
could again
This
become important in determining our location of
cooling water intake designs.
We will make additional studies to try to
tie down the differences that have been noted.
For example, the differences
could be related to towing direction in terms of towing the sampling net
or they might be due to varying sea conditions and the influence of the
headlands on the organism
in particular areas.
Therefore, we will repli-
cate our efforts and try to determine the importance of towing pattern and
headlands under varying wind conditions with the relative abundance of
samples attained
at different locations parallel to the beach.
Additional efforts will be devoted to checking the inherent capabilities of the sampling instruments in producing accurate replicate samples as
opposed to short term variations in the population which give the appearance
of nonuniform sampling techniques.
Several devices will be built and tested
during the coming summer to try to reduce the variation we see in this type
of program.
A good deal of further effort is required along these lines to
enable us to
plan intelligently future sampling programs in this area.
Certain other physical problems happened that reduced our sampling
efficiency; for example, on four sampling dates we found a great deal of
difficulty in obtaining reliable samples of zooplankton due to a clogging
of the net with either phytoplankton or with jelly fish.
As a result of
these difficulties we plan to use a sampling screen which will run in front
of the zooplankton sampler and allow us to screen out the jelly fish that
were clogging
the Clark-Bumpus net.
The problem with phytoplankton is of
course not so easily solved and it appears to be a problem we are forced
to live with.
8
In conjunction with the zooplankton sampling program we took data on
various physical parameters at each sampling date.
We determined the
salinity at the surface and at the bottom in all of our samples.
We con-
ducted the salinity sampling with the NIO water sampling bottle taking a
small aliquot from the bottle in a salinity sampling jar and reading the
value in the laboratory on an inductive salinometer.
These salinity data
are presented in Appendix II.
We also measured the transparency of the water with a secchi disk
reading, measuring the visibility by determining when the disk was no
longer visible from the surface.
This turbidity or visibility measurement
is also tabulated in Appendix II.
We also obtained data on the color of the water by the use of the
Forel scale.
This scale is used to compare the color of a sample of water
with a series of color comparitors that are provided as a part of the reading device.
In general a yellow green to yellowish color in the water is
indicative of a high level of plankton and hence probably a high level of
productivity, while a blueish color in the water is an indication of the
absence of particulate matter in the water and probably ,a low productivity
in that region.
Again we have provided the Forel scale readings in Appendix
II.
The final physical parameter that was measured was the temperature of
the water at the surface and the bottom.
The surface temperature was
obtained from a bucket thermometer hung overboard at approximately one
foot depth.
The bottom temperature was read from a reversing thermometer
attached to the NIO water sampling bottle.
Again these temperature measure-
ments are provided in Appendix II.
At this time we have not had enough time and experience with the
measurement of the physical parameters to ascertain fully their value in
this type of program.
Therefore, we proposed to continue making this
series of measurements which are not expensive or time consuming and
developing means for determining the meaning of these physical parameters
in terms of the samples of zooplankton that we obtain in a given region.
It will be especially easy to obtain these samples if we are able to equip
a dory with a hydraulic system that includes two winches.
One winch would
9
be used to handle the zooplankton
would be used to obtain water for
sampling itself
and the second winch
the measurement for the
various physical
parameters.
Behavioral Studies
During the summer of
1972 we attempted to dive several times to deter-
mine the feasibility of making behavioral observations of various marine
organisms in this area. Our attempt was to use scuba gear and to record
visually some of the behavior parameters of importance. We found that this
does,not appear to be a practical working mode at this time. Our difficulties were twofold. In many of the nearshore areas we found that it was
impossible to work safely during the time that the ocean was at all rough.
The surge produced by the swell could throw a diver into a rock or otherwise
injure him while working in this
zone.
However, a much more difficult problem was visibility.
estimate that you would be able to
studies something less than 10% of
At all other times the
It is our
behavioral
the time during the better summer months.
see adequately to conduct
to be less than 20 feet and makes
behavioral studies in this environ-
visibility appears
to conduct any direct
ment. Since we cannot plan a program based only on observations that can
be made 10% of the time, we feel that we must explore other modes of operait very difficult
tion or set up special laboratory studies to conduct the needed behavioral
studies that are relevant in the nearshore zone. We are continuing to
search for a protected area that provides the special conditions necessary
for the conduct of such field studies. However, the prospects do not appear
to be particularly encouraging at this time.
Large Animal Sampling
Due to the lateness of starting our work in the summer of 1972 and due
to the difficulty in obtaining equipment for such sampling we did not get
started with this work during that year. We have used the time since then
to obtain equipment and to design additional equipment for these specific
studies. We also hope to have a dory that will be equipped with a winch
large enough to handle this equipment for our studies.
10
We did have one day of experience in handling a beach seine and in using
a dory to set the seine outside of the surf zone.
workable.
The method appears to be
That is, the dory is very successful in coming ashore, leaving
a line on shore, going out and setting a seine parallel to the beach, and
returning to shore with the other line.
Our method of operation would be
to then have the dory leave the area to minimize disturbance of the fish in
the area and then at a time after the dory has left we would pull the seine
from the shore.
However, we also learned that pulling a beach seine from the shore is
in fact a massive undertaking.
by hand.
It will be impossible to pull such a seine
It will be necessary to have some type of a shore based winch
that will allow us to properly fish a seine in this area.
We now have also
obtained the necessary permits from the Oregon Fish Commission that will
enable us to sample in this area with any type of sampling device, including
a gill net, if we desire.
We feel that the gill net will be necessary to
obtain samples of some of the faster moving species in this area.
Our otter
trawls and mid water trawls will be too slow to capture these animals and
we feel it is doubtful if we will be able to capture such species as salmon
in a beach seine.
We will also consider the feasibility of sampling organ-
isms such as salmon by a typical sport fishing rig.
At least we will study
the statistics necessary to determine how often we would have to fish in
region to obtain the data about the catch per hour effort.
a
If the feasibility
studies prove good we will plan to incorporate such an experimental fishing
program into our 1974 program.
We will plan to obtain physical data at the same time we are making our
large animal samples.
We will be particularly interested in temperature and
salinity measurements, the stage of the tide, and the time of the day, as
well as the turbidity.
fish with these factors.
It will be important to correlate our catches of
A major emphasis will be placed upon the large
animal sampling program during the summer of 1973 and at that time we will
be able to assess our position in this field.
11
Benthic Sampling
We will begin a program to study both the infauna and the epifauna in
this nearshore region.
We will use crab pots to study the epifauna and will
modify the crab pot to a finer mesh size than that which is used by the
commercial fishermen.
We will also use various bottom dredges to study
and obtain samples of the infauna.
We realize the difficulties in these
studies but we also realize that they must be done.
We will attempt to
pull a dredge through the surf zone to obtain samples in that area and
we will also use
the dredge farther offshore to examine the benthic popu-
lations in that region.
We again can make little comment about our success
in that area, since our efforts will not start until the summer of 1973.
Introduction to Current Studies
The problem of nearshore circulation is complicated by the number of
forces that can cause water movement in this region.
Wind, tides, wave
transport and offshore current systems can all produce local currents and
obviously do not all need to be moving in the same direction and can change
quickly with time.
The bulk of the current study effort to date has been
concerned with developing techniques to measure the surface water movement
and to determine the causes of these movements.
Working as close to shore as we do means that large vessels cannot be
used and also that there are times when the sea is too rough for the small
boats to operate safely. Therefore, techniques for observing from shore or
light aircraft are most desirable and we have spent some time considering
these possibilities.
The standard method of measuring currents employs current meters of
various types.
We did not spend time in our observation period with them
partly because the technology of current meters is
well known and we wished
to experiment with other - less expensive - methods.
This is not to say
we feel they would not be useful or even necessary in a final survey, but
one should have a fair idea of where they should be placed before deploying
a network. That idea can be gained most inexpensively by employing free
floating objects whose path can be followed.
Thus we experimented with a
variety of devices designed to give an overall view of the surface current
patterns.
12
Drift Bottles and Bags
A drift bottle is simply a transparent bottle, in our case beverage
bottles of 10-12 oz capacity, with a card inside which is numbered so the
position and time of release can be recorded.
The bottle is weighted with
sand so it will float properly with a minimum area exposed to the wind and
capped in the conventional manner.
The bottles were released from our vessel
at various distance from shore but all were released from within two miles
of the beach.
The card inside instructs the finder to return part of the
card to the School after noting the time and place of recovery on the card.
Obviously we cannot tell the trajectory of the bottle, only the starting and
end points but the general movement of the water can be determined and we
can gain some idea of the speed of movement if we can recover the bottles
promptly.
To get a good idea of the time elapsed between drop and recovery on
shore we searched the beaches ourselves for the bottles so we did not have
to rely on returns from the public.
into
1/8 mile zones so
We divided Moolack and Beverly Beaches
the recovery positions could be easily recorded.
If
the bottles come ashore at other beaches along the coast we had to rely on
the public.
Besides giving us an estimate
of the time it takes surface
water to appear on the shore immediately landward of the drop we can also
determine whether the surface flow is predominantly
onshore, along
shore or
offshore and whether there is a separation of these flows by distance offshore.
We also experimented with small plastic sandwich bags partly filled with
water to give some weight and with only an identifying number in them.
This
precludes returns from the public but is a less expensive way of operating.
However, we found, from simultaneous drops of bottles and bags, that the
bags came ashore slightly sooner than the bottles.
This fact, coupled with observations of this behavior from the boat
makes us feel that they are more affected by the wind directly and, therefore,
a less satisfactory tracer of the surface water movement.
Also the lack of
public returns prevents us from learning about movements away from our immediate area.
Therefore, we did not use these much after the middle of August.
13
I summarizes the returns from all our drops except those made in
January 1973. The returns from which are not yet complete.
Table
Date (1972)
Number Dropped
% returned
10 June
240
7
26 June
108
84
6 July
120
76
19 July
110
63
9 August
120
70
17 August
24
50
18 August
24
58
7 October
48
41
Exclusive of the drop of 10 June this gives an overall recovery rate
of 69%, a very high return rate.
The 10 June drops were made further off-
shore than usual and with an east (offshore) wind.
Some preliminary inter-
pretations of these results will be given in the Result section. This data
is found in Appendix III.
Drogues Followed From Shore
To gain a better idea of the actual water trajectories we designed some
surface drogues (devices designed to follow the currents and whose position
can be determined at any time by one of several methods).
These consisted
of circular plywood disks, painted orange, with crossed vanes beneath them
to be pushed by the water.
sizes and vane
depths and found 3-foot diameter surfaces gave adequate visibility and 6-inch
deep vanes were fine.
We experimented with several
We launched a number with differing vane depths from
the same location on one day to determine if we could detect any difference
in movement due to current changes with depth.
Although the drogues did not
maintain their original orientation we concluded this was due to diffusion
and did not indicate any noticeable effect of variable currents.
We determined positions of these drogues by observing them with surveyors
instruments from the shore.
We found the standard meteorological theodolite
(an instrument like a transit that gives elevation
angles as well as azimuth)
insufficiently accurate since it can be read to only 0.1° of arc.
We used
a surveyors theodolite, loaned by the Civil Engineering Dept., which could
be read easily to 20" of arc and this proved sufficient. We were able to
14
obtain
readings as fast as every one minute if the speed of the drogue
required it and could follow then for several hours at this rate although
the observer began to be fatigued about then.
We generally tried to recover the drogues from the sea before they
became entrapped in the surf and came ashore.
On several occasions we let
them come ashore and tried to follow them but they tumble in the surf and
their motion there is no longer representative of the water motion so little
is gained by this.
In the Results section we will discuss some of the implications of
these measurements together with the drift bottle data.
As a technique for
determining the nearshore currents in detail the method seems admirable.
is inexpensive and gives quite good detail.
It
We have developed a computer
program which gives the velocities each minute and can smooth out some of
the irregularities.
The program can be expanded to give statistical details
of the motion if this should appear worthwhile later.
Furthermore, the
technique can be adapted to determine other details of the flow using multiple drogues whose positions are not recorded so often.
in Appendix IV.
This data is found
Die Markers Dropped From Aircraft
Because weather conditions sometimes prohibit small boat operation,
particularly in winter, we experimented with dropping die markers into the
ocean from a small aircraft and following them from the airplane.
We did
this in a particularly severe weather condition - 40 knot winds from the
south and rain.
Nevertheless we were able to drop two markers which could
be followed for over an hour from the plane.
Deriving quantitative data
from this operation is more difficult because aerial photography, while
possible, could give only the relative position of the markers since it
was not possible to keep a known point always in the picture.
However if
some object that could be jettesoned from the plane that also could be
tracked from shore could be developed we could be much more independent of
the weather.
We did try following die markers from the shore but this was
not successful:
they cannot be seen at the angles even from the bluffs.
15
Drogue Study From Ship
From 2-5 Jan. 1973 we were able to use R/V YAQUINA to study the nearshore circulation by using regular ship launched drogues (The ship was
available for this purpose because another study conducted by WPE for NSF
could be combined with drogue studies:
particular project.)
therefore there was no cost to this
This method consists of launching a drogue consisting
of a float carrying a mast with a radar reflector with a parachute suspended
underneath.
The parachute has so much more drag in the water than the mast
in the air that the whole thing follows the water.
deployed at any designed depth.
The parachute can be
For the most part we opened ours just
beneath the surface so we followed the integrated current in about the first
5 meters of water.
The ship's radar is then used to determine the position
of the drogues every fifteen minutes with reference to some fixed location either an anchored buoy or a point of land if close enough.
In this case
we laid out a line starting from 1 mile off Yaquina Head with 6 drogues
spaced at 1/2 mile intervals.
We followed the drogues for about 40 hours
or until they disapppeared from radar range (one came ashore and two drifted
out of range but we were able to get a final point when we recovered it).
This is much longer than is usual for this type of operation and we were
fortunate to collect some of the best data taken this close to shore.
Computer programs are available to reduce, plot and perform some preliminary
analysis of these data.
At this writing we have not completed the analysis
but some preliminary conclusions can be made and will be discussed under
Results.
This data is found in Appendix V.
Electromagnetic Current Meter
On 19 October we tested an electromagnetic current meter owned by the
School to see if it could give us some useful data.
The probe is mounted on
a 15' pole on the side of a small boat and the probe can be read while the
ship is underway.
This of course includes the ship's motion but time changes
in the current can be noted and the absolute current calculated if the boat's
velocity is known.
While data can be easily recorded the analysis is not
simple and must be done on a computer. To date only preliminary printouts
have been obtained and so no more can be said of the data. The instrument
16
might well be useful in conjunction with other measurements but the analysis
time will have to be considered against other factors, particularly since
it gives too much information for our particular purposes.
CUE Data
Much of the data produced by the CUE program is of interest to us. We
have the complete summary of the meteorological data which is in a large
format book plus the hydrographic data. Some special drogue measurements
were made during the period by groups from California and Connecticut which
will be available to us as soon as they have been analyzed by the scientists
who directed this part of the program. This should be in a matter of weeks
from this writing.
We list below some of the special observations which will be available
and one of particular interest to our program.
Vertical current meters moored in 70-80 m of water
10-18 July, 1972
Hydrographic data from Depoe Bay line
5-17 July
KAPPA buoy - moored current meters, 10 miles offshore From 15 April 1972
Aircraft measurements of atmospheric conditions surface temperature,
25 miles
surface chlorophyll
Tide recorders
Drogue trackings
mid July -
offshore
of Newport
August 10-17
mid August
2-3 miles offshore Lincoln Beach
7 August, 1972
We have not yet incorporated all the CUE data into our analysis program
be useful in interpreting our description of the nearshore
circulation.
Also the overall CUE program results on the reaction of the
water to changes in wind velocity will guide our subsequent analysis even
though not directly observed in our area. It should be mentioned in passing
that some of our drift bottle data have been quite useful to the CUE program
as well.
but they will
Results of
Current Studies
The most obvious impression we get from an overall view of our data is
system is quite variable from day-to-day. It is
extract general statements about the circulation and consequently
a given site cannot begin to be understood on the basis of a few
that the nearshore current
difficult to
implies
that
17
measurements.
In general the wind seems to be the most important
single
feature:
all our data show good correlation with the wind
direction.
Both
the drift bottles and the drogues go downwind
when the wind is more or less
parallel to the shore.
In one case (10 June) we dropped a number of bottles
with east (offshore) winds and found
none on our beach and only a 7% return
from the public overall.
In view of our usual experience we have to conclude
that these were blown well out to sea and probably
drifted South subsequently.
Because we dropped these farther out than subsequent
drops (we were using
R/V CAYUSE which could not approach nearer than
1
mile from shore) we don't
know what happens quite close.
In general the water movements closer than 1/4 mile
from shore almost
invariably are toward shore even if the winds
are parallel to it. Almost
all bottles and drogue observations indicate
a long-shore drift with a slight
component inshore. There is some evidence
that seaward of 1/4 - 1/2 mile
the drift is slightly offshore since bottles dropped
there are generally
recovered North or South of our beach.
Once the drogues or bottles are
caught in the surf zone they
come ashore quickly and as might be expected
their motion becomes less dependent on wind and
move dependent on the surf
and the set of the tide.
It is not always true, however, that the bottles
come on shore only with an incoming tide.
Furthermore, the tidal currents have considerable effect
on
and direction of flow and can be the main cause of motion if the
light.
the speed
winds are
We have yet to see motion against the wind but this does
not seem
impossible.
In general then there is some evidence that the nearshore
zone may
divide into two regions.
In the closest one the probability that the surface
water has a strong on-shore component and that material released
at the surface there will be found on the shore within a few hours
and within a few
miles of the release point. Seaward of this zone material
would drift along
shore for much greater distance and times.
At times the boundary between
the zones appears to be quite sharp - less than 1/4 mile thick.
At present
we cannot say whether this is a feature typical of all coasts
or whether
the presence of headlands to the north & south contribute
to this apparent
pattern.
This same pattern was noted in our January data.
All the drogues
showed the influence of the tidal motions but the
drogues launched furthest
18
from the shore showed a net drift toward the southwest whereas the middle
two drogues showed a net drift to the northwest and the inshore pair a very
slight drift toward the west.
Some mention should be made of the fate of those bottles which did not
come ashore in the immediate vicinity of the drifts.
For the most part they
were recovered, whether north or south, within 15 miles of the release points
but some travelled as far north as Cape Kiwanda and some as far south
as
Waldport or beyond.
One bottle, dropped 1 1/2 miles offshore, was recovered off the mouth
of San Francisco Bay 500 miles south. This has received some notoriety
because heretofore it was not expected that waters that close to shore would
drift that fast (ti 1/3 knot average).
south as Bandon, Oregon.
We also received returns from as far
There were indications that some clusters would
drift south with the wind and then turn north as the wind shifted and pass
the beach and end up around Pacific City.
These data have been of much
interest to the CUE study and will be of help to them in their analysis as
well as indicating to us that considerable offshore drift can occur from
distance fairly close to the beach.
One further observation should be discussed because of its implication
for biological sampling as well as for its suggestion about water movements.
When we dropped a die marker from the airplane one of the markers spent a
great deal of time following along a foam line. Judging from the known size
of the package the foam line was only about 1 foot wide and yet remained
intact with the marker floating in it for some distance even though the sea
was quite rough and the wind very strong.
Foam lines have been thought to
be areas of convergence where the surface waters come together and sink
leaving the floating material at the surface.
Our chance observations would
seem to confirm this and also to suggest that there may well be a number of
regions where convergence and divergence exist.
The same phenomenon was
seen, on a larger scale, during one of the CUE tests where drogues laid out
perpendicular to the shore were found subsequently in a line parallel to
the shore.
Such regions of convergence and divergence could quite possibly
affect the distribution of plankton and, therefore, those organisms that
feed on them.
Thus it seems imperative to investigate these regions since
this could lead to very uneven distribution of organisms in these waters
and increases the difficulty of obtaining representative population samples.
APPENDIX I
Appendix I shows an example of the data collected on one day's run.
Only the results of a single days measurements are shown, since the vari-
ability encountered during this first years operation was so great that
we have little confidence in the actual meaning of the numbers. Both the
field data and lab work-up analysis are presented.
The following pages contain the results of the spectrophotometric
determination of chlorophylls, phaeopigments and carotenoids in phytoplankton crops. The procedures and equations may be found in Strickland
and Parsons A Practical Handbook of Seawater Analysis.
DEPTH
is given in meters.
P. S.
denotes Parsons and Strickland.
S/U)
denotes SCOR/UNESCO.
CHLOROPHYLL
is given in mg/m3
PHAEOPHYTIN
is given in millispecified plant pigment
unit approximating the milligram.
Chi. A/Carot
is given in mg/millispecified plant
pigment unit.
station no.
time
or
of
coordinates
day
bottle
depth
!Q
5
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CRUISE IDEtlfIFiCAT {ON
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OBSERVER
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Pigment Content of a Phytoplankton Crop
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300
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630
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480
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645 630
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Pigment Content of a Phytoplankton Crop
Cruise IdentificationA rA o fffk Station Identification
a:..p1e
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.
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5
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PIGMENT ANALYSIS
North of Moolack
Station:
--
l
F14TE/t NUMBER.
R
:
Date: 8/21/72
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1
APPENDIX II
Zooplankton were sampled at varying stations throughout the summer.
These stations were all coded based on distance from shore and are indicated
in the attached drawing. Station coding for an individual sample was setup for the computer and is explained in the key to the appendix. Indications
may be made for distance from shore, relative position between the rocks,
depth, and replicate tows &
data for each sampling day.
printouts tabulate the
Each table contains the data for four stations
counts.
The computer
giving either absolute abundances or percentages
females and the immatures present.
the units are indicated
for the adult males and
The physical data
in the key to the appendix.
is also tabulated and
Key To The Appendix
General Station Designation:
ex:
1.50 indicates the station 1.5 miles offshore
.2N indicates the station 0.2 miles offshore on the North end
of the study region
.2C .2 miles offshore on the central sampling track
.2S .2 miles offshore on the South end of the study region
Special Designations:
July 26, 1972 - Replicate tow designation
.4N1
= first tow towing to the North at .4 mi. offshore
.4N2
= second tow towing to the North at .4 mi. offshore
S
= South
W
= West
SS
= Station at south end of study area
NN
= Station at North end of study area
August 1, 1972
Depth series designation
2.25A
= tow at 2.25 miles offshore at depth of 3 m
2.25B
=
15 m death, 2.25 mi. offshore
2.25C
=
30 m depth, 2.25 mi. offshore
2.25D
=
9 m depth, 2.25 mi. offshore
2.25EE
=
9 midepth, 2.25 mi. offshore
August 8, 1972
Replicate counts
.4R1: .4 = .4 mi. offshore
R = replicate count
1
= first count made on sample
Data Print-out:
ex:
Datum
Surface
.2C
Temp.
Surface Salinity
Bottom Temp.
Bottom Salinity
Forel No.
Secchi Reading
10.500
33.7600
9.800
33.7770
7
5.5
(Station Number)
(in ° C)
(in %o
)
(in ° C)
(in %o )
(pure number)
(in meters)
(from 8-8-72)
Forel Number Interpretation:
1-2
=
blue water
3-4
=
blueish-green
5-7
=
green
8-10 =
yellowish-green
Zooplankton Station Location
X 5.00
N
X 4.00
Key
x
Station
Rock
Surf
----- Shoreline
(not drawn to scale)
STATIONS ON 07/26/72
DA TUM
.4N1
SURFACE TEMP.
SURFACE SALINITY
9.8J0
33.5660
8.500
BOTTOM TEMP.
BOTTOM SALINITY
FOREL NO.
SECCHI READING
.4N2
.4,3
9.800
9.810
33.5060
33.5661
8.500
33.6120
33.6120
9
9
8.6
8.0
.4S4
9.800
33.b120
33.5660
8.500
33.6120
7.1i
3.0
8.500
6
THE FULLOWIJG TABLE LISTS ABSJLUTE ABUNDANCES
(NUMBER OF INDIVIDUALS PER CUBIC METER OF WATER FILTLREC)
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
FEl ALEES
MALES
IMMS
F_MALEi
MALES
IMMS
ACARTIA CLAUSI
ACARTIA LONGIREM
CALANUS SP
CENTROPASES MCMU
EUCALANUS SP
OITHONA SIMILIS
OITHONA SPINIROS
PSE000CALANUS
COPEPOD NAUPLIUS
50.8
48.3
36.6
34.1
73.2
23.3
74.2
74.2
31.7
29.2
91.7
28.4
2.5
99.5
97.5
6.0
2.U
31.8
39.8
95.5
77.6
59.7
53.3
0
0
124.5
110.5
1.3
2.6
0
0
0
0
0
0
0
107.9
68.6
3.8
1.3
1.3
2.5
GAMMARIO AMPHIPO
BARNACLE CYPRIS
BARNACLE NAUPLIU
CHAETOGNATHA
CRAB ZOEA
HERMIT CRAB LARV
PORCELAIN CRAB Z
CRUSTACEAN EGGS
DECAPOD LARVAE
0
0
2.5
1.7
0
.8
U
C.
U
0
0
0
0
0
G
00.7
.3
G
0
7.5
118.4
0
3.3
240.8
0
0
0
0
0
0
U
0
G
G
0
6.7
7.5
36.6
31.7
10.0
46.7
8.0
49.8
0
0
0
G
0
0
29.9
2.0
G
0
174.0
3.8
27.9
1.3
0
U
0
1.7
0
0
0
G
0
J
1.7
U
0
0
G
a
0
G
G
0
0
0
0
0
0
0
0
G
0
U
0
0
0
.5
1.7
G
G
0
0
0
0
0
0
0
0
0
.8
0
0
C
U
G
U
1.7
0
0
2.0
1.7
0
0
G
U
0
C
6.0
0
1.3
0
0
26.7
49.5
0
0
0
0
0
0
0
0
0
0
7.6
1.3
0
0
0
0
0
0
0
0
C
1
0
0
0
0
0
G
G
0
0
U
0
14.3
1.3
2.5
0
0
0
0
0
0
3.3
2.5
0
0
0
7.5
u
0
0
0
MEDUSAE
0
.8
0
D
2.0
0
0
MYSID LARVAE
3.3
0
0
12.5
0
1
6.0
0
0
THE FOLLOWING T ABLE LIbTS THE FRACTIJN OF TOTAL STATION ABUNSANCc
ACARTIA CLAUSI
ACARTIA LONGIREM
CALANUS SP
CENTROPAGES M CMU
EUCALANUS SP
OITHONA SIMI L IS
OITHONA SPI 41ROS
PSEUDUCALANUS
COPEPOD NAU?LIUS
GAMMARID AMPH IPO
BARNACLE CYPRIS
BARNACLE NAUP LIU
CHAETOGNAT H 4
CRAB ZOEA
HERMIT CRAB LARV
PORCE L A IN CAB Z
CRUSTACEAN EGGS
DECAPOD LARVAE
MEDUSAS
MYSID LARVAE
1
.1259
.1196
.0545
0
0
.1297
.1297
.0029
.0510
0
.1514
.0577
.0662
0
.1563
.0496
. 004 .
.u021
U
0
0
6
.6015
.0053
u 3J7
.055'.
0
u
u
0
U
.1505
0
.U186
.2070
0
u
0
6
.1241
.0397
.0496
.1131
.0968
.1469
.12 i6
.130'.
.0705
.0630
007 4
.0u25
0
0
.0015
.0015
.0025
G
0
0
G
0
0
0
.3002
0
0
.005L
0
6
0
U81n
.0372
.0099
.0620
.
0
d
.0165
.313o
.0907
u
u
0
0
G
0
.0025
0
U
0
G
0
.0029
.2054
.0045
.0330
.0015
0
.0641
0
0
0
U
0
G
0
0
0
0
0
0
0
G
0
0
7
u
0
0
.0390
.0015
6
G
.
0554
.
0175
.
0
0
0
0
0
0
U
0
.0029
0
.0021
0
0
0
0
0
3
u
0
0
0
G
G
.6025
0
0
U
0
U
.0015
.0029
.0041
0
0
0
u
0
0
0
.0131
.0015
.0219
0
0
0
.0082
.0062
.0032
0
0
0
u
0
0
7
0
0
.0074
.0025
.0074
0
.1274
.0810
.0045
.0015
.0015
.0030
0
0
.0315
.0585
0
0
0
0
0
0
0
G
0
0
6
0
0
0
u
0
0
0
0
0
0
G
0
0
0
u
0
u
.0165
.0015
.0033
0
0
0
0
0
0
G
0
0
STATIONS ON 37/2o/72
.4W5
DATUM
SURFAC. TEMP.
SURFACE SALINITY
BOTTUM TLMP.
BOTTOM SALINITY
FOREL NO.
SECCHI READING
.2
.4W6
.75
9.600
0
0
0
9.830
33.5660
3.533
33.6120
33.5660
8.501
33.6120
0
5
5
7
7.5
7.5
7
4.5
9.5
9.800
0
0
THE FOLLOWIVG TALE LISTS ABSOLUTE ABUNDANCES
(NUMBE,t OF INDIVIDUALS PER CU3IC MLTER OF WATER FILTERED)
FEMALES
ACARTIA CLAUSI
ACARTIA LONuIREM
CALANUS SP
GENTROPAGES '$CMU
OITHONA SIMILIS
OITHONA SPIAIRUS
PSEUOOGALANUS
COPEPOD NAU°LIUS
UNIDENT CALANOID
HARPACTICOID
SAMMARIO AMPHIPO
BARNACLE CYPRIS
BARNACLE NA!JPLIU
CRAB ZOEA
295.9
408.9
2.7
2.7
67.3
5.4
72.6
2.7
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
69.9
209.6
138.3
20.3
67.0
56.4
257.4
29.3
38.7
152.1
81.9
0
0
0
2.1
119.3
L
12.2
50.2
53.3
21.9
145.3
249.6
99.4
220.6
0
0
C
0
0
0
0
0
0
0
96.1
0
3.1
5.2
0
2.1
103.0
2.3
334.6
77.2
7.0
2.3
6.3
27.2
2.7
5.4
8.1
0
0
0
5.4
42.6
0
0
0
6.1
0
2.0
35.0
153.3
67.0
26.4
105.5
0
147.4
72.5
517.1
0
u
G
2.0
0
0
0
0
0
C
0
u
0
0
0
0
J
C
3
0
0
0
0
U
3
0
0
0
1.C
2.3
0
D
0
0
U
0
J
0
0
J
0
0
0
0
0
0
0
0
0
0
0
0
3
0
0
0
0
3
0
0
0
0
2.1
1.0
2.1
0
G.
0
0
0
0
0
0
0
0
0
0
0
U
3
C
0
0
3
0
0
0
0
18.7
0
0
0
0
0
0
0
0
0
0
0
u
0
0
0
0
0
0
0
0
0
2.7
CRUSTACEAN EGGS
DECAPOD LARVAE
GASTROPOD LARVAE
0
0
0
0
2.7
0
0
G
0
0
0
0
0
1.G
0
0
0
0
0
0
0
0
0
0
0
8.1
1
1.0
2.1
0
0
0
0
1
0
MYSIO LARVAE
0
0
14.6
1.u
PORCELAIN CRAB Z
MEOUSAE
2.3
0
0
0
4.7
2.3
9.4
2.3
2.3
4.7
THE FO LL O WING TA3LE LISTS
ACARTIA CLAUSI
ACARTIA LUNGIKL'1
CALANUS SP
CENTRUPAGES MCMU
OITHONA SIMILIS
OITHONASFINIROS
PSEUOOCALANUS
COPEPOD NAUPLIUS
UNIDENI CALANUID
HARPACTICUID
GAIMARIO AMPHIPO
BARNACLE CYPRIS
BARNACLE NAJPLIU
CRAB ZOEA
PORCELAIN CRAB Z
CRUSTACEAN EGGS
DECAPOD LARVAL
GASTROPOD LARVAE
MEDOSAE
MYSID LARVAE
THE FKACIIUN OF TOTAL STATION ABJNUANCE
.1713
.2368
.u4J5
.1277
.0016
u
0
.1015
.0841
.6631
.0347
.OC31
0
G
.0202
.6688
0
0
.0507
.6097
.0797
.6024
0
0
.0025
6
C
0
0
0
0
0
0
0
0
6
0
0
.0012
0
0
0
0
0
0
0
0
0
0
0
U
u
G
6
0
.0025
.0050
6
0
u
0
0
0
0
0
0
0
0
0
.OU25
0
C
0
0
0
0
0
0
3
0
C
0
J
.C024
0
0
G
0
0
.0056
O
O
6
u
.0016
O
.0012
0
u
0
0
0
0
0
0
0
0
0
0
0
0
.0016
0
0
G
0
0
0
0
0
0
C
0
.0025
0
0
0
0
0
.0049
.0012
.0097
0
0
0
0
.0025
0
0
0
0
0
0
0
0
G
0
G
3
J
.0050
.0047
0
0
.0012
0
0
0
0
6
C
0
G
0
0
.0024
0
0
.3016
.0389
.0031
.0421
.0016
.0016
.1b43
.2971
.1200
.1275
.0525
u
.0145
6
0
0
0
0
C
.3314
.0024
.1256
.2300
.0075
.0356
.32Y2
.0797
0
.1184
.1333
.0620
0
.1353
.3925
.0050
0
u
u
0
.0125
.0050
.0650
.0535
.6012
.0766
0
0
.0377
.2689
0
0
0
.0700
0
.0150
.0791
.0426
3
6012
. 1740
.0401
.0036
. 0012
0
0
0
.
0
NATIONS ON 07/26/72
DATUM
1.0
SURFACE TcMP.
SURFACE SALINITY
30TTOM TEMP.
BOTTOM
SALINITY
FOREL NO.
SECCHI READING
1.25
1.56
0
6
I
U
0
C
0
0
0
0
0
0
0
0
10.3
7.5
8
8
11.0
9.5
1.75
10
FOLLOWING TABLE LISTS ABSJLUTC ABUNDANCES
(NUMBER OF INDIVIDUALS PER CU3IC METER OF WATER FILT=R=D)
THE
ACARTIA CLAUSI
ACARTIA LONGIREM
GALANUS SP
CENTROPAGES MCMU
OITHONA SIMILIS
OITHONA SPINIROS
PSEUDOCALANUS
COPEPOD NAUPLIUS
HLRMIT CRAB LARV
PORCELAIN CRAB Z
CRUSTACEAN EGGS
DECAPOD LARVAE
GASTROPOD LARVAE
MEUUSAE
FEMALES
MALES
IMMS
FLhALES
109.6
174.6
44.7
65.0
0
4.1
69.u
77.2
8.1
0
0
0
0
0
0
0
61.2
5. 1
437.3
4. 1
0
20.3
125.3
0
0
20.3
0
8.1
MALES
IMMS
33.6
37.1
410.8
183.4
FEMALES
MALES
IM'IS
FEMALES
MALES
IMMS
48.7
1.7
355.3
16.8
5.0
102.2
1.7
48.6
2.9
58.U
751.1
11.7
237.7
5.3
184.8
37.1
4.6
0
0
0
1.7
73.7
0
36.9
111.:
0
0
0
0
C
14.7
0
0
0
58.7
U
u
2.3
0
u
6
0
0
0
0
0
73.1
1647.7
55.7
4.6
153.3
3.4
0
8.4
0
5.9
0
C
1
3.4
8.8
0
C
2.9
0
0
6
0
0
0
0
0
0
0
0
u
0
6
0
0
0
0
0
S
0
0
0
0
0
0
0
2.3
6
2.3
13.9
4.6
2.3
0
0
L
0
C
0
0
C
0
3
C
0
0
8.8
0
C
0
L
0
U
0
0
0
1.7
0
0
0
0
0
2.9
0
6
G
0
0
0
0
U
0
0
THE FOLLOWIAu TABLE LISTS THE FrtACTIuN OF TOTAL STATION A0UNUANCL
ACARTIA CLAUSI
ACARTIA LONGIREM
CALANUS 3P
CENTROPAGES MCMU
OITHONA SIMILIS
OITHONH SPINIRO5
PSZUOCCALANUS
COPEPOD NAUPLIUS
HERMIT CRAB LARD
PORCELAIN CRAB Z
CRUSTACEAN EGGS
DECAPOO LARVAE
GASTROPOD LARVAE
MEOUSAE
.0476
.0758
.0300
.0335
.0035
.0681
.3340
.3302
.1493
0
.0194
.0282
.3018
0
0
.0397
.0473
.0302
G
0
0
0
0
.0038
0
.0688
0
u
.u317
.4551
.1021
.0019
.0454
.0353
.0035
.2116
.0018
3u
.0025
.5381
.0254
.0376
.1548
G
.0021
.5333
.0792
.0083
.1638
0
.0025
.0736
.0558
0
2C+2
.1312
.3.17
.0;;25
0
0
G
0
0
0
.0104
C
C
0
U
0
3
0
J
.1117
0
U
C
.3038
.1229
3
.0127
U
0
.0063
.0021
0
0
0
0
0
.Ou51
.GG51
J
G
0
.0019
G
0
0
0
0
0
C
5
G
U
0
0
0
U
U
0
U
0
0
G
0
C
C
0
.0063
0
0
0
0
2
0
0
0
3
0
0
.0035
0
U
.0019
.0113
0
0
C
0
0
0
0
0
U
0
.G038'
0
0
.GC25
0
0
.0021
J
0
U
.0019
0
6
U
0
0
0
0
0
STATIONS ON 07/26/72
DATUM
2.0
SURFACE TEMP.
SURFACE SALINITY
BOTTOM TEMP.
BOTTOM SALINITY
FUREL NO.
SECCrII READING
2.25
0
10.700
0
33.0680
.4NN
.4SS
10.000
10.300
33.5560
33.5640
0
0
8.400
0
33.6680
33.6060
8.500
33.6220
10
IC
9
9
7.5
7.5
3.0
3.0
THE FOLLOWING TABLE LISTS ABSOLUTE ABUNDANCES
(NUMBER OF INDIVIDUALS PEk CUBIC MLTER OF WATER FILTERED)
ACARTIA CLAJSI
ACARTIA LONGIREM
CALANUS SP
CENTROPAGES MCMU
EUCALANUS SP
OITHONA SIMILIS
PSE000CALANOS
COPEPOD NAUPLIUS
HYPERIID AMPHIPO
CAB MEGALOPS
DECAPOO LARVAE
GASTROPOD LARVAE
FEMALES
MALES
IMMS
FEPALLS
6.4
378.3
0
C
132.0
959.3
23.2
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
0
J
11.4
283.9
262.4
155.3
308.0
69.5
9.8
32.1
6.5
211.7
174.1
115.2
IAMS
0
4.8
54.7
32.2
3.3
46.3
0
C
9.8
8.0
1.0
0
0
0
0
3.2
0
0
0
0
0
0
u
2.7
0
0
0
C
0
0
0
3.3
u
0
0
J
0
0
4.8
4.8
1.6
1.6
0
u
0
0
.5
0
0
0
8.1
0
6.6
5.4
u
12.9
18.7
10.7
0
0
9.9
9.9
5.4
61.6
0
0
0
0
0
0
0
0
C
0
0
0
0
u
0
J
0
0
0
0
0
0
0
0
3.3
C
0
0
0
0
0
J
0
0
1.6
0
0
3.3
0
0
0
0
J
3
0
0
0
0
1
0
0
0
.3
0
0
0
0
0
30.6
THE FOLLOWING TABLE LISTS THE FRACTION OF TOTAL STATION ABUNDANCE
ACARTIA CLAJSI
ACARTIA LONjIREM
CALANUS 3P
.0097
.5690
.0460
.1385
CENTROPAGES MCMU
U
EUCALANUS SP
OITHONA SIMILIS
PSEJJOCALAN'JS
COPEPOJ NAUPLIUS
MYPERIIO AMPHIPO
CRAB MEGALOaS
OECAPOJ LARVAE
GASTROPOD LARVAE
C
C
J
0
.6073
.0823
.0484
.7168
.6172
.1569
.0625
.U048
.0515
.0343
0
0
0
0
0
0
0
.0073
.0u73
.U024
0
0
u
.0121
.0674
.0074
0
G
0
0
.UU24
u
.10C
.3230
.6661
.1164
U
0
.1005
.0820
.u106
0
C
0
0
.6025
C
6
0
0
.6049
.0053
.0556
0
0
0
0
0
0
0
0
0
.0025
0
u
.1024
U
u
.0025
u
0
0
0
0
0
0
0
.2031
.1877
.1111
.2203
.125
.082,+
J
G
0
0
.0019
C
0
U
0
G
0
0
0
0
6
0
0
.1323
.U134
.0077
.0638
.0441
C
C
0
0
0
0
0
0
0
u
0
0
0
U
0
0
0
0
G
0
U
C
0
O
0
O
.0 .26
u
STATIO'4S ON 39/01/72
DATUM
2.25A
SURFACE TEMP.
SURFACE SALINITY
BOTTOM TEMP.
9.4J0
33.6076
0
0
SALINITY
FOREL NO.
SECCHI READING
BOTTOM
2.25
2.25
2.25
9.400
33.6070
9.406
33.7430
9.400
33.6070
8.900
33.8140
9.400
33.6070
0
33.3270
10
1G
13
10
6.u
8.0
8.0
8.0
THE. FOLLUWI4G TABLE LISTS ABSOLUTE ABUNJANCES
(NUMBER JF INDIVIDUALS PER CUBIC METER OF WATER FILTcKED)
IMIS
FEMALES
MALES
IMMS
FEMALES
MALES
9.9
44.8
6.1
78.8
42.4
103.1
175.8
6.3
380.5
18.1
139.2
197.2
199.3
108.7
0
u
0
G
12.1
0
6.1
200.1
42.4
6.1
200.1
12.1
2..2
179.0
0
0
u
19.9
875.2
533.5
1339.9
0
3
12.1
127.3
U
0
223.7
18.1
0
u
G
0
u
G
0
7
6.1
0
0
0
5.0
0
3
12.1
0
0
9
0
0
0
J
0
7
6.1
48.5
0
3
0
0
0
0
0
0
FEMALES
MALLS
1MMS
3 ARTI4 CLAJS1
ACARTIA LONSIREM
CALANUS SP
8.9
539.9
0.9
253.7
11.8
19.9
168.2
11.8
6
CENTROPAGES MCMU
14.8
44.3
11.8
0
5.9
5.9
3.u
353.1
34.8
5.0
29.8
0
0
0
U
0
0
G
35.4
:i.9
383.5
119.4
29.5
0
u
U
0
0
24.9
5.0
0
U
0
3.0
0
0
0
0
0
0
u
0
8.9
0
0
0
0
0
5.0
24.9
94.5
5.0
0
U
0
0
3.0
0
0
0
0
0
0
0
u
OITHONA SIMILIS
OITHONA SPIAIROS
PSE'JDGCALANJS
COPEPOD NAUPLIUS
HYPERIIO AMPHIPO
ANNELID LARVAE
BARNACLE NAUPLIU
CHAETOGNATHA
PODON LEUCKARTI
CRUSTACEAN EGGS
DECAPOD LARVAE
GASTROPOD EGGS
GASTROPOD LARVAE
ISOPOOA
MEDUSAS
FEMALES
24.9
9.9
5.0
MALES
0
5.9
104.4
3
0
0
24.2
0
6.0
6
IMMS
U
0
0
0
0
978.5
0
U
0
0
0
0
0
0
u-
0
u
0
0
0
0
0
0
0
0
0
G
0
0
12.1
151.0
0
u
0
6.1
0
0
0
0
0
G
0
0
0
J
0
0
1
1,
0
0
0
0
36.2
0
0
u
0
0
0
0
0
0
THE FCLLOWI`JG TABLE LISTS THz FRACTION OF TOTAL STATION ABUNDANCE
ACARTIA CLAUSI
ACARTIA LONGIREM
CALANUS SF
CENTROPAGES MCMU
UITHONA SIMILIS
OITHJNA SPINIROS
PSEUOOCALANUSS
COPEPOD NAUPLIUS
HYPERIID AMPHIPO
ANNELIO LARVAE
BArrNACLE NAUPLIU
CHAETOGNATHA
PJDUN LEUCKARTI
CKUSTACEAN EGGS
DEGAPOJ LARVAE
GASTROPOD ESGS
GASTROPOD LARVAE
ISOPuOA
MEOUSAE
.0057
0,::?7
.3466
.0076
.1629
.007b
.1080
.0092
.1625
.0046
.0824
.0206
.0095
.0284
.0038
.0038
.0160
.0023
0
.0491
.3076
.u046
C
.OU19
.0137
0
0
0
0
0
0
.0227
.0189
.J3S8
.2462
.0092
u
u
U
U
0
.0549
.0114
.0023
0
3
0
0
0
0
0
-
.0019
C
u
0
1
0
0
.061.1
.3023
.0667
.0141
.0C20
.0020
.0263
.0141
.3343
.0586
.0025
.1573
.0100
.0130
.0777
U
.3075
.0827
.0451
0
0
C
3
.0025
0
0
C.
.0050
0
0
.0667
JCv0
.1776
0
0
3
C
0
.0424
.4465
0
.4060
.G4C
0
G
.0927
.0075
0
0
0
0
0
.:020
J
0
G
0
0
0
0
u
0
040
0
0
1
C
G
0
0
0
0
0
0
0
G
0
0
0
0
.0059
.0627
0
u
.x020
102
0
0
0
L
u
3
0
J
0
0
u
0
0
0
3
.4027
0
0
C
O
.0023
.0023
.0114
.0435
.JG23
0
0
0
0
0
.3020
.0019
0
0
.0114
0
C
u
.0150
0
0
C
u
.0046
0
0
0
U
0
U
0
J
0
0
0
.0023
0
L
0
0
0
0
0
U.
-
.0057
0
C.
STATIONS ON 03/01/72
2.25t
uATUM
9.4u0
SURFAC
TEMP.
SURFACE SALINITY
33.bJ7U
BOTTOM TcMP.
BOTTOM SALINITY
FOREL NO.
U
33.j270
10
8.0
SECCHI R AOING
THE FOLLOWING TABLE LISTS A3SOLUTE ABUNDANCES
(NUMBER OF INDIVIDUALS PEF. CUBIC MLTLR OF WATER FILTcREC)
FEMALES
ACARTIA CLAUSI
ACARTIA LONJ-IREM
CALANUS SP
CENTROPAGES MCMU
OITHONA SIMILIS
PSEUDOCALANUS
COPEPOD NAUPLIUS
BARNACLE NAJPLIU
CRUSTACEAN EGGS
MALES
IMMS
11.3
11.3
11.3
420.0
7.5
3.8
26.3
82.5
20.3
7.5
108.8
288.8
97.5
26.3
3.8
0
3.8
0
0
3.8
551.3
0
J
U
0
G
0
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
THE FULLOWINL TA3LL LISTS THE FRACTIuN OF TOTAL STATION AEUNDANCE
ACARTIA CLAUSI
ACARTIA LONGIRc.M
CALANUS SP
CtNTROPAGES MCMU
OITHONA SIMILIS
PSEUDOCALANJS
COPEPOD NAUPLIUS
BARNACLE NAJPLIU
CRUSTACEAN EGGS
.0066
.2479
.0044
.OG22
.0155
.487
.6155
.0044
0642
.JJ66
.1704
.0066
0
U575
0155
.GU22
.0022
G
0
.JU22
.3252
G
0
6
0
0
0
STATIONS J.4 03/08/72
DATUM
.4R1
SURFACE TEMP.
SURFACE SALINITY
BOTTOM TEMP.
BOTTOM SALINITY
FOREL NO.
SECCHI READING
16.400
33.7640
9.400
33.78-)0
.4R2
.4R3
10.4J0
33.7640
9.40G
33.7890
10.400
33.7640
9.400
33.7390
1.0
10.350
33.7710
8.600
33.8120
7
7
7
7.u
6
7.0
7.0
6.0
THE FOLLOWI.40 TABLE LISTS ABSULJTt ABUNDANCES
(NUMBER OF INDIVIDUALS PE( CUBIC METER OF WATER FILTERED)
FEMALES
MALES
IMMS
FEMALE
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
419.6
155.1
173.3
173.3
711.5
695.4
205.2
136.8
125.4
056.6
191.5
109.4
136.6
76b.1
259.9
389.3
40.5
C
54.7
0
G
0
0
109.4
356.9
48.7
0
786.6
171.0
68.4
324.4
209.8
0
0
56.8
CENTROPAGES .'1CMU
0
9.1
0
0
0
0
C
G
0
0
0
0
OITHONA sIMILIS
PSEUDOCALANJS
COPEPOD NAU?LIUS
ANNELIJ LARVAE
BARNACLE CYPRIS
BARNACLE NAJPLIU
PODON LEUCKA2TI
CRAB ZJEA
HERMIT CRAB LARV
PORCELAIN CRAB Z
CRUSTACEAN EGGS
18.2
1322.7
282.3
J
0
u
a
13.1
0
0
0
1696.7
91.2
1755.o
150.5
1942.6
162.2
786.7
u
u
U
7
9.1
G
0
0
0
0
0
11.4
1272.2
437.8
16.2
811.0
+70.4
0
173.3
34.2
1333.8
296.4
0
0
C
G
0
16.2
0
C
0
0
J
G
0
a
L
G
0
0
0
0
0
U
G
u
u
L
0
0
0
0
0
0
3
13.7
41.0
0
0
0
C
0
G
0
0
C
0
0
0
0
0
0
0
u
0
0
0
0
0
0
0
0
0
J
0
0
0
0
AGARTIA JLAJSI
ACARTIA LONoIREM
CALANUS SP
9.1
9.1
9.1
8.1
308.2
97.3
0
0
0
u
0
0
0
C
0
3
C
0
G
216.9
16.2
64.9
16.2
0
0
148.2
0
0
123.1
0
0
64.9
OECAPOO LARVAE
0
G
0
0
0
0
G
C
0
GASTROPOD LARVAE
0
G
0
0
0
0
C
C
MEOUSAE
0
0
0
0
0
0
C
0
0
0
40.5
16.2
8.1
8.1
THE FOLLOWING TAaLE LISTS THE FRACTION OF TOT,L STATION ABUNOANCL
ACARTIA CLAUSI
ACARTIA LONGIREI
CALANUS SP
.0742
.6274
CENTROPAGES 'ICMU
OITHONA SIMILIS
PSEOOOCALANJS
CUPEPOD NAUPLIUS
ANNELID LARVAE
BARNACLE CYPRIS
BARNACLE NAJPLIU
PODON LEUCKARTI
CRAB ZOEA
HERMIT CRAB LARV
PORCELAIN CKAB Z
CRUSTACEAN =SGS
DECAPOD LARVAE
GASTROPOD LARVAE
MEDUSAE
.1187
.0350
.0306
.6306
.1253
.0371
G
U
.0016
.0697
0
0
.OG32
.2339
.0500
0
0
.0058
.6306
.3u0u
G
u
.0016
.2276
.0506
L
0
0
.0019
0
.0233
.6214
.1342
.0292
.1055
.03J8
.1231
.0418
G
G
.0117
.G176
.0220
0
0
.0176
0
0
0
G
0
J
C
0
.0022
G
0
.0038
.6156
.2996
.0242
.3121
G
.2644
.0703
C
0
.1687
.109+
U
0
G
3
.0038
.C83u
.6113
.0906
.0094
.0755
.0019
G
0
.0132
0
0
0
.6019
.6717
.022b
.0038
.0151
.0038
.0151
0
U
0
0
0
0
0
0
0
.0016
.0016
.0016
0
0
0
0
0
0
0
0
G
0
0
0
.0022
OObb
0
0
0
0
0
G
0
0
0
3
J
U
U
0
0
J
0
0
0
0
0
U
0
0
J
U
G
0
.0387
0
0
.0253
G
G
.0198
0
O
0
0
0
0
0
U
0
0
0
J
0
0
0
0
G
6
0
0
.6094
.0039
0
U
0
C
0
1
0
G
0
.0019
0
0
.0377
.1830
0
0
0
0
0
0
0
0
0
0
0
O
0
0
0
0
G
0
0
0
0
0
G
0
STATIONS ON 63/09/72
DATUM
1.5
10.400
SURFACc TEMP.
SURFACE SALINITY
10.450
33.7610
BOTTOM SALINITY
FOREL NU.
SECCHI READING
.2N
10.400
10.300
33.7740
U
7.9u0
0
33.7330
9.500
33.315C
33.8160
33.8140
33.7920
6
6
6
7
5.0
4.5
6.0
6.0
33.7570
BOTTOM TEMP.
2.5
2.0
THE FOLLOWING TABLE LIS1S ABSOLUTE ABUNDANCES
(NUMBER OF INDIVIDUALS PER CUBIC METER OF WATER FILTcREO)
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
ACARTIA CLAJSI
ACARTIA LONGIREM
ACARTIA SP
CALANUS SP
EPILABIDOCERA
170.5
62.0
155.0
10.9
5.5
65.7
16.4
79.4
44.7
54.6
29.8
39.7
0
0
0
38.1
27.4
16.4
0
0
0
16.4
0
0
64.5
0
0
62.0
108.5
93.0
57.2
19.0
5.0
62.U
95.3
38.1
152.4
31.0
0
0
133.3
27.4
G
76.6
0
0
39.7
0
0
C
19.3
0
0
0
U
U
0
J
19.9
5.0
0
OITHONA SIMILIS
19.0
0
C
62.0
0
U
176.5
1813.5
4210.6
342.9
2228.8
NAOPLIUS
1674.1)
573.5
87.6
75.4
0
0
20-9.5
0
0
32.1
GAMMARIO AMPHIPO
0
0
0
C
0
0
HYPERIID AM3HIPO
ANNELID LARVAE
0
6
0
0
0
0
62.0
31.0
465.0
0
0
0
0
0
0
0
114.3
0
0
0
0
0
0
0
0
6
0
0
0
0
G
0
J
0
0
0
0
0
0
0
0
0
0
0
PSEUDOCALAN'JS
COPEPUD
BARNACLE CYPRIS
BARNACLE NAUPLIU
CHAETOGNATHA
PUDON LEUCKARTI
HERMIT CRAB LARV
CRUSTACEAN EGGS
DECAPOD LARVAE
GASTROPOD LARVAE
MEDUSAE
31.0
15.5
232.5
62.0
108.5
0
U
38.1
0
38.1
57.2
190.5
304.8
76.2
19.0
0
0
0
0
0
0
5.5
5.5
,.5
1u.5
142.3
5.5
16.9
5.5
186.1
229.9
32.8
16.4
0
0
60.2
355.8
G
0
0
0
94.3
908.6
0
983.1
99.3
0
0
0
0
0
0
0
0
u
0
0
0
0
0
u
0
0
0
u
0
0
G
0
0
G
0
0
0
0
0
0
0
0
0
0
0
0
0
0
C
0
0
0
19.9
0
0
0
0
5.0
0
0
0
0
0
0
0
0
0
0
0
0
THE FOLLUWINS TABLE LISTS THE FRACTION OF
ACARTIA CLAUSI
ACARTIA LONGIREH
ACARTIA SP
CALANUS SP
EPILABIDJCERA
OITHONA SIMILIS
PSEUDOCALANJS
COPEPOB NAUDLIUS
GAMMARID AMPHIPO
HYPERIID AMPHIPO
ANNELID LARVAE
BARNACLE CY?RIS
BARNACLE NAJPLIU
CHAETOGNATHA
P000N LEUCKARTI
HERMIT CRAB LARV
CRUSTALEAN EGGS
DECAPOO LARVAE
GASTROPOD LARVAMEDUSA`
.0274
.0050
.0130
ulu0
TOTAL STATION ABUNDANCE-
.0288
0
0
.0249
.0103
.0174
0
0
0
G
.0149
u
0
0
0
0
0
0
.004b
.0157
.6022
.0106
.2687
u
0
0
0
.0384
0
u
.3274
.0920
.2910
.0022
.4966
.22629
.3309
.0264
.1559
0
3
.0247
.u404
0
3
0
0
0
0
0
0
0
0
.0366
.0024
.0080
.394.0398
0
C
3
0
0
0
G
U
3
0
0
0
0
0
C
0
G
0
0
0
3
0
0
0
0
0
0
0
3
0
0
3
0
0
G
0
0
0
0
G
0
0
0
C
0
.0093
.0020
C
0
0
0
.0100
.0112
.0045
.0067
.0022
.0181
J
0
J
.0045
0
0
.JC50
.0746
0
C
0
0
0
0
0
.0135
0
0
J
0
C
0
0
3
0
0
0
0
J
0
3
0
0
0
0
0
0
.0050
.0025
.0373
V
0
0
0
.0045
.0067
.0225
.0360
.3100
.0174
0
u
U
0
0
G
0
.0090
.6022
.0120
.0072
.0048
.0024
c
G
.0072
.0072
C
0
.0120
.0120
.0159
.0259
0
.3336
0
0
.
0
0
0
0
.0026
0
0
.0378
.3645
0
0
0
0
0
0
.0024
.3C2.
.0048
.0o24
.0024
.3046
.6024
.0815
.1007
.0144
.0072
.0319
.0179
C
.3320
.0219
0159
0
0
u
0
0
0
0
STATIONS Ov 03/08/72
DATUM
.2C
.2S
9.d0U
10.800
33.7480
9.800
33.7770
33.7820
10.500
33.7obu
SURFACc TEMP.
SURFACE SALINITY
BOTTOM TEMP.
BOTTOM SALINITY
FOREL NO.
SECCHI RcADING
7
7
:.5
5.u
THE FOLLOWING TABLE LISTS ABSOLJTE AUUNOANCES
(NUMBER JF INDIVIDUALS PER CUBIC 4LTER OF WATER FILT_RcD)
ACARTIA CLAJSI
ACARTIA LONuIREM
ACARTIA SP
CALANUS SP
CENTROPASES MCMU
OITHONA SIMILIS
PSEUDOCALANJS
COPEPOD NAUPLIUS
BARNACLE GYPRIS
BARNACLE NAUPLIU
PODON LEUCKARTI
CRAB ZOEA
CRUSTACEAN EGGS
GASTROPOD LARVAE
FEMALES
MALES
1MM5
FEMALES
MALES
IMMS
X40.3
86.4
64.6
14.4
144.1
100.9
381.6
10.9
267.1
38.2
279.1
16.4
0
0
43.2
G
0
27.3
0
7.2
36.1
C
u
16.4
0
7.2
u
0
u
0
0
U
27.3
u
0
1462.4
223.3
43.2
y72.:i
691.5
147.2
065.1
G
0
38.2
0
0
3
0
0
u
u
0
0
0
u
0
14.4
0
0
0
0
0
0
9
50.w
5.5
0
0
0
0
0
7.2
0
0
0
G
3
21.6
16.4
43.b
60.0
0
FEMALES
MALES
IMMS
FEMALES
MALLS
IMMS
THE FOLLOWING TABLE LISTS THE FZACTION OF TOTAL STATION ABUNDANCE
ACARTIA CLAUSI
ACARTIA LON,IRt1
ACARTIA SP
-
.1407
.0225
.0109
.3u38
.0375
.0263
.1397
.0040
.1978
.1018
.0113
.0140
0
0
.0694
0
0
.0060
.0100
.6001
0
L
0
1
.0100
.2495
0
0
.0539
.2435
0140
0
J
0
0
0
u
0
0
0
0
.0019
.3u19
.3355
u
PSEUDOCALANLJS
COPEPOD NAUPLIUS
BARNACLE CYPRIS
BARNACLE NAJPLIJ
.3809
.0532
.2533
PUDUN LEUCKARTI
CRAB ZOEA
CRUSTACEAN :GGS
GASTROPOD LARVAE
CALANUS SP
CENTROPACES MCMU
OITHONA SIMILIS
.0113
0
0
0
0
u
0
0
.7038
0
0
u
u.
a
0
C
C
0
J
0
3
0
0
0
J
.u131
.0019
:0060
.u160
.0220
.0020
0
J
0
0
SAMPLE AT STATION .4
STATIONS ON 03/17/72
NOT QUANTITATIVE
DATUM
SURFACE TEMP.
SURFACE SALINITY
BOTTOM TEMP.
BOTTOM SALINITY
FOREL NO.
SECCHI READING
1.5
1.u
.4
12.li0
11.940
33.6340
12.100
33.5750
12.100
12.100
33.5910
11.850
33.5976
33.6080
2.0
33.5840
11.700
33.593u
0
33.5820
8
9
7
7
4.6
4.3
4.5
4.5
THE FOLLOWING TABLE LISTS ABSOLUTE ABUNUANCES
(NUMBER OF INOIVIUUALS PEk CUBIC0 METER OF WATER FILTERED)
ACARTIA CLAUSI
ACARTIA LONGIREM
ACARTIA SP
CALANUS SP
OITHONA SIMILIS
OITHONA SPINIROS
PSEUDOCALANUS
COPEPOD NAUPLIUS
HARPACTICOID
GAMMARID AMPHIPO
ANNELID LARVAE
BARNACLE CYPRIS
BARNACLE NAUPLIU
CHAETOGNATHA
P000N LEUCKARTI
CRAB ZOEA
HERMIT CRAB LARV
PORCELAIN CRAB Z
CRUSTACEAN EGGS
DECAPOD LARVAE
EUPHAUSIID NAUPL
EUPHAUSIID CALYT
GASTROPOD LARVAE
MEDUSAE
MYSID LARVAE
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
30.0
11.0
34.0
24.0
137.6
47.1
86.9
68.8
119.5
133.3
173.9
61.4
112.5
51.1
201.2
68.2
153.7
153.7
202.3
226.5
129.4
0
0
30.7
u
0
4.0
0
0
17.0
0
0
12.1
0
u
60.7
0
0
0
0
0
0
0
10.2
37.5
52.6
0
28.3
32.4
4.u
0
0
0
0
3.4
0
0
0
0
0
0
C
0
0
0
0
0
4.0
64.7
0
0
0
0
33.0
30.0
1.0
7.0
0
0
57.9
0
C
29.0
25.3
7.2
3.6
119.5
3.6
3.6
0
0
0
J
0
0
0
0
8.0
0
0
0
0
0
6.0
3u.0
1.0
3.0
1*.0
0
J
0
0
0
C
0
0
0
0
0
108.6
0
0
0L
0
0
u
G
0
G
1.0
15.0
58.0
1.0
49.0
0
0
2.0
18.0
1.0
3.0
0
31.0
2.0
0
2,42.7
0
21.7
0
0
85.3
3.4
3.4
64.8
0
0
3.4
0
0
0
u
0
0
3.4
6.8
78.4
159.3
G
u
150.0
0
0
186.1
0
0
0
G
0
u
0
G
u
0
0
195.5
0
J
0
0
0
0
u
95.5
27.3
0
18.1
G
C
0
0
0
0
0
u
0
0
0
14.5
G
0
0
0
0
0
0
10.2
37.5
0
0
0
0
0
0
0
0
10.9
0
0
0
0
0
0
G
0
65.2
0
D
0
0
0
0
0
0
G
0
27.3
3.4
0
G
83.3
6
0
0
0
36.2
36.7
0
0
0
0
0
0
0
3.6
40.9
3.4
0
0
0
0
0
101.1
4.0
8.1
16.2
12.1
8.1
32.4
0
0
0
0
0
0
0
0
32.4
G
0
0
16.2
0
0
0
0
0
0
0
G
0
0
THE FOLLOWING TA3Lc LISTS THc FRA3TIUN OF JJTAL STATION ABUNDANCE
ACARTIA 3LAJSI
.333
ACARTIA LON ;IREM
ACARTIA 3P
-
.3752
0
0
CALANUS SF
OITHONA SIMILIS
OITHONA 3PINIRCS
PSEUDOCALANUS
COPEPOD NAUPLIUS
HARPACTICOIO
GAMMARIO AMPHIPO
ANNELID LARJAE
BARNACLE CYPRIS
BARNACLE NAJPLIU
CHAETOvNATHA
PODON LEUCKARTI
0
0
.0023
.0159
.3182
0
0
0
0
6
.0137
L3od
.6319
GRAB ZUEA
HERMIT CRAB LARV
PORCELAIN CRAB Z
CRUSTAUEAN EGOS
OECAPOO LARVAE
EUPHAUSIID NAUPL
LUPHAUSIIU U4LYT
GASTROPOD LARVAL
MEDUSAE
MYSID LARVAE
.u273
.3683
.0774
.0547
.0844
.0289
.u533
.0422
G
0
0
U
U
.0156
.0044
.0022
.0733
.0323
U
u
.0022
0
C
0
.3023
0
O
.342
.0683
.117.
.0413
.0757
.3344
0
G
0
.0733
.0800
.0356
.0173
0
G
J
0
J
a
.0133
0
0
0
U
0
0
0
0
0
u
0
J
.0573
.GL23
.0323
.043E
.G023
.0023
.0046
.0528
.1639
.0841
.084d
.1116
.1339
0
G
0
.1353
.0459
.3206
.0115
3
U
.1250
.0714
.0022
.0067
C
0
.0335
0
0
0
J
0
0
0
..069
.0252
.2022
.0290
0
0
.0150
.0179
0
0
u
.0023
u
0
0
0
G
u
0
0
0
0
0
0
0
G
0
0
C
0
.0022
.0357
.1027
0
0
C
u
.1321
.0023
.1110
U
0
.0022
.0022
.3667
.0978
0
3
6
u
J
G
0
0
0
u
.1260
0
0
0
6
0
.3111
0
0
C
1
.Ub42
.3183
0
C
0
0
0
G
C
u
G
0
0
.0045
.0410
.OG23
OOb8
0
U
.0067
C
0
0
0
0
.0089
.6069
0
G
0
.6252
0
6
u
u
G
G
0
C
0
0
0
0
.0400
0
J
0
0
0
6
J
.0706
0
u
J
.0183
.0023
.0558
.0022
.0045
.0089
.0067
.3C+
.0179
0
0
0
0
.0511
0
.OU46
0
0
0
.0206
.0275
0
0
.0222
0
0
0
6
G
J
.0023
U.
0
0
0
O
0
0
0
0
0
0
0
0
0
0
0
0
0
0
G
0
.0179
0
0
0
0
.0089
0
0
0
1
3
C
0
SAMPLE AT STATION 3.0
STATIONS ON 03/17/72
NOT QUANTITATIVE
DATUM
2.5
SURFACE TEMP.
SURFACE SALINITY
BOTTOM TEMP.
BOTTOM SALINITY
FOREL NO.
SECCHI READING
.2N
3.0
.2C
12.130
33.5340
11.oUC
33.5676
11.850
33.549u
8.400
33.6640
6
6
7
7
5.0
o.G
3.5
4.',
12.100
33.6040
11.803
33.6013
12.100
33.6363
11.900
33.6,;36
THE FULLOWING TABLE LISTS ABSOLUTE ABUNDANCES
(NUMBER OF INDIVIDUALS PEP CUOIC METER OF WATER FILT_PED)
ACARTIA CLAUSI
ACARTIA LONuIREM
ACARTIA SP
CALANUS SP
CENTROPA6ES MCMU
OITHONA SIMILIS
PSEJOOCALANUS
COPEPOJ NAU!3LIUS
FEMALES
MALES
IMMS
FEMALES
MALES
282.2
437.5
190.5
412.8
254.0
1C.G
43.3
0
U
0
0
U
35.3
21.2
0
0
'+09.2
IMMS
FEMALES
MALES
10.0
8.0
44.0
35.1
78.3
24.3
48.6
0
38.0
12.0
0
0
G
0
4.3
6
G
145.8
21.6
-21.6
2.7
16.2
13.8
167.4
6
G
IMMS
FEMALES
MALES
IMMS
91.8
197.6
43.4
139.8
351.9
24.1
192.8
0
6
0
0
2.7
0
4.8
9.6
38.6
4.9
0
67.5
0
0
2.7
13.5
J
4.8
33.7
0
0
0
0
115.7
4.3
0
0
G
0
0
0
9
3
0
0
0
0
0
C
0
0
0
0
0
0
0
0
0
3
G
0
G
G
U
77.6
77.6
112.9
0
0
0
J
35.3
12G.u
5.0
34.0
0
0
13.u
30.0
13.0
C
0
0
0
0
0
0
0
0
0
J
0
0
0
0
0
6
0
3
0
0
0
J
0
0
0
0
0
3
0
0
0
0
2.0
5.6
15.0
1.6
u
CRAB ZOEA
HERMIT CRAB LARV
42.3
134.1
204.6
14.1
42.3
2.7
8.1
10.8
108.0
56.4
0
J
6
0
0
9.6
139.3
149.4
197.6
33.7
6
G
0
0
G
G
0
C
0
0
PORCELAIN CRAB Z
1.0
0
0
1.0
0
0
C
G
0
0
0
0
29b.4
0
0
0
100.0
0
0
2.7
0
0
0
0
7.1
0
0
0
J
G
0
0
0
0
u
0
0
0
0
120.5
0
0
0
1.0
37.8
0
0
0
4.0
7.0
19.3
4.8
0
0
0
0
0
0
0
0
0
0
0
G
0
0
u
0
0
43.4
0
0
0
0
0
0
32.4
0
0
0
0
0
0
0
37.8
57.8
0
2.L
3.0
0
0
0
0
GAMMARIO AMPHIPO
HYPERIID AMPHIPJ
ANNELID LARVAE
BARNACLE CYPRIS
BARNACLE NAUPLIU
POOON LEUCKARTI
CRUSTACEAN EGGS
DECAPOO LARVAE
EUPHAUSIIO NAUPL
EUPHAUSIIO CALYT
GASTROPOD EGGS
35.3
GASTROPOD LARVAE
42.3
56.4
MEDUSAE
C.
43.4
0
THE FOLLOWING TABLt LISTS THE FwACTIUN OF TOTAL STATION ABUNDANCE
ACARTIA ;:LAJSI
ACARTIA L0NCIRE1
ACARTIA SP
CALANUS SP
CENTROPAGES MCMU
OITHONA SIMILIS
PSEUJOCALANUS
C3PEPOD NAUPLIUS
GAMMARID AMPHIPO
HYPERIID AMPHIPO
AN'JELIO LARVAE
3ARNACLE CYPRIS
BARNACLE NAUPLIU
P3)UN LEJCKARTI
CRAB ZOEA
HERMIT CRAB LARV
PORCLLAIN CRAB Z
CRUSTACEAN EGGS
OECAPOD LARVAE
EUPHAUSIIO NAUPL
EUPHAUSIID CALYT
GASTROPOD EjGS
GASTROPOD LARVA=
MEDUSAS
.0826
.1281
.-» 8
.13i-
J
u
0
.0144
.1198
.0103
.0062
.0245
.1654
.u245
.1078
0
u
C
0
.0342
.0763
.G237
.0474
0
0
u
.6196
.69.1
.0294
.0093
6
6
0
C
0
0
0
J
.6123
.0833
.0895
.1421
.0211
.0211
.0026
.0928
.0204
.0656
.0113
U
0
0
0
.6317
0
0
.0026
.3132
u
.0023
.0158
.6543
6
0
.0023
0
0
U
6
0
.0023
6
0
.3319
.3735
.0319
6
J
.0026
.0155
.3105
.1632
0
0
0
0
C
0
6
0
0
J
0
0
U
0
0
6
0
o
6
0
0
J
U
0
0
0
u
0
.3124
.G393
.3599
.0041
.0124
u
0
6
0
G
6
0
U
L
0
0
U
a
6
U
U.
U
0
.0227
.0227
.0331
C.
.
6
J
.,,3
.0351
.0103
5
3
0
0
0
.0649
.0123
.0368
.0025
.GG25
.0025
.2451
.0095
.0172
.0025
,,
u
6
0
0
6
0
.0049
.3074
.J568
.0021
0
.0124
.Olb5
G
0
.i 52
.0905
.6045
.0181
.0023
0
.0626
.0679
.0105
.1053
.3642
0
3
0
0
0
0
3
.0045
.ObSc
.0701
.6923
.0158
C
0
0
0
0
i
0
0
0
0
u
0
0
0
0
J
u
0
.0626
0
0
0
0
0
G
6
0
0
0
G
.0368
C
.0090
.0023
C5bo
U
G
0
6
0
J
6
0
C
G
0
u
L
6
G
u
0
0
0
0
0
6
3
0
0
6
0
.0316
.0368
0
0
.6264
.0271
.6204
0
0
J
6
G
C
0
3
0
0
G
0
6
STATIONS
04 ;:8/17/72
.2S
DATUM
SURFACE TEMP.
SURFACE SALINITY
BOTTOM TEMP.
3OTTOM SALINITY
12.2uu
33.7650
11.950
33.5970
FOREL NO.
SECCHI R=AGING
7
4.0
THE FGLLGWING TABLE LISTS ABSOLUTE ABUNDANCES
(NUMBER OF INDIVIDUALS PER CUBIC MITER OF WATER FILTERED)
FEMALES
ACARTIA CLAJSI
ACARTIA LONSIREM
ACARTIA SP
CALANUS SP
MALES
IMMS
13.1
2.9
24.7
26.1
16.9
36.3
0
0
0
0
18.9
16.9
G
CENTROPAvES MCMU
OITHONA SIMILIS
PSEU000ALANUS
COPEPOD NAUPLIUS
HARPACTICJIO
ANNELID LARVAE
BARNACLE CYPRIS
BARNACLE NAJPLIU
0
1.5
27.5
14.5
94.3
1.5
10.2
17.4
75.4
G
0
0
1G.2
0
0
0
0
u
j
PODON LEUCKARTI
52.2
CRUSTACEAN EGGS
EUPHAUSIID JAUPL
GASTROPOD EGGS
GASTROPOD LARVAE
MtOUSAE
2.9
-37.7
24.7
21.8
23.2
0
O
0
0
0
0
u
0
G
0
0
0
0
0
0
0
FEMALES
MALES
IMMS
FEMALES
MALLS
IMMS
FEMALES
MALES
IMMS
THE FOLLJWIVG TA3LE LISTS THE FkACTION OF TOTAL STuTIUN At3JNDANCE
ACARTIA CLAJSI
ACARTIA LCNJIREM
ACARTIA SF
-
CALANUS SP
CENTROPAGES MCMU
OITHONA SIMILIS
PSEJDOCALANJS
COPEP09 NAUPLIUS
HARPACTICOI7
ANNELID LARIAE
3ARNACLE CY2RIS
BARNACLE NAJPLIU
POOON LEUCKARTI
LRJSTA4EAN LOGS
EUPHAUSIIC 4AUPL
GASTROPOD EGGS
GASTROPOD
MEDUSAE
LARVAL
.1222
.0444
.J049
.0420
.0321
.0uI7
0
C
0
U
0
.0025
.J469
.0247
.1b05
.0025
.0173
.0296
.1284
.0689
.0049
.0642
.6420
.0370
.0395
.0321
.0321
0
U
0
U
.u173
u
u
J
0
0
u
6
u
u
u
0
0
U
u
0
0
u
0
0
0
0
u
STAIIUNS ON 03/22/72
DATUM
1.
.Y
SURFACE TEMP.
14.530
32.9360
13.930
33.1310
SURFACE SALINITY
BOTTOM TEMP.
30TTOM SALINITY
FOREL NO.
SECLHI READING
1.5
14.630
33.0490
12.730
33.2263
6
14.550
32.8990
11.350
33.341G
14.70G
33.066
11.650
33.296u
7
t.5
2.G
6.5
0
5
6.J
7.0
THE FOLLOWING TABLE LISTS ABSOLUTE ABUNDANCES
(NUMBER OF INDIVIDUALS PER CUBIC MITER OF WATER FILTERED)
AGAr(TIA CLAJSI
ACARTIA LONGIRE'1
ACARTIA SP
CALANUS SP
CENTROPAGES MCMU
UITHONA SIMILIS
PSEUDOGALANJS
COPEPOD NAUPLIUS
ANNELID LARVAE
BARNACLE CYPRIS
BARNACLE NAJPLIU
PODON LEUCKARTI
CRAB ZOEA
HERMIT CRAB LARV
PORCELAIN CRAB Z
CRUSTACEAN EGGS
FEMALES
MALLS
IMMS
FEMALES
MALLS
IMM3
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
35.4
10.4
47.9
1i.4
713.9
517.5
108.4
721.3
55.4
8.6.2
165.1
660.5
82.6
9391.2
+2.0
1816.3
81.5
140.7
59.3
140.7
L
484.9
1399.9
66.7
0
L
29.2
u
u
7622.4
1398.6
279.7
G
U
268.3
0
0
G
0
0
L
0
0
20.6
0
0
0
0
2.1
6.3
0
0
3
28.0
0
32.6
22.2
88.9
414.3
J
u
0
L
C
0
20.6
20.6
7.4
u
u
u
L
u
C.
U
0
0
0
0
0
26.C
7.4
0
J
u
u
0
u
23.6
u
0
L
0
u
0
41.3
0
0
0
0
0
0
u
20.t
G
C
J
u
0
0
0
0
0
0
29.6
0
0
0
0
0
0
0
0
0
G
G
,;
0
0
0
8.3
u
0
42.0
0
0
L
0
C
3
0
12.5
0
0
0
0
0
0
0
0
3
3
u
0
14.0
14.0
20.6
20.6
20.6
u
U
0
0
u
0
0
0
J
20.6
0
0
0
0
0
u
0
C.
0
0
0
0
0
U
0
0
G
0
0
0
0
0
0
0
0
0
0
0
0
0
0
20.6
20.6
0
G
0
0
0
28.0
C
u
20.6
0
0
7.4
0
0
0
0
0
0
0
0
0
0
20.6
0
G
0
0
4.2
2.1
GASTROPOD LARVAE
8.3
0
0
0
0
u
2.1
0
3
OIKOPLEURA
0
0
20.8
FISH EGGS
GASTROPOD SGS
MEDUSAE
G
0
0
28.0
14.0
14.u
0
7.4
0
THE FOLLOWI41i TA;3Lt LISTS THL FRACTION OF TOTAL STATIOi4 ABUNDANCE
.u344
.0101
.u466
.3101
J
0
CENTROPAGES MCMU
a
OITHONA SIMILIS
0
PSEUDOCALANJS
0
G
J
J
0
0
.u326
0
0
0
0
u
.0039
ACARTIA CLAJSI
ACARTIA LONSIREM
ACARTIA SP
CALANUS SP
COPEPOD NAUPLIUS
ANNELID LARVAE
BARNACLE CYPRIS
BARNACLE NAUPLIU
POOON LEUCKARTI
CRAB ZOEA
HERMIT CRAB LARV
PORCELAIN CRAB Z
CRUSTACEAN OGGS
FISH EGGS
GASTROPOD ESGS
GASTROPOD LARVAE
MEOUSAr-
OIKOPLEURA
.0476
.0039
0
.6984
.1053
.0233
0
0
0
G
CU20
.6661
C
3
.6621
.0101
G
.7014
.1287
.0257
0
C
.6994
.1333
.0197
0
0
C.
,
0
u
.6026
0
0
3
0
J
.0015
.0015
G
0
G
G
0
0
0
.0015
G
C
0
G
.5669
.0051
0
u
0
0
0
U
.0485
.0061
3015
.0061
.0275
.047t
.0200
.0475
U
0
0
0
. 0075
. 0300
.0025
.1650
.4725
.0225
0
.
1400
0
0
U
6
. UG25
0
G
0
C
0
0
0
G
0
0
C
0
0
3
.0103
0
0
U
0
0
0
0
0
0
u
0
0
.U121
G
C
0
u
.062E
G
0
0
0
0
0
0
0
6
0
.0013
.0013
.0036
.0015
.0015
.0015
.0015
3
J
C.
U
0
0
0
0
0
0
G
0
0
.3G4U
.0015
0
0
0
0
0
0
U
J
6
0
3
0
0
0
0
0
u
0
0
0
G
0
&
G
u
0
0
U
0
0
0
0
0
G
0
0
u
G
0
0
0
.0025
0
0
0
0
u
0
0
0
0
0
0
u
.0025
0
0
.Uu15
0
0
0
.3031
.0202
.0020
.0081
U
u
.3020
G
0
.0026
.0u13
.0613
.0&15
.0015
.0015
G
0
STATIONS ON 03/22/72
DATUM
2.5
SURFACE TEMP.
SURFACE SALINITY
BOTTOM TEMP.
BOTTOM SALINITY
FORLL NO.
SECCHI READING
4.0
3.0
5.0
14.b50
15.200
32.7440
15.000
32.5010
15.150
32.4J20
8.300
33.6640
32.3970
8.100
33.7080
9.450
8.450
33.5330
33.6120
5
5
5
5
10.0
10.5
7.5
7.5
THE FOLLOWING TABLE LISTS ABSOLUTE ABUNDANCES
(NUMBER OF INDIVIDUALS PER CUBIC MLTER OF WATER FILT_RED)
FEMALES
ACARTIA CLAUSI
ACARTIA LONGIREM
ACARTIA SP
CALANUS SP
CENTROPAGES ICMU
EUCALANUS SP
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
3b.5
-2 1.1
276.2
J
0
321.3
235.7
42.2
4.4
0
1285.2
21.9
65.7
613.4
714.6
1.7
3.4
408.9
623.4
222.9
41.2
1566.0
76.0
15.2
84.4
98.7
44.2
190.0
0
0
0
182.3
40.5
0
0
35.4
0
3.4
u
0
68.4
3.4
3.4
1.5
6.8
2.1
2.9
2.9
0
0
0
0
0
0
0
38.0
53.2
0
0
0
u
0
0
1
0
0
0
1.5
1.5
0
0
0
0
7.4
73.0
7.3
146.0
0
U
7.3
21.9
U
0
15.2
0
J
6
0
0
0
0
0
7.6
0
0
6
0
0
0
4.4
42.7
0
0
0
0
7.3
1.7
28.7
0
0
0
U
0
0
7
0
0
0
0
0
0
0
0
0
0
0
3.4
0
0
J
0
0
0
0
0
0
1. 5
0
0
0.
0
0
0
C
0
0
J
0
0
0
0
J
7.6
7.6
0
0
0
C
0
0
0
0
43.8
u
0
76.0
0
J
55.7
0
0
6
0
0
U
J
0
0
0
0
CRAB ZOEA
14.7
2. 3
0
0
0
0
0
0
0
0
0
0
0
PORCELAIN CRAB Z
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
25.0
28.0
14.7
0
0
0
0
OITHONA SIMILIS
PSEUDOCALANUS
COPEPOD NAU?LIUS
UNIDENT CALANOID
HARPACTICOID
HYPERIID AMPHIPO
ANNELID LARVAE
BARNACLE CYPRIS
BARNACLE NAJPLIU
P000N LEUCKARTI
CRUSTACEAN EGGS
ECHINODERM LARVA
EUPHAUSIID NAUPL
EUPHAUSIID CALYT
GASTROPOD LARVAE
MEOUSAE
OIKOPLEURA
U
21.9
7.3
7.3
365.1
0
0
0
0
U
0
0
0
0
0
0
0
0
0
0
0
43.8
7.3
36.5
22.8
68.4
38.0
0
7.6
30.4
0
0
0
0
0
91.2
0
0
0
1.7
1.7
5.1
3.4
25.3
13.5
10.1
1.7
42.2
0
30.9
J
0
0
0
0
0
0
0
0
39.8
0
0
0
THE FOLLOWIJG TABLE LISTS THE FRACTION OF TOTAL STATION ABUNDANCE
ACARTIA CLAUSI
ACARTIA LONGIREM
ACARTIA SF
-
CALANUS, SP
CZNTROPAGES MCMU
EUCALANUS SP
OITHONA SIMILIS
PSEUDOCALANUS
COPEPOD NAJPLIUS
JNIDENT CALANUIJ
HARPACTICOID
HYPERIID AMPHIPO
ANNELID LARVAE
BARNACLE CYPRIS
BARNACLE NAJPLIU
.0094
.0132
.1057
.0189
.0u19
.0377
.0698
.3321
.0057
.0170
.1585
.0630
0
0
0
.0101
.0141
.0626
.4162
.0202
.0040
.0192
0
.1899
0
.1657
0
0
C
0
.0021
.2767
.0042
.1048
G
0
.0042
.0042
.0069
.1537
.0608
0
.0524
.2264
.0503
u
0
0
. 0042
0
.0084
U
0
.0042
.2959
.0550
.002 3
.0046
.0046
.0046
.0023
0
-u
.0115
0
0
.0019
0
0
0
G
0
0
.0057
0
0
.0040
0
0
G
0
0
0
0
.0057
G
L
C
.0021
0
0
0
0
.0061
.0020
0
3
.0356
.0023
.0069
0
0
0
0
u
.0019
.0665
0
0
0
J
0
0
0
0
0
0
0
0
u
0
0
0
.0042
0
0
0
0
0
0
0
0
0
0
0
.0019
0
0
0
0
0
0
0
0
0
0
J
0
0
0
0
0
0
0
C
.0113
0
0
J
0
0
0
0
.0020
.0620
.0202
.0023
0
0
U
J
0692
C
0
.
0223
0
0
0
0
0
0
0
0
0
G
0
0
0
0
0
0
0
0
0
0
0
0
0
u
0
0
.0943
.0063
u
ECHINODERM LARVA
EUPHAUSIID NAUPL
EUPHAUSIID CALYT
.0182
0
CRUSTACEAN EGGS
.0019
G
. OG21
.0021
.U046
U
0
0
G
0
0
0
0
0
C
0
0
0
0
.0101
.6482
0
J
0
0
0
J
0
0
0
0
J
0
0
0
G
.039J
0
0
0
.0113
.0019
.0094
0
0
GASTROPOD LARVAE
0
0
0
0
C
0
.6436
.0229
0
J
J
0
0
0
.0020
.0081
C
0
0
G
0
0
0
0
0
0
0
0
0
0
0
0
.0619
0
0
.0242
0
0
0
PUDON LEUCKARTI
CRAB ZOEA
PORCELAIN CRAG Z
MEDUSAE
OIKOPLcURA
.
.0u42
.0314
.0168
.0126
.0021
.0524
0
0
0
STATIONS ON 03/22/72
DATUM
.2N
14.200
32.983u
SURFACE TEMP.
SURFACE
BOTTOM
BOTTOM
SALINITY
15.506
33.0170
14.900
33.0860
1+.350
33.1250
TEMP.
SALI41TY
FOREL NO.
SEGCHI READING
.2S
.2C
15.40G
0
14.300
33.1020
7
9
9
5
5.0
5.0
THE FOLLOWING TABLE LISTS ABSULUTE ABUNJANCES
(NUMBER OF INDIVIDUALS PER CUBIC METER OF WATER FILTERED)
ACARTIu CLAUSI
ACARTIA LOiy,;IREM
ACARTIA SP
-
CALANUS SP
CENTRUPASES MCMU
EURYTEMORA
UITHUNA SIMILIS
PSEUOOCALANUS
COPEPOD AAUPLIUS
HARPACTICOID
HYPERIID AMPHIPO
ANNELID LARVAE
BARNACLE CYPRIS
BARNACLE NAJPLIU
PODON LEUCKARTI
CRUSTACEAN EGGS
ECHINODERM LARVA
EUPHAUSIID CALYT
FISH EGGS
FORAMINIFERA
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
37.7
13.7
70.6
13.7
16.8
9.9
2.3
0
17.6
3.8
121.1
45.3
6.1
13.5
72.2
47.7
0
G
647.1
47.9
30.8
0
0
0
0
0
0
G
u
0
0
J
0
0
2.4
1.2
0
0
u
C
0
0
0
0
1.2
13.5
0
.8
0
3
6
0
0
6.3
0
U
1.5
0
1.5
8.6
0
0
0
0
0
0
0
0
0
0
0
2.4
1.2
0
0
U
0
0
1.2
0
C
0
0
0
0
0
0
0
G
0
0
0
0
0
0
0
0
U
0
.8
.8
0
3.4
0
0
0
0
10.3
0
0
U
0
0
0
4.6
167.3
22.9
u
3.4
0
0
0
0
0
27.4
0
it
0
0
0
3
0
0
0
u
0
0
0
0
0
513.6
34.2
0
0
0
GASTROPOD EGGS
GASTROPOD LARVAE
MEDUSAE
10.3
10.3
OIKOPLEURA
13.7
0
0
0
.8
0
C
3
0
0
C
3
1.5
0
3
6.1
3.1
C
0
0
7.6
.8
0
0
0
0
26.9
1.2
2.4
0
0
0
0
0
0
0
0
0
0
0
0
0
13.0
11.5
2.3
0
2.4
156.5
8.6
1.2
2.4
1.2
12.2
6.1
8.6
0
0
0
0
0
0
0
0
0
0
0
0
0
FEMALES
MALES
IMMS
THE FO LLOWIYG TABLE LISTS THE FRACTIUN OF TOTAL STATION ABUNDANCE
ACARTIA CLA'JSI
ACARTIA LON;IRE1
ACARTIA SP
CALANUS SP
CENTROPAGES ACMU
EURYTEMORA
OITHONA SIMILIS
P SEUDOCALANJS
COPEPOD 4AUPLIUS
HARPACTICOID
HYPERIID AMPHIPO
ANNELID LARVAE
BARNACLE CYPRIS
BARNACLE NAJPLIU
P03ON LEUCKARTI
CRUSTACEAN EGGS
ECHINODERM LARVA
EUPHAUSIID CALYT
FISH E.GS
FORAMINIFERA
GASTROPOD E3GS
GASTROPOD LARVAL
MEOUSAE
OIKOPLEURA
.0248
.0090
.0519
.0090
0
J
.0545
.0322
.0074
0
. 0124
0
.4266
.0316
.0203
0
0
0
G
0
0
0
G
U
U
G
C
0
0
U
C.
.0021
.0042
.0021
.0234
0
0
G
.0053
0
.0145
0
G
G
0
0
0
C
0
J
. 0042
.0021
G
0
U
C
0
0
0
G
0
0
0
0
.0569
.21u2
.
0796
.0106
.
0234
.
.1253
.3 6 28
0
U
U
U
0
0
.0045
u
0
.3625
.0050
0
0
0
0
U
0
0
U
u
.0025
.0025
0
0
G
.U068
0
0
0
U
0
0
0
U
0
U
0
.0021
.0042
.2718
0
0
0
U
. 01 4 9
0
0
0
0
u
.
0021
0
.0181
C
U
0
0
0
0
G
0
0
0
0
0
0
0
C
0
0
.0042
.0467
.0021
0
0
.0149
.5421
.0743
.0L50
.0198
.0699
0
C
0
0
0
u
.
00 4 2
0
0
0
0
0
.0068
.0023
.3386
.0226
.0023
0
.3U68
.0393
0
.
0025
0
J
U
.0248
.0025
0
0
G
0
0
0
0
0
.0021
U
0
0
0
U
0
0
U
.G212
0
0
0
0
0
0
C
0
0
0
.3421
.0371
.0074
.Ui06
.0149
0
0
u
0
STATIONS ON 03/08/72
.4
DA TUM
SURFACE TEMP.
SURFACE SALINITY
BOTTOM TEMP.
BOTTOM SALINITY
FORLL NO.
SECCHI READING
.2N
.2S
.2C
12.400
33.2650
U
0
0
0
33.2750
0
11.901'
U
U
0
33.2680
0
0
0
0
C
0
0
0
0
0
0
THE FOLLOWING TABLE LISTS ABSOLUTE ABUNDANCES
(NUMBER OF INDIVIDUALS PER CUBIC METER OF WATER FILTcREO)
ACARTIA CLAJSI
ACARTIA &.ONJ-!REM
CALANUS SP
CENTROPAGES MCMU
OITHONA SIMI-IS
PSEUJOCALANUS
HARP4CTICOIO
ANNELID _ARVAE
AQUATIC MITE
BARNACLE CYoRIS
3ARNACLE NAJPLIU
P000N LEUCKARTI
DECAPOD LARVAE
FORAMINIFERA
GASTROPOD E 55
GASTROPOD LARVAE
ISOPODA
OIKOPLEURA
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
iMMS
4583.0 12221.3
0
265.7
4606.0
1526.6
4000.6
991.1
991.1
2265.3
C
0
0
0
66.4
C
6
0
0
0
0
0
0
0
C
0
0
U
0
U
0
0
131.6
0
0
212.4
0
0
425.0
U
0
265.7
0
26.3
131.6
0
70.8
424.7
0
0
0
U
1
0
0
0
0
0
0
FEMALES
MALLS
IMMS
FEMALES
10517.3
159.4
3134.1
159.4
8.286.7
5645.7
478.1
0
0
0
0
0
0
0
0
53.1
13
53.1
0
G
0
0
MALES
0
0
0
0
0
0
0
U
u
u
0
0
52.6
52.6
0
53.1
0
0
0
U
0
0
0
0
G
0
0
70.8
70.8
0
0
0
0
0
2690.0
0
0
13
2737.3
131.6
0
0
0
0
0
1926.2
132.8
2125.4
0
0
684.3
0
0
0
0
0
0
C
0
G
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
141.6
1912.3
159.4
8764.8
0
0
0
66.4
0
0
212.5
0
0
199.3
0
0
0
0
0
0
0
0
26.3
684.3
26.3
106.2
0
0
0
0
79.0
66.4
70.8
0
283.2
15078.3
70.8
70.8
0
0
0
0
0
0
u
0
0
495.5
0
0
0
0
0
0
0
THE FOLLOWING TABLE LISTS THE FRACTION OF IOTAL STATION ABUNDANCU
ACARTIA CLAUSI
ACARTIA LON,IREM
CALANUS SP
CENTROPAGES MCMU
OITHONA SIMILIS
PSEUDOCALAN!J3
HARPACTICOID
ANNELID LARVAE
AQUATIC MITE
BARNACLE CYPRIS
BARNACLE NAUPLIU
PODON LEUCKARTI
DECAPOD LARVAE
FORAMINIFERA
GASTROPOD LSUS
GASTROPOD LARVAE
ISOPODA
OIKOPLEURA
.2960
.0045
.0632
.2332
.0135
.2024
.1643
.OU45
0
0
.4381
.0695
0
U
0
0
0
0
0
.uG15
0
.0015
U
0
0
U
u
.0978
.2563
.0894
0
C
.0024
.0391
_i
.0391
G
0
.3028
G
0
0
0
0
0
C
J
U
0
0
3
0
0
0
U
0
.0084
0
0
.OG8
0
0
.0120
0
u
.0095
.0017
.0084
3
.0028
.0163
a
0
0
0
0
0
0
0
0
J
.0634
.0034
u
0
0
0
J
0
0
3
0
0
0
C
0
.2466
U
0
.u690
.0048
.0762
0
0
.0034
.0438
0
0
U
G
u
J
0
0
0
0
0
U
6
0
.0060
0
U
.0024
.0671
0
0
0
.0030
U
0
.6015
U
.0536
.0045
.2951
U
6
0
0
0
0
0
.1154
0
0
0
6
0
0
C
0
C
J
U
0
0
.0028
.6023
.1061
.0112
.5950
.0025
.6023
0
0
.0017
0
0
0
0
0
U
0
J
.0438
.0017
.0024
6
3
.0051
0
0
0
0
0
0
0
0
0
0
0
0
G
0
U
U
G
0
0
0
.0146
0
0
0
0
0
0
0
u
.6056
0
0
0
6
3
STATIONS ON 01/12/72
DATUM
SURFACE TEMP.
SURFACE SALINITY
BOTTOM TEMP.
BOTTOM SALINITY
FOREL NO.
SECCMI READING
12.3u
12.450
33.1920
11.000
33.2750
2.0
1.5
1.:
12.900
32.9130
11.200
33.5776
12.600
33.0600
16.100
33.4870
33.1480
10.100
33.4420
9
7
6
6
6.0
6.6
3.5
5.5
TABLE LISTS ABSOLUTE ABUNDANCES
(NUMBER OF INDIVIDUALS PEP CUBIC MCTLR OF WATER FILTERED)
THE. FOLLUWIN
ACARTIA CLAUSI
ACARTIA LON3IREM
ACARTIA SP
CALANUS SP
CENTROPAGES MCMU
OITHONA SIMILIS
PS EUDO CAL ANUS
COPEPOD AAUPL1US
GAMMARID AMPHIPO
HYPERIIO AMPMIPO
ANNELID LARVAE
BARNACLE CYPRIS
BARNACLE NAUPLIU
CMAETOGNATHA
POJON LEJCKARTI
CRAB ZOEA
HERMIT CRAB LARV
PORCELAIN CRAB Z
CRUSTACEAN EGGS
DECAPOD LARVAE
GASTROPOD LARVAE
OIKOPLEURA
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
402.3
125.5
11.1
5572.7
6j40.3
3756.4
0
123.2
30.8
7321.D
77.5
6314.6
39.0
5016.8
30.8
4895.6
194.9
155.0
8135.4
38.7
0
0
258.4
3.7
3. 7
5183.0
3.7
0
0
0
0
0
0
0
0
0
a
0
0
0
0
116.3
0
0
92.4
u
0
0
u
0
7.4
0
0
77.9
G
0
30.8
0
39.7
33.7
11.1
3.7
u
3
0
0
0
33.2
15.9
506.0
369.5
184.7
61.6
0
0
428.7
77.9
39.9
0
7.4
246.3
1539.5
426.1
1317.2
11.1
G
0
J
0
0
0
G
0
0
0
0
77.5
U
0
0
0
U
0
0
232.4
193.7
155.1
G
0
0
0
0
0
0
0
0
u
0
0
61.6
0
0
77.5
0
0
0
0
0
0
G
J
0
0
u
0
6
0
36.8
30.8
77.9
311.8
116.9
0
0
0
J
697.3
155.0
0
0
0
0
0
J
492.6
892.9
61.6
0
0
0
0
0
937.9
0
U
1519.8
0
3
1346.9
0
3
3331.6
u
0
a
a
3
0
0
0
30.8
0
0
0
0
0
0
0
0
C.
0
0
G
0
0
0
3
0
0
77.9
0
a
G
0
0
0
0
G
a
0
0
0
0
0
0
0
0
0
u
0
G
0
u
30.6
G
0
0
3.7
0
0
389.7
G
a
0
0
38.7
38.7
38.7
38.7
77.5
309.9
0
0
0
0
G
0
0
0
0
0
77.5
0
0
0
492.6
184.7
0
0
0
0
0
T
HE FOLLOWING TABLE LISTS THE FRACTIUN OF TOTAL STATION ABUNDANCE
ACARTIA CLAUSI
ACARTIA L ON J- IREM
ACARTI A SP
C A LANUS SP
CENTRUPAGES M CMU
OITHONA SIMI LIS
PS UOOCA L A N J S
COPEPOD NAUP L I U S
GAM ARID A M P HIFJ
HYPERIIO A M P HIPO
ANNELID L ARVA E
9ARNAC LE CYPRIS
BARNA C L E NAJPLI'J
CHAETOGNAT H A
P000N L EUC K A RTI
CRAB Z OE A
HERMIT CRAB L A RV
PORCELAIN CRAG Z
CRUSTACEAN EGGS
O C CAPOD L ARV A E
GASTROPOJ LARVAE
OIKOPLEURA
.1993
.u622
.0013
.uu:55
.1233
.0018
0
0
.0018
0
0
.2213
.0083
.2379
.2579
.0017
J
.2264
.Ju14
.2208
.0056
0
0
0
0
0
0
U
0
0
0
C
.0056
.0033
.0183
u
J
.0067
0
0
.0037
.0655
.Ju13
.0037
.0055
0
U
.0165
0
0
.0033
.0017
0
0
0
0
0
u
u
0
J
0
U
.0033
C
0
U
u
.0384
.0133
.0050
.0014
.2204
.0023
.1904
.0047
.2453
.6012
0
0
0
0
3
0
0
u
.J012
.0012
.1694
.0042
.0014
0
0
.6216
.0167
.0083
0
G
.0111
.0073
.005c
0
G
.0628
.0694
G
0
C
0
uul4
0
U
U
J
u
.0014
.0028
0
C
0
0
C
3
0
0
.0129
.3397
.0047
0
0
u
0
0
0
u
0
0
0
0
G
0
0
0
.UG23
.0213
0
0
0
0
.0047
C
G
G
0
J
0
0
0
0
.10G5
0
0
.0012
0
0
0
0
0
G
u
0
0
.4153
0
u
.0649
0
0
0
0
3
0
0
)
.0222
.0403
.3328
.0472
.3014
0
u
0
0
0
0
0
0
.0012
0
U
0
0
0
0
0
0
.0012
0
J
.0033
0
0
0
0
0
3
0
0
0
u
0
0
.GG12
0
0
U
0
0
0
0
0
0
3
.3116
0
u
0
0
0
0
u
0
G
0
3
0
0
.0093
.0023
0
u
.3014
.3222
.J683
.6023
3
u
0
3
0
.0013
0
STATIONS ON 10/07/72
.4
DATUM
9.400
33.5630
9.100
SURFACE TEMP.
SURFACE SALINITY
BOTTOM TEMP.
BOTTOM SALINITY
9.70u
33.5040
FOREL NO.
SECCHI READING
8.60C
b
5
4
5.0
10.0
11.0
8
4.5
9.700
33.3890
8.400
33.6320
9.60u
33.3980
8.900
33.5630
33.5b40
33.5170
2.0
1.5
1.u
THE FOLLOWING TABLE LISTS ABSOLUTE AdUNUANCZS
(NUMBER OF INDIVIDUALS PER CUBIC MLTER OF WATER FILTERED)
FEMALES
ACARTIA CLAUSI
ACARTIA LONGIREM
CALANUS SP
CENTROPAGES MCMU
OITHONA SIMILIS
OITHONA SPI:NIROS
PSE0000ALANJS
TORTANUS OI3CAUD
COPEPOD NAUPLIUS
ANNELID LARJAE
BARNACLE CYPRIS
BARNACLE NAUPLIU
CHAETOGNATHA
CLAOOCERA,EVADNE
POOON LEUCKARTI
CRUSTACEAN EGGS
GASTROPOD
EGGS
GASTROPOD LARVAE
ISOPODA
OIKOPLEURA
5028.3
IMMS
FEMALES
17+5.5 14005.7
3165.0
MALES
0
0
0
0
0
0
0
u
0
166.2
0
41.6
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
imms
4807.8 12321.6
795.4
74.4
272.9
1208.7
18.6
811.8
54.1
1912.2
0
C
1017.2
24.8
49.6
0
0
MALES
0
0
0
0
U
24.2
0
0
J
0
0
724.8
24.2
483.2
265.8
0
49.6
967.b
74.4
322.5
0
C
0
748.1
249.4
1537.7
0
u
0
U
0
0
24.2
0
0
41.6
0
0
u
0
0
0
u
0
0
0
0
U
0
24.2
604.0
24.2
0
0
u
0
0
0
0
0
0
0
u
0
0
U
83.1
0
0
338.2
U
0
J
0
0
0
0
u
0
0
0
0
0
C
0
0
0
0
it
24.2
393.2
223.3
U
0
0
0
0
0
0
0
0
1
0
24.2
48.3
0
1353.0
0
0
24.8
74.4
49.6
0
1172.6
0
0
0
0
0
99.2
1116.4
505.1
180.4
1569.5
0
0
0
0
0
0
0
0
0
0
13.0
0
0
0
0
36.1
36.1
0
0
0
0
0
0
0
18.1
378.3
0
0
545.8
0
0
3
0
3
24.8
0
C
297.7
248.1
272.9
24.8
0
54.1
18.0
0
90.2
16.0
18.0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
U
0
0
U
0
0
0
0
0
0
0
0
0
36.1
0
0
1
THE FOLLOWING TABLE LISTS THL FRACTION OF TOTAL STATION ABUNDANCE
ACARTIA CLAUSI
ACARTIA LON,IRE1
CALANUS SP
.2115
.3734
.5692
.1222
.1856
.4757
.0603
.0276
0
0
u
0
0
0
.3075
0
0
0
.0017
0
0
.0003
0
0
CENTROPAGES MCMU
.1030
.0025
.0050
0
0
U
0
0
3
OITHONA SIMILIS
OITHONA SPIIIROS
PSEUDOCALANJS
TORTANUS DISCAUO
COPEPOD 4AUPLIUS
ANNELID LARVAE
BARNACLE CYPRIS
BARNACLE NAJPLIU
CHAETOGNATHA
CLADOCERA,EVADNE
POOON LCUCKARTI
CRUSTACEAN EGGS
GASTROPOD EGGS
GASTROPOD LARVAE
ISOPODA
OIKUPLEURA
0
.0070
.0075
0
u
0
3
.0050
.0066
C
.1435
.6022
.0280
.0350
.093G
.0075
.0327
.0025
.1473
.0022
6
.0993
.0066
.2340
0
. 0110
0
.0022
.0022
0
u
u
.0315
u1Jti
.0647
.0009
.0187
.0103
0
0
0
0
0
.6522
.0009
C
0
0
0
0
0
0
0
C
0
0
0
0
0
.0022
0
0
.u017
0
u
0
G
0
C
0
0
0
0
G
J
G
0
.0644
0
0
0
0
0
G
J
0
0
GGv+
0
0
0
u
C
0
U
0
.u302
.0251
.0276
.0025
0
0
.0009
.0233
.0009
J
0
0
3
0
C
0
0
0
G
L
3
C
0
u
.6022
.0035
6
0
u
u
.0131
0
0
0
.C46
0
0
0
0
0
0
0
.0935
.0226
0
0
0
0
0
0
0
0
0
0
.0009
0
l
G
0
C
0
G
0
0
0
0
0
0
J
.0553
0
G
0
0
0
J
0
0
.0009
G
0
0
G
G
0
0
0
.JG19
0
0
0
.G025
0
0
.0044
u
0
0
5
0
.0101
J
.
1131
0
.
0619
.
6221
0
.
1921
STATIONS
ON 10/u7/72
2.5
DATUM
9.750
33.3890
8.300
SURFACE TLMP.
SURFACE
BOTTOM
BOTTOM
3.0
SALINITY
TEMP.
SALINITY
FORLL NO.
SECCHI READING
5.0
4.0
33.6420
9.950
33.3750
9.050
33.6540
33.3490
8.200
33.6900
5
5
6
7
12.0
12.0
13.3
10.0
9. 350
9.360
33.3630
8.200
33.E956
THE FOLLOWING TABLE LISTS ABSOLUTE ABUNDANCES
(NUMBErt OF INDIVIDUALS PER CUBIC METER OF WATER FILTCRLD)
ACARTIA CLAJSI
ACARTIi LONJ-IREM
ACARTIA SP
CALANUS SP
CENTROPAGES ICMU
OITHONA SIMILIS
PSEUDOCALANJS
COPEPOD NAUPLIUS
ANNELID LARVAE
BARNACLE CYPRIS
BARNACLE NAUPLIU
CHAETOGNATHA
CLADOCERA, EVADNE
P000N LEUCKARTI
HERMIT CRAB LARV
CRUSTACEAN EGGS
ECHINODERM LARVA
GASTROPOD LARVAE
OIKOPLEURA
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
639.4
374.8
1499.4
1381.2
2355.4
5546.5
46.3
2400.3
152.0
76.0
114.0
1638.3
1200.1
46.8
538.4
117.1
3267.1
22.0
3815.3
0
57.2
57.2
114.3
0
0
0
0
0
6
0
0
0
0
0
0
0
0
0
C
0
0
0
44.1
46.3
23.4
117.1
93.6
152.0
1557.E
76.0
0
0
22.0
22.0
154.3
132.3
132.3
110.3
1608.1
0
0
0
88.2
0
0
0
0
0
44.1
1264.1
1030.0
491.6
23.4
23.4
0
0
0
44.1
0
0
0
0
1455.3
859.9
22.0
154.3
22.0
132.3
0
44.1
44.1
0
0
0
140.5
70.2
515.0
0
u
0
0
0
0
0
0
0
0
0
210.7
23.4
46.8
280.9
70.2
38.0
190.0
O
70.2
1802.6
190.0
2773.3
0
0
759.8
227.9
209.5
133.3
C
0
0
0
0
0
0
0
0
0
0
0
u
0
38.0
76.0
0
0
0
0
0
0
0
0
0
0
0
0
0
d
607.8
0
0
133.3
57.2
209.5
19.0
19.0
495.3
0
0
0
0
0
0
0
6
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
38.6
379.9
0
C
0
19.0
19.0
19.0
133.3
19.0
38.1
514.3
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
u
0
0
0
0
0
0
0
0
266.7
38.1
T HE
FOLLOWI G TABLE LISTS THt FRACTION OF TJTAL STHTiUN ABUNDANCE
'
ACARTIA CLAJSI
ACARTIA LON;IREM
A CARTIA SP
CALANUS SP
CENTROPAGES ICMU
UITHUNA SIMILIS
PSSE000CALANJS
OP PO NAUPLIUS
COPEPOD
ANNELID LARVAE
BARNACLE CYPRIS
B A RNACLE NAJPLIU
CHAETOGNATHA
CLADOCERA,tVADNt
POOON LEUCKARTI
HERMIT CRAB LARV
CKUSTACEAN EGGS
ECHINODERM ARVA
G A STROPOD LARVAE
OIKOPLLURA
.0759
0
.6445
.0026
0
0
0
0
J
uuti2
.1728
.1021
0
uu26
.1760
.002b
.0183
.0157
.0157
.0131
.2141
0
0
0
.0105
0
0
.1099
.0037
.0428
.0093
.3035
.0037
.1717
.0060
.1238
.uG40
0
0
0
C
0
C
0
.0093
6037
.0074
0
.0056
.
.2914
.0060
.1737
.0061
.1273
.0061
0
0
0
0
0
0
. 0020
0
0
.0020
0
.0020
.6020
.0040
.0141
.0020
.0545
u
0
0
.0015
.1006
.u819
.0391
.0019
.0019
0
J
.0052
0
0
.0052
0
6
0
.002u
6040
0
0
.0112
0
0
G
G
0
.
0040
0100
143'.
0080
.0016
. 0399
0106
0
.0120
.145 7
C
G
0
0
0
6
D
0
0
0
G
0
0056
.
.
.
.
.
0
C
.0222
.0141
0
.2545
.0121
0
0
0
0
0
0
0
0
G
0
0
0
.0183
.0026
0
0
.0056
0
0
C
0
0
0
J
.0410
0
J
.d15
.0141
.0061
.0 2 22
.0020
.0020
0
0
.0525
0
0
0
0
G
0
0
C
G
.0157
0
0
0
0
0
0
0
0
0
0
0
0
0
J
u
0
0
0
C
0
0
0
0
0
0
0
0
0
0
0
0
u
G
6
.0020
.020C
.0283
0
0
.01b8
.0015
.6037
.0223
0
C
0
.0046
0
a
.0026
.0652
.0052
.
STATIONS ON 10/07/72
.3N
OAT UM
9.700
33.4990
9.550
33.5050
11.000
33.4710
10.100
33.4970
SURFACE
TEMP.
SURFACE SALINITY
BOTTOM
BOTTOM
.2S
TEMP.
SALINITY
FOREL NO.
SECCHI READING
7
9
5.u
3.u
THE FOLLOWING TABLE LISTS ABSOLUTE ABUNDANCES
(NUMBER OF INDIVIDUALS PER CUBIC METER OF WATER FILTtRLD)
ACARTIA CLAJSI
ACARTIA -ONJIREM
CALANUS SP
CENTROPAoES MCMU
EUCALANUS SP
OITHONA SIMILiS
OITHONA SPI4IROS
PSEUDOCALANUS
COPEPOC NAUPLIUS
HARPACTICOID
GAMMARID AMPHIPO
ANNELID LARVAE
BARNACLE CYPRIS
BARNACLE NAUPLIU
P000N LEJCKARTI
CRAB ZOEA
CUMACEAN
EUPHAUSIIO CALYT
FORAMINIFERA
GASTROFUO E GS
GASTROPOD LARVAE
ISOPODA
MYSID LARVAE
OIKOPLEURA
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
210.9
122.7
3.8
433.7
3.8
205.'.
7.7
0
0
0
3.8
0
0
379.7
3.8
15.3
7.7
3.8
184.1
3.8
0
7.7
0
0
456.5
79.9
7.6
0
3.8
J
0
0
0
106.5
3.8
0
u
0
7.6
84.4
15.3
23.0
391.2
3.8
7.6
300.5
0
0
u
0
0
U
0
0
0
0
G
u
0
0
0
U
11.5
26.8
0
0
3.8
3.8
7.b
0
0
0
0
64.7
G
0
3.8
0
0
0
0
0
23.0
0
0
79.9
0
0
0
0
u
0
0
3.8
3.8
0
0
0
0
G
0
0
0
0
0
u
0
G
0
3
0
0
0
0
0
0
0
3.8
7.6
3.8
3.8
0
0
0
0
0
0
0
0
0
U
3.8
0
0
0
0
0
0
3.8
3.8
0
3.8
U
FEMALES
MALES
IMMS
FEMALES
MALES
IMMS
TH: FOLLJWI4u TABLE LISTS [HL FRACTION OF TOTAL STATION ABUNOANCL
ACARTIA CLAUSI
ACARTIA LON31REM
CALANUS SP
CENTROPAGES MCMU
EUCALANUS SP
UITHJNw SIMILIS
UITHONA SPINIROS
PSEUDOCALANJS
COPEPOD NAUPLIUS
HARPACTICOID
GAIMARID AMPHIPO
ANNELID LARVAE
9ARNACLE CYPRIS
BARNACLE NA'JPLIU
PO0UN LEJCKARTI
CRAB ZOEA
CUTACLAN
EUPHAUSIID CALYT
FORAMINIFERA
GASTRUrD3 E"GS
GASTrt;OP00 LARVAL
IGOP07A
MYSID LARVA_
OIKO'L=URA
.1338
.0049
.0779
.0024
.2409
.0024
.6097
.2222
.0019
.1053
.2333
.0039
.6409
0
0
.GG39
0
.0619
0
0
.0049
.uu24
G
U
J
.1168
.0049
.uu24
u
.0619
0
0
u
.0535
.0097
.0140
.2462
.6546
.6019
.0039
0
u
0
u
0
0
0
0
u
0
.0024
0
.u073
.0170
.UG24
.0145
U
u
u
G
G
0
G
u
.1540
0
G
0
0
.0019
G
3
19
0
!3
.0039
0
0
.0331
0
3
0
0
3
.0409
u
J
0
0
0
.0019
0
.0024
0
u
u
0
6
0
0
0
]
3
u
u
0
0
0
0
G
0
0
u
u
.OG19
.0639
.0019
.OG19
G
l
0
U
J
3
.0019
0
]
v
0
0
3
0
.uu24
.0024
u
0
.0024
u
]
APPENDIX III
Appendix III contains maps showing the areas from which each set of
drift bottles were returned.
drops:
There are 2 maps for each set of bottle
the first shows the returns from the immediate survey area (Moolack
Beach).
The arrows on these local maps are the specific release points of
bottles found outside of Moolack Beach and indicate their general direction
of travel.
vey area.
The second map shows the area of returns made outside the sur-
10 June 1972
24
--------j
Kelp
13
18
X20
/
II
15
23
17
i
13
13
7
9
it
*
83
fILOtter Rock
8
(//)
9
15
S
..
I"
II
19
5`
's
1
16
Kelp
53:
18
21
1
4i
S
5
17
*.
I
g
I
54
It
-C4
II
14
4,
19
9
14
19
20
16
22
18
14
23
16
24
23
8
I
3s
L)
ceun Purl
'
' Beverly Beach /
24
22
p en ce'
Kelp
13
25
n
- *,
7
83
/10
26
' Jmo Otter Rock
7
.10
13
No nlocal returns on this date
10 June 1972
26 June 1972
24
18
1.20
26
23
17
17
21
S
19
16
25
19
24
19
20
16
22
18
22
21
23
19
16
22
24
18
23
13
26 June 1972
6 July 1972
6 July 1972
19 July 1972
24
26
21
25
24
22
23
24
No local returns on this date.
19 July 1972
27 July 1972
18
26
23
21
19
25
19
24
19
20
22
18
22
23
19
16
22
24
18
23
9 August 1972
18
26
23
21
18
19
25
19
19
20
22
23
16
24
23
9 August 1972
9 August 1972
Returns of 16 August 1972
9 August 1972
Returns of 17 August 1972
9 August 1972
Returns of 18 August 1972
9 August 1972
Returns of 19 August 1972
9 August 1972
Returns of 20, 21, 22 August 1972
APPENDIX IV
Appendix IV is a listing of the drogue data reduction process.
set of data is presented in 2 parts:
Each
the first is information necessary
for plotting the data points (shown in Figure:iV-i); the second contains
additional plotting information, the variations in speed from point to
point ("Smoothed Linear Speed"), and the cumulative average speed ("Average
Speed" in cm/sec or nautical miles/hr).
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065CP,V#7700 100/07r
-.__M
m
OATL
OF 29SE4JTIJ;+ = AUU
HIGH TIDE AT
17, 1972
733
OF DATA 'coI:nTS
45
DIST FROM 0111\T
O-- OBS[RVt TI;"+ TU Y-Ax; ;
0120.9 MET=F,S
CORRECTION IN
ZERO POINT =
J;:( <LE'
1'.JTFS 7 SECONDS
ANGLE OF RUTATI;jN = 14 OLGF EEC 2: 'i1-+UTES 40 fS E ,C,, Cv
NUMBER
DIST FRO'l
READING
1
2
TIM=
OZIMUTh
1042
1346
36
3
17571
4
1355
5
11
6
7
11 5
1110
1115
1120
1125
1130
1135
1140
1144
1146
1150
1155
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
26
27
28
29
33
31
32
33
34
35
36
37
38
39
40
41
42
43
44
C
12 C
12 5
121C
1215
1220
12?5
1230
1233
1234
1235
1236
1237
1239
1239
1240
1245
1246
1250
1255
13
0
13 5
1310
1315
1320
1325
1330
1335
45 25
77 ?9 43
33 12 45
4 25
39
39 37 10
43 21 40
41 23 30
42
0 30
0
42 25
42 46 50
43 13 20
43 29
5
43 33 45
43 43
0
43 49 40
43 45
0
43 41
5
43 33 30
43 40 10
43 44 15
44
1 40
44 10 55
44 19 15
44 51
0
45
5 20
45 14 20
45 10 10
45 ii 50
45 11 10
45 12 40
45 13 25
45 15
0
45 31 43
45 33 25
45 51
0
46 22 45
47
0
15
48
2 10
49
1 20
EL_VATION
51
91
91
91
91
45 35
46 50
43
0
49
51
9i1
53
91 54
51 56
91 57
25
30
25
55
36
45
91 57
0
41 53
G
92
0 50
92
2 25
92 2
0
92 2 20
92 3 25
92
3 25
02
92
92
92
92
92
92
92
92
92
92
92
92
92
92
92
92
92
52
92
92
92
340
2
4
4
5
50
5
40
6
50
20
25
7
6
0
5
5
7 20
1G 20
7 25
8 10
9 30
8 40
10
10
11
12
13
15
15
30
49 59
0
50 32 15
45
15
14 50
14 45
92 16 35
92 16 55
51 34 0
53
4 30
54 16 20
92 16 0
92 14 0
92 11 30
03SERV c7T
1041.6
1629.4
1018.2
1065.1
979.
969.6.
9570
943.9
933.9
939.8
931.9
910.1
899.3
901.3
893.9
891.0
891.0
889.2
895.2
385.8
886.2
879.1
875.0
867.0
863.5
869.8
863.5
843.6
863.C
857.9
8'"9.1
854.6
844.2
844.2
836.2
828.3
825.2
815.5
816.0
805.0
803.1
808.4
820.5
836.2
k
-It'. TFRS)
1469.9
1487.8
15714.8
1524.8
1547.9
1563.6
1985.0
1600.8
1611.9
1613.7
1624.0
1639.2
1646.5
1643.1
1649.7
1652.9
1652.0
1651.3
1649.6
1654.9
1659.1
1664.8
1668.7
1679.8
1684.6
1683.4
1685.7
1696.1
1686.2
1689.1
1693.7
1691.2
1706.0
1700.4
1708.1
1718.7
1726.1
1745.7
1758.0
1775.71
1782.9
1793.8
1808.7
181809
y
(' ETERS)
CCPRECTFD A71M
:Lz:JATI:rt
IN pAOIW:S
IN rA --, T1 o
811.4
.8930491
810.1
809.1
792.4
792.0
791.5
786.4
781.7
789.9
787.1
770.9
761.6
766.1
764.3
75b.9
756.4
753.8
759.9
753.2
755.1
750.3
747.9
745.2
744.1
750.6
744.7
727.7
744.3
740.1
732.6
737.6
730.6
730.8
726.0
723.0
724.6
723.0
729.8
726.0
727.5
738.4
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1.6058894
1.6104718
1.6119274
1.0159749
1.0164576
1.0151622
1.013962E
1.0117554
1.0136957
1.0148833
1.0199479
1.0226380
1.0250641
1.0343009
1.6384888
1.0410869
1.0358?53
1.0403582
1.0401662
1.0406011
1.3408200
1.0412818
1.0461282
1.0466380
1.0517542
1.0809674
1.0718569
1.0899080
1.1071184
1.1238946
1.133565E
1.1515287
1.6015086
1.6513717
1.6022135
1.cu2E044
1.6004702
1.oC7733C
1.6042229
1.60469+7
1.6053476
1.6049316
758.0
779.0
1.1778523
1.1987484
837.8
1.6111;1225
1.6859430
1.6:54.,54
1.6662374
1.6063914
1.6060963
1.6CE6963
1.6067533
1.6065254
1.6068672
1.6068912
1.o071321
1.6073501
1.6076390
1.6078359
1.6075590
1.6078359
1.6087086
1.6076599
1.6080738
1.6084657
1.6082228
1.6086346
1.6086846
1.609475
1.6094134
1.6395573
1.6160162
1.6099922
1.6105260
1.6106220
1.6103580
1.6097762
1.6 090475
45
13 40
55 43
SMOOTHED
X-3PEOu
READING
2
3
4
5
C1/SE0
7.36
7.b5
h.61
6.54
E.63
9
5.88
5.37
3.18
10
it
12
13
14
15
16
17
?.58
3.04
3.65
'.b7
1.4b
1.76
.54
.17
7
9
19
19
20
21
-0.37
35
52
SMUJT4_0
Y-SPEED
CM/Sw r,
0.49
0.50
-1.98
1.5?
-1.81
0.65
-1.15
-0.13
08
-1.23
-3.15
-2.33
-0,92
-1.29
-1.35
-1.15
.33
.33
-0.35
.86
1.69
.14
-1.07
22
23
24
25
26
27
23
1.53
-0.59
2.30
2.20
-1.10
-O.E9
29
30
31
1.88
-1.34
2.81
32
33
34
35
36
6.10
.75
9.39
2.59
3.09
-5.28
-0.20
-6.41
-1.05
-0.70
37
4.17
-0.34
2.72
3.28
6.37
1.54
.50
-0.29
-9.08
-3.50
-2.52
2.72
-3.75
38
39
40
41
42
4.36
5.21
4.13
3.98
3.75
43
44
4.01
4.47
5.71
6.30
45
4.49
6.92
.76
.15
.50
.95
3.56
P
20
850.2
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7°7.3
1.224128:
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c;-z
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T ,4
4.43
1487.5
4.E
1505.3
4.18
4.03
4.16
3.55
3.29
1.91
1.55
1.9o
2.89
1525.3
1545.,
1545.3
? 3.1
1593.?.
7
1559,3
1608.8
1616.5
1625.6
1636.6
1644.6
1648.1
1650.2
1651.5
1652.1
1651.0
1651.9
1654.5
1659.b
1664.2
1671.1
1677.7
1682.5
7
2.1.3
1.54
1.31
.87
.7u
?3
.29
.53
1.20
.98
1.53
1.38
1.66
1.98
6.65
2.29
1.89
1.82
2.81
4.84
.46
6.82
1.68
1.89
2.51
2.66
3.13
2.50
2.46
3.10
4.19
4.88
3
1684.6
1688.4
1689.3
1690.4
1689.6
1691.3
1695.0
1697.2
1702.8
1709.1
1718.3
1730.8
1743.9
1759.5
1771.3
1783.3
1795.1
1807.1
1320.6
1834.0
310.2
3' .G
77.4
?.
.,
76.
7
792.3
773.2
7 6.2
764.5
7b2.4
759.2
755.7
776.7
755.6
756.1
752.9
751.1
747.9
745.7
746.6
746.4
741.0
733.9
737.4
739.0
736.8
733.6
733.0
729.2
726.5
724.5
723.5
720.3
726.3
727.3
730.6
741.3
753.5
773.K
799.6
AVc.RAGE
SC <<0
(CM/SEC
1.:.0",
AVEa0G;SPE
4.43
4.51
4.38
.09
.09
.09
4.35
4.27
4.14
4.r1
3.74
3.48
3.32
.09
.05
,u3
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.07
.07
.007
3.28
3.ls
3.04
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LE
2.99
,b
2.87
2.72
2.5E
2.43
2.32
2.26
2.19
CE
2.16
2.12
2.11
2.11
2.15
2.15
2.15
2.15
2.15
2.18
2.11
2,14
2.13
2.12
2.13
2.15
2.19
2.20
2.20
2.23
2.29
2.36
G
?
(Kt+CTS)
C
.05
.05
05
.04
.04
.04
.04
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G4
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04
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0
417;'
DATE OF 09SEi2VATION = AUG
LOW
17, 1972
TIDE AT 1206
NUM3ER OF DATA POINTS = 85
DIST FROM POINT
OF 03SFRVATION TO Y-AXIS = 2122.9 1::T-RS
CORRECTION IN
ZERO POINT =
1 MINUTES . SECCNCS
3 D'GRcES
ANGLE OF ROTATION = 14 DEGFE6S 25 MINUTES 40 SECONDS
READING
1
2
3
TIME
AZIMUTH
1351
1355
21 31 20
22 34 10
24 30 15
14
0
4
14 5
5
1410
1417
1422
1424
1426
1429
1431
1432
6
7
3
9
10
11
12
13
14
1434
1435
15
16
17
1437
1438
1439
18
19
20
21
1440
1441
1442
1443
1444
1445
1446
1447
22
23
24
25
26
27
28
29
30
31
32
33
34
35
36
37
38
26
29
33
37
39
40
43
44
45
22
41
35
14
55
46
8
ELEVATION
25
5
30
5
35
10
34 25
55 30
0
47 33 43
48 33
0
49 52 20
91
9
0
51 50
0
52 42 25
1458
1459
53 33 35
54 32 40
55 22 45
56 21 25
57 10 40
57 59 10
59
7 10
59 56 45
60 57 40
61 56 55
62 50 15
63 51 40
64 42 25
66 28
0
67 10 35
67 59
0
68 51 25
69 38 45
15
70
1448
1449
1450
1451
1452
1453
1455
1456
1457
0
15 1
20
71 10
71 50
5
0
39
15 2
40
41
15 4
15 5
73 14 40
42
43
15 6
15 7
74 38 20
44,
15
8
5
73 57 30
75 24 0
76 6 50
91
91
91
91
91
91
91
91
91
91
91
91
17 20
21
25
29
33
33
41
43
45
48
49
50
51
53
40
0
10
20
25
29
55
15
45
20
40
91
55
91
30
91 54 25
91 55 25
91 56 5
91 56 45
91
58
0
91 58 30
91 59 20
92
92
3
0
0
92
1
2
5
5
92
0
92
92
92
92
92
92
92
2
2
3
4
4
25
20
40
20
45
30
25
92
92
92
92
92
92
92
4
40
4
5
55
92
92
92
92
92
2
3
5
DIST FROM
JBS6RV PT
1422.3
1346.8
1293.9
1233.4
1178.4
1117.5
1035.3
1058.3
IC44.9
1011.3
1005.8
993.7
962.6
958.9
908.1
901.3
898.3
898.9
1.2034988
1.2180671
1.2351335
1.2494589
1.2635690
864.3
1.2833488
865.0
869.7
871.2
869.6
870.1
1.2977709
1.3154911
1.3327255
1.3482414
1.3661056
867.3
872.6
1.3808688
1.4115828
872.6
872.6
873.3
869.8
870.8
881.2
882.5
1.4239679
1.4380540
1.4533001
1.4670677
1.4790928
1.4936131
1.5052731
1821.1
1833.7
1848.3
1867.4
1880.7
1895.9
1942.3
1956.2
883.8
1982.8
882.1
880.3
879.1
1993.9
2006.4
2019.8
2032.4
2042.8
897.7
1
55
15
25
906.9
913.2
0
1.1863124
866.1
864.7
865.2
868.6
865.5
1926.1
30
1
863.8
888.6
883.2
2
902.0
+395498
1789.7
1804.6
891.6
883.8
884.4
887.4
1.5932916
1."19.5512
1.5355228
1773.4
1911.5
874.5
.6271530
.645431E
.6791980
.7185161
.7640693
1756.7
896.5
25
20
3 55
Ili RADia^,S
1.0988779
1.1219543
1.3423882
1.1561831
1.1714292
2054.8
2065.0
2086.6
2097.4
2107.9
2119.9
2131.3
352..
886.7
897.3
901.9
906.9
913.2
L EVATIZN
IN RAOIGNS
863.0
865.9
917.9
867.0
867.8
1741.3
915.7
834.7
810.2
812.8
811.9
5-'=.3
331.5
?35.2
CORRECTED AZIM
359.3
857.5
855.2
865.3
867.4
947.3
941.9
931.9
928.0
921.5
916.3
Y
(M0TE-S)
.9074974
.9364391
.9656993
1.0120227
1.0356085
1.0566988
1.0816166
952.8
874.5
4
4
971.3
1047.0
1116.1
1194.4
1272.1
1376.7
1454.7
1495.7
1528.5
1586.3
1605.9
1634.2
1661.2
1682.4
1705.9
2378.5
961.1
45
5 45
5
x
(MITERS)
1.5298753
1.5423360
1.5542142
1.5674989
1.5799560
1.59E-7344
1.5979460
1.59'4245
1.6332732
1.631:230
1.601.4125
1.6024295
1.6026334
1.8029373
1.6333532
1.6039120
1.6040739
1.E043695
1.5045647
1.6047567
1.6051225
1.6052665
1.5055094
1.6057036
1.6057276
1.6360185
1.6062954
1.6064754
1.6063314
1.6064774
1.6366723
1.6067923
1.6070112
1.6369872
1.6070592
1.6071312
1.60713?1
1.6773741
1.6073741
1.6069972
1.6069632
1.6068403
1.6064294
1.6062585
1.6060665
1.6058236
45
46
47
48
49
50
51
52
53
54
55
56
57
58
59
60
61
62
63
64
65
66
67
68
69
70
71
72
73
74
75
76
77
78
79
80
81
82
83
84
85
READING
2
3
4
5
6
7
8
9
10
11
12
13
14
15
15 9
1510
1511
1512
1513
1514
1515
1516
1517
1518
1519
1520
1521
1522
1323
1525
1526
1527
1528
1529
1530
1531
1-332
1533
1534
1535
1536
1537
1538
1539
1540
1541
1342
1543
1544
1545
1546
1547
1548
1549
1550
76
77
78
79
79
80
81
82
82
83
34
84
85
86
86
88
83
89
90
90
91
92
92
93
93
94
95
95
96
96
97
98
98
99
46 35
30
0
21
0
2
20
43 30
34 40
13
0
1
5
41
28
11
49
31
15
55
40
50
5
50
25
5
20
10 45
t>4 50
31 40
9 40
41
0
23 50
1 50
37 20
16 50
55 50
32 25
7 25
45 30
27 55
56 40
32 25
7 50
41 50
17
5
5 10
3C 40
2 30
42 10
13
0
49 45
100
130
101
101
102
102
103 24
0
91 59 50
91 59
0
91
91
91
91
91
91
91
53
57
57
55
35
40
15
56
55
C
91
91
91
91
91
91
91
91
91
52
0
50
50
56
49
45
20
20
20
43
5
54 30
52 25
91 52 25
91
91
91
91
47 30
46
5
46
45
44
42
42
42
41
15
30
25
45
50
10
35
91
91
91 41
0
91 4u 20
91 39 35
91 33 50
91 37 45
91 33 10
51 36 50
91 36 20
91 35 45
91 35.50
91 35 0
91 33 40
91 33 26
91 32 15
91 31 55
91
31
5
917.7
924.0
927.3
934.6
937.9
949.4
956.2
960.4
973.2
978.2
981.8
993.0
996.7
996.7
1005.8
1017.4
1023.0
1036.6
1035.0
1042.4
1053.2
1070.4
1069.5
1076.4
1082.6
1068.8
1096.1
1.104.4
1112.6
1125.1
1120.3
1135.8
1141.6
1148.7
1147.7
1157.6
1174.2
1178.4
1192.2
1196.6
1207.5
SMOOTHED
SMOOTHED
X-SPEED
CM/SEC
Y-SPEED
CM/EEC
LINEAR
SPEED
30.64
24.79
-6.44
18.78
14.95
25.01
28.94
?0.66
24.84
42.19
36.73
21.16
29.36
2.53
.57
2.11
3.43
4.13
7.66
.64
2.36
1.65
5.52
41.32
20.14
-0.61
39.79
.36
199.26
14. 02
2141.9
2153.7
2167.6
2179.1
2190.5
2205.5
2218.1
2230.4
2245.9
2257.2
2269.6
2282.4
2294.9
2307.3
232u.6
2344.7
275x.7
2372.6
2383.3
2394.4
2409.1
2425.8
2436.2
2454.0
2463.6
2476.5
2489.4
2503.7
2519.4
2532.6
2541.7
2558.3
2570.7
2584.2
2598.8
2610.7
2627.5
2641.0
2657.2
2676.6
2686.2
917.5
923.5
926.2
932.9
935.4
945.8
951.4
954.'.
970.7
959.0
970.8
980.1
981.8
979.5
986.2
993.0
995.5
1006.1
1001.7
1006.4
1013.4
1026.6
1022.5
1025.5
1027.6
1029.8
1033.0
1036.7
1039.8
1047.9
1039.1
1049.0
1050.2
1051.3
1044.4
1049.8
1060.2
1058.1
1065.7
1063.9
2068.0
SMOOTHED
15.01
17.41
12.56
15.11
28.73
22.02
12.77
17.64
25.01
12.09
23.37
119.85
SMCOTHED-X
1044.8
1119.2
1194.2
1281.1
1367.3
1442.3
1493.3
1537.0
1575.1
1610.3
1635.1
1659.3
1683.2
1922.3
SMOOTHEC'-Y
819.2
311.6
813.3
819.7
834.1
846.5
855.7
856.4
860.7
862.6
665.9
865.2
865.4
882.2
1.5915200
1.6041509
1.6189861
1.6310083
1.6429532
1.6578164
1.6704733
1.68:0053
1.6948093
1.7385289
1.7268209
1.7320911
1.7441882
1.7568911
1.7685991
1.7905352
1.8033588
1.8140734
1.3251269
1.8342437
1.8467008
1.8577543
1.6680827
1.8705711
1.8909162
1.9015588
1.9117396
1.9228178
I.9351549
1.9435190
1.9539187
1.9642195
1.9738192
1.9843558
1.9983523
2.0057688
2.0150289
2.0265689
2.0355381
2.0462265
2.0511913
AVERACE
SPEED
(CM/SEC)
18.78
16.65
1.5055534
1.6054134
1.6052905
1.5056236
1.6049036
1.6644398
1.602498
41329
1.6034971
1.6034971
1.50, 33771
1.6736113
1.6025913
1.6028;13
1.6,26794
1.
1. 502?375
1.6320566
1.6+016537
1.5017)37
1.6014348
1.66116)9
1.6008841
1. 60 C7J31
1.6505161
1.6"_03+32
1.60017??_
1.5999323
1.5997534
1.5995445
1.5992205
1.59%35"?5
1.598:527
1.3998137
1.5966473
1.5996718
1.5981+318
1.5980+20
1.7979461]
1.5975311
1.5975322
1.5972922
AVERAGE
SPEED
(KNOTS)
.37
.33
16.07.32
16.42
.32
15.38.36
15.34.3631
15.97
16.31.32
16.03.32
16.12.32
16.33.32
16.14
.32.
16.31.32
20.81
.41'
16
17
18
19
20
21
22
23
24
25
26
27
28
29
30
31
32
33
34
35
36
37
38
39
40
41
42
43
44
45
46
47
48
49
50
51
52
53
54
55
56
57
58
59
60
61
62
63
64
65
66
67
68
69
70
71
72
73
74
75
76
77
32.70
23.22
-336.18
26.87
26.62
26.49
24.45
2.24
1.04
-30.01
-0.52
-1.69
.76
1.54
24.27.49
-0.49
25.73
26.11
26.46
34.51
25.23
25.77
24.81
31.48
-2.14
2.29
3.80
2.55
.18
-2.12
1.69
14.33.70
27.91
2.90
20.59
21.39
20.24
19.39
18.13
74.32
11.83
23.86
13.51
18.84
13.87
18.78
20.17
.21
-1.56
-0.99
4.54
7.08
8.83
4.48
10.76
11.24
8.81
3.67
9.23
7.27
20.68
3.56
20.46
6.61
10.85
10.32
10.54
13.85
9.73
9.12
5.21
7.11
4.53
3.40
6.23
4.44
11.06
4.86
6.10
4.05
13.81
8.96
6.73
21.05
21.62
22.17
21.36
21.75
21.78
21.37
23.92
20.93
21.22
27.68
14.27
28.92
21.46
19.82
20.67
23.63
23.24
22.33
20.96
22.41
21.89
22.28
23.85
24.01
21.11
21.59
21.13
23.80
.58
4.02
4.17
5.02
5.52
8.26
1.34
5.15
1.27
7.08
19.66
ib.94
202.51
16.12
16.00
15.90
14.70
14.57
15.44
15.72
15.94
14.88
15.22
15.46
14.94
18.92
8.61
16.83
12.36
12.87
12.16
11.95
11.65
15.52
7.59
15.70
12.99
12.48
12.46
12.56
12.86
13.43
12.90
14.21
14.37
14.73
1941.9
1958.3
1757.1
1773.2
1789.2
1805.1
1819.9
1834.3
1649.8
1865.4
1881.3
1896.0
1911.2
1926.6
1941.5
1960.4
1977.6
1994.3
2006.7
2019.5
2031.7
2043.3
2054.2
2068.3
2083.0
2097.3
2108.4
2119.7
2131.0
2142.3
2154.4
2166.8
2179.1
2191.7
2204.7
2218.0
15.27
2230.8
14.30
14.17
13.20
13.25
12.89
12.89
17.02
8.96
18.57
13.20
12.44
12.64
16.42
14.94
13.99
12.58
13.66
13.37
13.70
14.69
2243.9
2256.9
2269.7
2282.3
15.23
12.69
13.32
12.70
14.90
2294.3
2307.6
2324.2
2341.3
2358.7
2371.5
2383.4
2395.8
2410.0
2423.9
2437.3
2449.9
2463.4
2476.5
2489.9
2504.?
2518.6
2531.3
2544.2
2556.9
2571.2
883.6
884.2
8b5.2
865.9
864.9
865.3
866.3
8E6.5
866.3
865.0
666.4
868.6
870.2
870.3
869.0
870.0
870.9
872.6
872.7
671.8
871.2
873.9
879.2
883.5
880.3
895.3
902.0
907.3
912.5
918.3
922.4
927.5
931.5
938.7
944.2
950.5
959.8
964.7
970.2
973.3
977.5
980.4
982.5
986.2
991.5
998.2
1001.1
1004.8
1007.2
1015.5
1020.9
1024.9
1025.2
1027.6
1030.2
1033.2
1036.5
1041.4
1042.2
1045.3
1046.1
1050.3
20.79
20.71
24.42
.41
.41
.48
23.93
23.7E
23.59
23.44
.47
.47
.45
.46
22.90
22.77
22.65
22.59
.45
.45
.45
.44
21.92
21.79
21.64
21.50
.43
.43
.43
.42
20.91
20.84
20.73
20.62
20.52
20.41
20.32
.41
.41
.41
.41
.40
.40
.4C
19.94
19.88
19.82
19.75
19.68
19.61
19.53
19.46
19.43
.39
.39
.39
.39
.39
.39
.38
.38
.33
18.98
.37
.37
.37
.37
.37
.37
.37
.37
.37
.37
.36
.36
.3E
24.25.48
24.09.47
23.30.46
23.17.46
23.03.45
22.15.44
22.07.43
21.36.42
21.28.42
29.23.40
20.14.40
20.07.39
20.06.39
19.21.38
19.20.38
19.14.33
19.07.38
19.01.37
18.94
18.89
18.83
18.78
18.73
18.68
18.64
18.61
18.55
18.51
18.45
18.42
78
79
80
81
82
83
84
85
22.48
22.25
23.90
23.77
25.85
23.93
24.82
24.90
-2.60
-0.19
4.68
7.62
8.94
2.03
5.50
3.51
13.58
13.35
14.61
14.98
16.39
14.41
15.26
0
2584.7
2598.0
2612.3
2626.6
2642.1
2656.5
2671.4
2686.2
1048.9
1048.7
1051.5
1056.1
1061.4
1062.6
1065.9
1068.0
19.38.36
1d.3Z.36
19.30.36
18.27.36
19.2E.36
19.22
.3E
18.20.36
0
0
DATE OF OBSERVATION = AUG
21, 1972
HIGH TIDE AT 1144
NUMBER
OF DATA POINTS = 35
DIST FROM POINT
OF OBSERVATION TO Y-AXIS = 2122.9 METERS
CORRECTION IN
ZERO POINT =
10 DEGREES 15 MINUTES 35 SECONDS
ANGLE OF ROTATION =
14 DEGREES 25 MINUTES 40 SECONDS
READING
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
TIME
AZIMUTH
1131
1133
1135
1137
1139
1141
1142
1143
1144
1145
1146
1147
1148
1149
1150
1151
1152
1153
1154
25
25
26
26
26
27
27
27
1155
1156
1157
1158
1159
12 0
26
27
28
29
30
31
32
33
34
35
READING
2
3
ELEVATION
15 15
44 40
7 40
30 15
55
5
15
17 45
26 55
27 35
5
27 42 55
27 49 25
27 55 20
27 59 25
28
5 55
8 20
28
28 12
5
28 11 55
10
28 13 25
28 16
0
28 20 20
28 24 15
28 25 20
28 27 55
28 30 10
28
30
125
20
23 25 40
1210
1215
1220
1225
1230
1235
1240
1245
1250
28
27
27
27
27
27
27
27
27
14
56
32
43
43
46
33
SMOOTHED
X-SPEED
CM/SEC
6.20
9.61
5
45
25
35
10
45
20
31 50
19 40
91 35 25
91 35 40
91 36
0
91 37 35
91 37 40
91 33 25
91 39 10
91 39 15
91 40 40
91 41 15
5
91 42
91 42 25
0
91 44
91 44 50
91 45 40
91 46 45
91 47 10
91 43 35
91 49 30
91 50 25
91 52 15
91 53 15
91 55
0
91 55 45
91 57 45
92 4 15
92
9 20
92 17 10
92 23
0
92 27 15
92 31 45
92 36
0
92 39 10
92 41 45
92 47 25
SMOOTHED
Y-SPEED
CM/SEC
5.21
2.42
DIST FROM
OBSERV PT
1152.6
1149.6
1145.6
1127.0
1126.1
1117.5
1109.0
1108.1
1092.5
1086.2
1077.3
1073.8
1057.4
1049.1
1040.8
1030.2
1026.2
1061.7
1004.3
996.0
979.7
971.0
956.2
X
(METERS)
1118.9
1126.4
1133.8
1153.5
1158.5
1166.5
1177.0
1179.3
1193.9
1200.6
1209.2
1213.2
1227.7
1235.9
1243.2
1252.3
1256.2
1226.4
1275.3
1283.0
1297.3
1304.8
1317.6
950.1
1323.2
933.9
885.0
850.2
801.6
768.8
746.6
724.5
704.7
690.6
679.6
656.6
1336.8
1377.3
1405.1
1444.0
1468.8
1489.0
1508.3
1525.0
1536.0
1544.7
1563.1
SMOOTHED
LINEAR
SPEED
4.86
5.95
SMOOTHEO-X
1126.4
1137.9
Y
(METERS)
566.2
573.3
577.9
574.9
581.4
581.2
578.8
580.9
574.9
573.7
570.7
570.5
562.3
560.1
556.2
551.6
549.3
568.8
538.6
535.2
527.4
523.0
515.6
512.9
504.2
476.8
455.6
426.1
404.1
394.5
383.6
372.9
364.0
357.1
343.0
SMOOTHED-Y
572.5
575.4
CCRRECTEC AZIM
IN KADIfNS
ELEVATION
IN RADIANS
.5135142
.5220703
.5287603
.5353310
.5425555
.54t9E63
.5491466
.5518127
.5541908
.5564671
.5583594
.5600808
.5612684
.5631571
1.5985518
1.5966238
1.5987227
1.5991316
1.5992956
1.5994245
1.5996434
1.5996674
1.6000793
1.6002492
1.6004921
1.6005891
1.6010499
1.6012999
1.6015328
1.6018477
1.6019706
1.6009270
1.6026484
1.6029153
1.6034491
1.6037400
1.6042498
1.6044658
1.6050476
1.6069392
1.6084177
1.6106969
1.6123943
1.6136299
1.6149375
1.6161160
1.6170957
1.6178465
1.6194959
.5638618
.5649534
.5649625
.5653403
.5660930
.5673526
.5684922
.5688071
.5695569
.5702136
.5702616
.5689C31
.5655352
.5604917
.5534141
.5566620
.5579565
.5575827
.5551355
.5532432
.5497044
AVERAGE
SPEED
(CM/SEC)
4.86
5.40
AVERAGE
SPEED
(KNOTS)
.10
.11
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
3.92
9.63
6.51
11.54
14.14
13.13
16.63
10.69
15.06
14.78
16.71
13.91
11.30
-9.37
12.50
14.90
39.42
16.40
2.26
.92
1.09
-0.30
-3.48
-2.86
-5.64
-2.49
-6.05
-5.93
-7.90
-6.26
-5.96
6.95
-7.17
-7.8.
-22.97
-8.69
19.26
-10.89
14.35
17.77
33.14
-8.39
-10.47
-21.60
26
9.10
27
31
32
33
34
11.91
10.17
9.32
7.15
6.24
5.22
4.04
4.23
-8.67
-8.07
-6.79
-4.72
-3.47
-3.39
-2.94
-3.32
35
5.05
3'.90
23
29
30
6.36
5.52
5.81
3.96
6.93
8.74
8.07
10.54
6.59
9.74
9.55
11.09
9.15
7.66
7.00
8.65
10.10
27.37
11.14
13.27
9.88
12.37
23.74
6.66
8.84
7.79
6.92
5.14
4.28
3.73
3.00
3.23
2.57-
1148.6
1160.2
1168.0
1174.3
1183.4
1191.3
1201.2
1207.7
1216.7
1225.6
1235.6
1243.9
1250.7
1245.1
1252.5
1261.5
1285.2
1295.0
1306.6
1315.2
1325.9
1345.7
1373.1
1408.8
1439.3
1467.3
1488.7
1507.4
1523.1
1535.2
1547.9
1563.1
578.1
579.2
580.5
580.3
578.2
576.5
573.1
571.6
568.0
564.4
559.7
556.0
552.4
555.6
552.2
547.5
533.8
528.5
522.0
517.2
510.9
497.9
478.8
452.8
428.6
408.2
394.1
383.7
373.5
364.7
354.7
343.0
5.44
5.53
5.22
5.37
5.65
5.84
5.18
6.20
6.42
6.61
6.86
6.98
7.01
7.01
7.09
7.22
8.06
8.18
8.38
8.43
8.57
9.10
8.74
8.75
8.64
8.47
8.16
7.83
7.51
7.18
6.92
18.48
.11
.11
.10
.11
.11
.11
.12
.12
.13
.13
.13
.14
.14
.14
.14
.14
.16
.16
.16
.17
.17
.18
.17
.17
.17
.17
.16
.15
.15
.14
.14
.36
DATE OF 09SERVATION = AUG
21, 1972
TIDE AT 1641
LOW
NUMBER
OF DATA POINTS =
26
DIST FROM POINT
OF OBSERVATION TO Y-AXIS = 2122.0 M_TEKS
CORRECTION IN
ZERO POINT = lu DEGREES 11 MINUTES 50 SECONDS
ANGLE OF ROTATION =
14 DEGREES 25 MINUTES 40 SECONDS
TIME
AZIMUTH
1311
1314
1316
1327
1330
1335
1340
30 31 55
30 35 20
30 36 30
30 47 15
31 51 40
31
1 4U
31
0 15
91 52
91 54
91 55
91 59
0
92
92
2
2
92
8
9
10
1345
1350
30 48 25
30 39 20
1355
11
14
0
30
30
92
92
92
12
1,4
5
13
1410
1415
READING
1
2
3
4
5
6
7
ELEVATION
1425
1430
1435
28 10
16
0
30 20 30
30 10 15
30
7
0
29 34 40
29
6
0
28 50 50
28 28
5
1440
1445
28 8 5
27 49 50
92
92
21
22
23
1450
1455
15 5
92
92
92
24
25
26
1515
27 33 10
27 32 15
27 33
0
27 40 40
27 50 40
28
5 20
14
15
16
17
18
19
1420
20
15
0
1510
SMOOTHED
READING
2
3
4
5
6
7
8
9
10
11
12
X-SPEED
CM/SEC
92
92
92
92
92
92
92
92
92
92
92
SMOOTHED
Y-SPEED
CM/SEC
6.31
13.64
2.26
8.84
2.61
2.72
1.95
-3.87
-6.08
-1.30
-4.66
-1.37
-2.03
-2.19
1.69
.91
.50
.39
-2.30
-1.74
-0.96
-0.88
15
0
10
10
25
C
40
4 35
5 35
6
5
6 50
6 50
7 10
7
40
40
15
3 15
8 45
8 10
8 10
7
8
GIST FROM
UBSERV PT
1317.2
1330.1
1338.3
1366.3
1374.9
1386.0
1389.6
882.6
875.6
558.6
550.8
545.5
529.5
525.0
520.3
517.2
1399.3
1403.6
506.7
500.6
872.1
867.0
1405.0
1407.5
496.5
491.0
867.0
1408.1
864.7
861.3
861.3
857.4
857.4
854.1
1408.6
1410.9
1466.3
1405.7
1403.6
1403.3
857.9
857.9
40
5
5
40
875.0
10
4
5
878.5
886.2
10
8
7
0
V
(METERS)
979.7
964.6
954.8
922.7
913.2
901.3
896.5
857.9
859.0
861.3
3
X
(METERS)
SMOOTHED
LINEAR
SPEED
4.44
9.51
1.56
5.99
1.77
2.04
1.76
1.71
1.18
.65
.58
CORRECTED AZIM
IN RADIANS
ELEVATION
IN RADIANS
.6067187
.6077143
.6080532
.6111811
.6124647
.6153730
.6149621
1.6034491
1.6039589
1.6042978
1.6054614
1.6058236
1.6062654
1.6064774
.6115200
.6085870
1.6070352
1.6073261
.6056300
.6020912
492.0
1.6074730
1.6076997
.6033988
1.6076990
488.5
486.0
479.2
471.1
467.9
461.4
.60C4178
.5900661
.5817289
.5773152
.5706994
1397.4
1394.9
459.3
455.4
1.6077979
1.6079319
1.6079319
1.6081328
1.6081028
1.6082468
.5648814
.5595710
1.6080798
1.6080738
1392.7
1391.7
1389.8
451.9
.5547246
.5544577
.5546766
1.5080788
1.6080303
1.6079319
452.3
453.6
1379.2
462.5
1377.6
1373.1
466.5
473.8
SMOOTHED-X
SMOOTHED-Y
1328.5
1344.9
1359.8
1375.7
1383.5
1391.7
551.6
541.9
533.3
524.9
520.8
514.7
1397.6
1402.6
1405.4
140b.9
1408.0
508.2
501.3
496.0
493.2
490.5
.5994731
.5569049
1.6073501
.5598139
.5640807
AVERAGE
SPEED
(CM/SEC)
1.6072061
1.6068912
AVERAGE
SPEED
(KNOTS)
4.44
6.47
3.10
3.55
3.18
2.98
.09
.13
.06
.07
.06
.06
2.80
2.66
2.50
.06
.05
.05
2.31
2.15
.05
.04
13
14
15
16
17
18
19
20
21
22
23
24
25
26
.38
-0.20
-0.32
-3.81
-0.34
-0.92
-0.96
-1.17
-0.63
-0.57
-1.50
-1.56
-1.86
-1.17
-0.56
-1.41
-1.94
-2.00
-1.99
-1.32
-1.39
-1.06
-0.78
-0.20
1.13
1.58
2.24
2.06
.41
.36
1.13
1.33
1.21
.96
1.02
.95
.60
.36
1.15
1.33
1.75
6.66
14C9.2
1408.6
1467.6
1405.2
1404.2
1401.4
1398.5
1395.0
1393.1
1391.4
1386.9
1382.2
1376.6
1373.1
488.8
484.6
473.8
472.8
466.8
462.9
458.7
455.5
453.2
452.6
456.1
460.9
467.6
473.3
2.06
1.91
1.86
1.82
1.78
1.73
1.69
1.65
1.60
1.54
1.52
1.51
1.52
2.40
.04
.04
.04
.04
.04
.03
.03
.03
.03
.03
.03
.03
.03
.05
DATE OF OBSERVATION = AUG
22, 1972
HIGH TIDE AT 1219
NUMBER
OF CATA POINTS = 29
DIST FROM POINT
OF OBSERVATION TO Y-AXIS = 2122.9 METERS
CORRECTION IN
ZERO POINT =
1 DEGREES 59 MINUTES 35 SECONDS
ANGLE OF ROTATION = 14 DEGREES 25 MINUTES 40 SECONDS
READING
TIME
AZIMUTH
ELEVATION
10
10
29
92 17
92 27
92 29
92 32
92 33
92 36
92 38
92 41
92 44
92 45
92 48
92 50
93
1
93 13
93 25
93 40
93 57
94
5
94 16
94 25
94 41
95
0
95 12
95 22
95 54
96 37
97 24
98 13
100 43
7
1010
6 10
30 22 50
30 33 50
30 44 25
30 56 50
31
6 40
31 18 40
A
1011
31 32 20
9
10
It
12
1012
1013
1014
1315
31
31
31
32
13
1020
14
15
16
17
1025
1030
1035
1040
32
32
18
19
20
21
22
23
24
25
26
27
28
29
1042
1045
1047
31
31
31
1050
30 56
0
30 15 30
29 42 45
28 32 40
25 25
0
1
2
3
4
5
6
READING
2
3
4
5
6
7
8
9
0
5
10 6
10 7
10
8
10
9
1053
1055
1057
11
0
11 2
11 5
11 7
1118
32
32
31
42
48
57
10
41
25
22
It
59
38
17
6
0
10
0
0
5
0
0
0
10
15
20
20
19 36 30
19
2
5
21 53 20
26 31
0
10
15
30
0
55
20
40
55
0
50
20
45
20
26
55
50
10
15
0
35
45
5
40
0
0
40
25
20
40
DIST FROM
OBSERV PT
801.6
746.6
735.4
723.2
714.3
703.2
692.8
678.9
670.3
662.9
653.0
643.7
606.1
568.4
533.6
497.5
463.1
447.8
428.9
413.4
389.6
365.7
350.9
340.6
309.7
275.4
246.2
221.5
168.9
SMOOTHED
X-SPEED
CM/SEC
SMOOTHED
Y-SPEED
CM/SEC
SMOOTHED
LINEAR
SPEED
12.72
40.31
15.86
15.64
14.95
16.96
15.91
14.23
-6.01
-20.37
-9.35
-9.49
-8.77
-10.67
-9.84
-9.24
8.44
27.10
11.05
10.97
10.40
12.02
11.23
10.18
X
(METERS)
1522.9
1575.2
1585.1
1595.5
1603.3
1613.2
1622.4
1634.3
1641.9
1648.0
1656.2
1664.5
1695.2
1719.9
1744.3
1768.3
1792.1
1801.2
1812.9
1823.2
1839.7
1854.1
1862.8
1865.7
1878.4
1889.5
1910.7
1940.0
1991.5
SMCOTHEG-X
1561.1
1585.2
1594.8
1604.1
1613.1
1623.3
1632.8
1641.4
Y
(METERS)
531.5
507.4
501.5
494.9
490.6
494.4
479.1
471.4
466.7
462.4
456.7
452.0
429.5
400.9
376.6
349.4
324.1
311.5
296.5
284.8
267.5
247.9
235.4
223.4
190.0
146.1
124.8
124.9
166.2
SMOOTHED-Y
513.5
561.3
495.7
490.0
484.7
478.3
472.4
466.9
CORRECTED AZIM
IN RADIANS
ELEVATION
IN RACIANS
.7249654
.7472651
.7504650
.7535449
.7571557
.7600160
.7635068
.7674834
.7702964
.7720898
.7746599
.7784409
.7874828
.7828644
.7819317
.7787318
.7752897
.7692048
.7631199
.7599200
.7569157
.7451328
.7356058
.7152195
.6606313
.5592554
.5317915
.5990593
.6798300
AVERAGE
SPEED
(CM/SEC)
1.6106369
1.6136299
1.6142337
1.6150124
1.6155673
1.6162720
1.6169493
1.6173945
1.6185032
1.6190341
1.6197629
1.6204646
1.6235438
1.6270346
1.6306934
1.6350329
1.6397962
1.6421367
1.6452646
1.6480507
1.6527531
1.6580875
1.6617463
1.6644633
1.6737721
1.6864721
1.7000717
1.7143011
1.7580337
AVERAGE
SPEED
(KNOTS)
8.44
11.55
11.48
11.41
.17
.23
.23
.22
11.26 "
.22
11.30.22
11.37.22
11.36.22
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
26
27
28
29
12.19
12.61
26.24
7.08
8.36
8.18
9.02
6.32
12.26
5.76
10.70
7.63
7.32
7.23
6.74
4.94
12.50
11.41
23.36
6.68
-3.14
-3.17
-18.31
-6.21
-8.45
-3.90
-3.53
-7.17
-14.71
-7.29
-12.21
-5.98
-9.17
-12.26
-16.09
-16.54
-27.38
-12.06
-11.09
-1.98
8.79
9.01
19.20
5.65
7.34
7.25
7.03
5.74
11.49
5.57
9.74
7.07
7.02
8.54
10.47
10.36
18.06
9.96
18.27
3.15
1648.7
1656.3
1672.0
1693.2
1719.3
1744.3
1768.4
1787.4
1802.1
1812.4
1825.3
1839.3
1852.2
1960.9
1869.0
1877.3
1892.9
1913.4
1947.4
1991.5
462.0
457.1
446.1
427.5
402.1
375.4
349.9
328.3
310.7
297.6
282.9
266.7
250.3
235.6
216.3
186.5
153.6
131.9
118.6
106.2
11.07.22
.21
.23
10.02.20
9.46
.19
10.93
11.48
9.11
3.81
8.43
8.57
9.37
9.43
8.35
8.28
8.29
8.36
8.46
9.77
8.83
9.11
5.32
.18
.17
.17
.17
.16
.17
.16
.1E
.16
.16
.17
.17
.17
.18
.10
DATE OF OBSERVATION = AUG
22v 1972
TIDE AT 1730
LOW
NUMBER OF DATA POINTS =
34
DIST FROM POINT
OF OBSERVATION TO Y-AXIS
CORRECTION IN
ZERO POINT =
2 DEGREES
2122.9 M_TLRS
MINUTES 15 SECONDS
14 DEGREES 24 MINUTES 40 SECONGS
ANGLE OF ROTATION =
READING
=
0
DIST FROM
O6SERV PT
TIME
AZIMUTH
1
2
3
1325
1330
25 43
25 40
0
1335
91 35 40
91 42 40
1149.6
1071.2
25 24 50
91 47 55
1340
1342
1345
1347
1019.1
4
25
1 20
24 47 20
24 22
5
24
7
0
91 55 10
91 57 30
92
1 25
92 4 25
1350
1352
954.8
935.9
905.7
883.8
23 39 20
23 17 45
22 56 45
22 34 40
92
8 20
92 11 0
92 15 55
856.8
839.3
5
6
7
8
9
10
11
12
1355
1357
14
0
13
14
15
16
17
14
14
14
14
2
4
6
8
18
19
20
ELEVATION
0
21
21
20
19
19
47 15
11 15
33 15
56 15
7 25
1410
1411
1412
18
18
17
17
33 20
21
22
1413
1414
16
23
24
25
1415
1416
1417
26
27
28
29
30
31
32
33
34
1418
1419
14 9
1420
1421
1422
1425
1424
1425
1426
10
36
12
16 41
1
15
30
20
20
35
15 28 20
14 54 20
14 9 15
13 37 50
12 53 20
12 19 0
it 40 40
10 59 20
10 27 20
9
49
9
14 40
55
0
8
0
92
92
92
92
92
92
18
23
25
23
31
34
92
92
92
92
35 30
37
0
30
30
55
50
10
15
39
0
39 40
X
(METERS)
Y
(METERS)
1219.5
1279.6
1317.9
13E4.7
1377.4
1397.5
1412.7
1430.3
1441.3
711.1
660.5
°
624.3
580.3
565.8
542.2
526.0
504.4
489.8
809.0
793.9
766.2
1463.1
1472.5
753.5
1495.3
1481.5
-1508.5
1515.4
468.1
455.2
430.6
416.9
415.9
389.1
372.7
1516.7
1520.1
1524.3
1524.3
363.7
356.2
345.8
340.2
1526.0
1526.5
332.2
322.9
764.4
727.2
712.7
707.0
700.2
691.4
663.5
1489.2
92 40 55
92 42
5
92 43 40
683,2
678.2
92 43 25
92 44 0
672.7
670.3
1529.2
1525.2
1523.4
314.1
308.6
299.7
92 44 40
92 45 25
667.6
664.5
92 46
662.2
1523.1
1522.1
293.0
283.9
0
92 47
0
92 47 10
92 48
0
92 48 20
92 47 35
92 48 10
671.6.
CORRECTED AZIM
IN RADIANS
.6668369
.6645097
1.E103311
1.6110339
1.6125333
1.6132401
1.6126343
1.6147695
1.6156662
.5403963
.5336816
.5238E37
.5168341
1.6160291
1.6164669
1.6170487
1.6172407
.5078169
.4962529
1.6176036
1.6179454
.4865819
.4766920
.4635775
1.6184043
1.6183323
1.6185032
.4544374
.4414945
1.6186952
1.6189141
276.9
1522.0
1519.4
654.3
653.0
268.6
261.1
1520.0
1518.4
.4203555
.4083333
254.2
247.0
655.9
653.6
1513.3
1514.0
.3990245
.3878750
242.0
237.7
.3778855
.3721671
.4315079
SMOOTHED
LINEAR
SPEED
2
17.61
16.13
10.87
-15.18
13.95
3
1272.3
13.02
9.08
665.5
1320.7
1353.3
13.95
621.9
590.3
13.49
4
1.6081268
1.6089035
.6170202
.6105964
.5968648
.5863324
.5752789
.5645163
.5503102
SMOOTHED
Y-SPEED
CM/FFC
-14.53
-10.53
1.6042378
1.6049756
1.E0E1145
1.6069372
.6294082
.6231284
1521.4
SMOOTHED-Y
1.6021366
.653260E
.6491887
.6418442
.6374567
658.2
657.5
SMOOTHEO-X
1.5986238
1.E006601
.6600953
SMOOTHED
X-SPEED
CM/SEC
READING
EL=VATION
IN YAOIAtiS
AVERAGE
SPEED
(CM/SEC)
1.6190350
1.6193759
1.6194239
1.6196668
1.6197628
1.6195439
1.6197148
AVERAGE
SPEED
(KNOTS)
.27
.27
12.02.24
5
22.10
6
8.89
7
8
14.69
9
14.01
10
11
12
13
14
15
16
17
18
7.82
19
4.25
-22.97
-10.06
-17.06
-9.70
-16."9
-9.11
-16.45
-9.43
-10.91
-11.53
-12.28
-14.49
-18.28
-14.92
-13.06
20
21
3.26
-13.33
1.26
2.71
-12.74
-14.52
-13.08
-12.89
-11.E9
22
23
24
25
26
27
28
29
30
31
32
33
34
9.12
13.29
5.96
2.51
5.36
5.60
9.76
6.44
4.90
-17.41
-1.74
-3.40
-1.74
-1.09
-0.60
-13.72
-12.64
-13.57
-1.49
-0.78
-0.66
-12.69
-12.64
3.42
10.61
-9.18
-7.56
-?. 34
-2.02
-4.00
19.13
8.05
13.50
7.59
12.80
7.20
12.69
6.72
6.72
7.63
8.10
10.48
11.63
9.43
8.24
8.23
7.68
1379.8
1395.3
1413.5
1428.1
1444.9
1459.0
1474.9
1485.6
1488.7
1495.1
1561.3
1513.5
1517.4
1520.3
1522.9
1524.8
8.86
1527.2
7.85
7.81
7.30
8.30
7.61
8.15
7.67
7.60
2.44
-6.69
5.86
16.13
1525.6
1527.0
1525.9
1523.9
1522.9
1522.2
1521.8
1521. 0
1520.5
1519.3
1517.2
1515.2
1514.0
5E2.3
544.7
524.2
506.7
487.4
12.85
.25
11.70
.23
.23
12.13.24
12.26.24
11.78
471.0
11.32.22
451.3
434.2
421.1
11.41
407.3
10.61
392.6
375.2
364.2
355.2
347.4
339.4
331.13
323.1
315.2
307.5
300.5
292.2
10.49
10.49
10.52
10.49
10.44
10.40
284.6
276.5
268.9
261.3
254.1
247.7
242.2
237.7
11.01.22
10.77
.22
.21
.21
.21
.21
.21
.21
.21
.20
10.34.20
10.31.20
10.2E.20
10.21.20
10.16.20
10.12.20
10.07.20
10.04.20
10.00.20
9.95
9.58
9.85
9.79
8.39
.20
.19
.19
.19
.17
DATE OF OBSERVATION = SEPT
8, 1972
HIGH TIDE AT 1342
NUMBER OF DATA POINTS = 29
DIST FROM POINT
OF OBSERVATION TO Y-AXIS = 2122.9 METERS
CORRECTION IN
ZERO POINT =
0 MINUTES
U DEGREES
0 SECONDS
ANGLE OF ROTATION =
14 DEGREES 25 MINUTES 40 SECONDS
READING
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
26
27
28
29
TIME
AZIMUTH
1131
1132
1133
1134
1136
1137
1138
1139
1140
1141
1142
1143
1144
1145
1146
1147
1148
1150
1151
1152
1153
1154
1155
1156
1157
1158
1159
27 49 40
28 37 40
29 20 20
30
3 40
31 33 43
32 14 50
12
0
1221
READING
2
3
4
5
6
7
8
9
ELEVATION
33
6 30
34
35
1
36
37
20
5 20
3
0
3 40
38 7 40
39 14 40
40 10 20
41 21 40
42 23
0
43 32 20
46
4 30
47 22 20
48 47 50
50
6 30
51
53
54
56
57
59
60
97
SMOOTHED
X-SFEED
CM/SEC
28.93
31.76
44.30
23.18
38.59
28.53
33.85
35.42
91
91
91
Si
91
91
91
91
92
92
92
92
92
92
92
92
92
45
47
47
50
53
55
55
57
21
24
24
40
0
40
0
50
20
20
40
0
20
0 40
3 50
5 20
7
5
8
20
11
5
15
0
14 20
92 16 30
92 21 10
0
92
92
92
92
92
92
40
0
92
8
0
92 31 40
92 34 10
92 34 20
32
0
5
0
37 40
6
56 40
18
0
.39
-3.80
-3.59
1.56
2.56
.80
-0.22
0
0
24
5
27 30
29
0
30 20
SMOOTHED
Y-SPEED
CM/SEC
4.71
40
DIST FROM
OBSERV PT
1040.8
1027.7
1021.4
999.7
966.1
953.5
953.5
934.6
913.8
911.3
888.0
877.3
865.2
856.8
838.8
814.4
818.5
805.5
778.8
776.1
763.5
763.5
763.0
745.4
737.8
731.3
724.9
713.1
712.3
X
Y
(METERS)
(METERS)
1352.6
1371.9
1385.3
1409.7
1451.7
1468.7
1479.2
1503.0
1529.6
1543.0
1570.0
1589.5
1610.3
1626.6
1651.3
1677.1
1688.8
1726.3
1754.9
1773.3
1794.6
1811.9
1831.0
1856.5
1876.9
1898.1
1917.8
1942.9
2386.6
699.9
701.b
706.5
700.6
694.8
693.6
703.4
699.4
695.1
703.0
694.9
696.6
697.1
698.4
693.7
681.6
693.9
701.1
686.4
692.9
689.3
697.3
705.0
696.1
695.6
695.9
695.2
690.0
661.7
'SMOOTHED
LINEAR
SPEED
17.59
19.C6
26.68
14.07
23.17
17.19
20.31
21.25
SMOOTHED-X
1369.9
1389.0
1415.6
1443.4
1466.5
1483.6
1503.9
1525.2
SMOOTHED-Y
702.7
702.9
700.6
696.3
697.3
698.8
699.3
699.1
CORRECTED AZIM
IN RACI.NS
ELEVATTCN
IN RADIANS
.7374959
.7514584
.7638704
.7764744
.9026547
.8146289
.8296590
.845EC98
.8642267
.o81CG22
.8986475
.9172644
.9367540
.9529477
.9736969
.9915400
1.6117174
1.0559701
1.0786116
1.1034e14
1.1263651
1.1512378
1.1782901
1.2052442
1.2309409
1.2582848
1.2838826
1.3154911
1.9500170
AVERAGE
SPEED
(CM/SEC)
17.59
1.6015329
1.6019226
1.6021146
1.6027953
1.6039080
1.6043458
1.b043458
1.6050236
1.6057996
1.6058956
1.6068163
1.6072541
1.6077639
1.6081268
1.6089275
1.6100671
1.6098722
1.6105020
1.6118605
1.6120045
1.6126952
1.6126852
1.6127092
1.6137019
1.6141397
1.6145266
1.6149135
1.6156422
1.6156902
AVERAGE
SPEED
(KNOTS)
.35
18.32.36
21.11.42
18.29
.3E
19.11.38
.37
18.83
19.02.37
19.27.38
11
12
13
14
15
16
17
13
19
20
21
22
23
24
25
26
27
28
79.14
66.24
53.E8
39.64
79.60
39.66
79.55
56.56
57.92
58.52
58.92
57.94
50.20
58.33
60.23
464.87
24.27
91.99
-31.27
-16.11
-16.26
-5.20
-2.32
3.27
2.10
4.92
1.69
-1.61
-4.99
-3.33
-12.50
-15.74
-7.38
-28.95
-2.71
-15.86
51.06
40.93
39.43
35.92
+7.79
23.87
47.75
34.06
34.77
35.12
35.49
35.12
30.89
36.54
36.41
279.46
14.65
27.21
1796.3
1636.0
1874.2
1910.0
1957.3
2005.4
2053.1
2087.0
2121.8
2156.9
2192.2
2227.0
2263.1
2298.4
2334.6
2613.5
2919.3
3250.5
624.7
615.0
605.3
602.2
600.8
604.7
605.9
603.9
609.9
638.9
606.0
601.0
593.5
584.0
579.6
562.2
523.1
471.0
33.29.65
33.37.67
34.21.67
34.32.69
35.11.69
33.92
34.62
34.59
34.E0
34.62
34.66
34.68
34.76
34.83
34.88
43.32
.67
.68
.63
.68
.68
.69
.63
.69
.69
.69
.85
31.28.62
13.10.26
DATE OF OBSERVATION = SEPT
8, 1972
HIGH TIDE AT 1342
NUMBER OF DATA POINTS =
28
DIST FROM POINT
OF OBSERVATIO;4 TO Y-AXIS =
2122.9 METERS
CORRECTION IN
ZERO POINT =
2.1 OEGRLES
ANGLE OF ROTATION = 14 DEGREES 25 MINUTES 4o SECONDS
READING
TIME
AZIMUTH
ELEVATION
16
17
18
19
20
21
22
23
1131
1135
1136
1137
1138
1139
1140
1141
1142
1143
1144
1145
1146
1147
1148
1150
1151
1152
1153
1154
1155
1156
1157
24
1158
25
1159
1160
1221
1227
30.8
33.6
33.7
36.4
37.9
39.6
41.4
43.0
45.1
47.7
50.0
52.7
55.5
58.0
61.2
67.9
71.1
74.3
77.5
80.9
84.2
87.5
90.8
94.6
97.8
100.7
140.0
145.0
358.2
358.1
357.9
357.9
357.8
357.8
357.7
357.7
357.7
357.5
357.4
357.3
357.2
357.1
357.1
357.0
357.0
357.0
357.0
357.0
357.0
357.0
357.0
357.0
357.3
357.1
358.4
358.5
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
26
27
28
READING
2
3
4
5
6
7
6
9
10
GIST FROM
O9SERV PT
1018.2
964.6
872.7
872.7
833.0
833.0
796.7
796.7
796.7
732.9
704.7
678.5
654.3
631.7
631.7
610.6
610.6
610.6
610.6
610.6
610.6
619.6
610.6
610.6
610.6
631.7
1145.6
1222.0
X
Y
(METERS)
(METERS)
1379.8
1452.0
1517.0
1547.3
1590.0
1609.2
1651.5
1669.7
1694.0
1756.8
1795.6
1836.4
1876.0
1910.3
1943.8
2019.3
2053.0
2087.0
2121.1
2157.3
2192.3
2227.1
2261.6
2300.7
2333.0
2370.0
3137.5
3250.5
696.1
693.0
628.0
655.9
640.2
655.7
642.3
655.2
671.4
634.9
624.1
615.1
605.9
594.8
605.8
601.7
606.6
609.5
610.6
609.6
606.6
601.6
594.6
584.1
573.3
581.3
532.0
471.0
SMOCTHED
SMOOTHED
X-SPEED
CM/SEC
Y-SPEED
CM/SEC
LINEAR
-9.89
18.43
1449.6
-22.34
57.42
1505.4
672.4
659.0
49.23
1551.4
641.4
29.09
93.05
76.70
51.25
57.94
44.25
47.07
58.45
69.98
-29.34
15.39
-7.53
8.35
9.70
-4.13
-17.31
SMOOTHED
SPEED
32.11
35.06
27.02
28.72
35.16
43.26
CORRECTEC AZIM
IN RADIANS
.7527204
.8015896
.8033350
.8504589
.9766388
.9063894
.9377254
.9656507
1.0023026
1.0476812
1.0878238
1.1349477
1.1838169
1.2274502
1.2833007
1.4002378
1.4560864
1.5119390
1.5677895
1582.2
1616.9
1643.5
1671.7
1706.8
1748.8
SMOOTHED-Y
650.6
646.1
651.1
656.3
653.8
643.5
1.6022129
1.6039583
1.6074489
1.6074489
1.6091943
1.6091943
1.6109396
1.6109396
1.6109396
1.6144303
1.6161756
1.6179209
1.6196662
1.6214116
1.6214116
1.6231569
1.E2315t9
1.6231569
1.6231569
1.6231569
1.6231569
1.6231569
1.6231569
1.6231569
1.6231569
1.6214116
1.5987223
1.5969770
1.6271307
1.6847266
1.7423225
1.7999184
1.3662409
1.9220915
1.9727061
2.6566208
2.7455873
AVERAGE
SPEED
SMOOTHED-X
ELEVATION
IN RADIANS
(CM/StC)
AVERAGE
SPEED
(KNOTS)
.36
26.23.52
30.07.59
30.3E.60
30.95
.61
30.51
.60
30.33.60
39.71
.61
18.43
31.81
.63
10
11
12
37.19
-2.53
22.36
19.96
22.55
13
14
15
31.45
34.34
37.03
34.55
+1.66
21.61
46.95
37.98
31.63
32.09
34.34
3E.14
37.24
34.06
36.60
271.41
24.14
1.97
-1.E1
-9.60
-2.52
4.13
1.34
-0.55
-6.55
6.04
6.73
3.78
-0.91
-5.09
-0.49
-3.15
-18.58
-1.63
18.90
16
17
18
19
20
21
22
23
24
25
26
27
28
29
33.26.94
37.43
-3.28
20.62
22.84
20.79
25.12
12.99
28.17
23.12
19.35
19.67
20.73
21.69
22.55
20.44
22.04
163.24
.37
1547.5
15E7.5
1589.9
1608.8
1629.4
1651.6
1672.4
1697.4
1723.3
1751.5
1774.3
1793.3
1812.5
1833.1
1854.8
1877.2
1897.6
1919.6
2082.4
2386.6
697.6
698.1
696.2
697.3
696.4
691.2
689.7
692.2
693.8
693.5
689.5
693.2
697.2
699.5
698.9
695.9
695.6
693.7
682.3
661.7
19.58
19.61
19.86
19.78
.39
.39
.39
.39
19.34.39
20.04.39
20.09.40
20.38.40
19.61
.39
20.03.39
20.18.40
20.14.40
20.12.40
20.15.40
20.21.40
20.30.40
20.31.40
20.37.40
25.29.50
11.20.22
APPENDIX V
Appendix V contains data collected during the January 2 - 5, 1973,
cruise offshore from Newport to Moolack Beach.
The map shows the 40-hour
paths of six surface drogues, identified by color, with the vertical axis
approximating the trend of the coastline.
The drogues were set out in
a
line beginning southwest of Yaquina Head; points of release are circled.
Also included is a listing of the hydrographic data collected at times of
tidal changes during the period of drogue tracking.
above Station D-1.
Columns are identified
HYDROGRAPHIC DATA
CRUISE Y7301A
3-5 January 1973
Station D-1
Latitude 44 42.8 N
Wind Direction 12°
Longitude 124 08.8 W
Time 1855 (Jan. 3)
Swell Direction 30°
Wind Velocity 08 Knots
Height 07 Feet
Period 10 Seconds
Depth
Temperature
Salinity
e.
(°/oo)
0
9.26
10
9.35
20
30
10.16
10.10
30.98
31.00
32.30
32.95
23.97
23.97
24.84
25.36
Station D-2
Wind Direction 07°
Latitude 44 43.4 N
Wind Velocity 11 Knots
Longitude 124 09.7 W
Time 0220 (Jan. 4)
Swell Direction 31°
0
10
20
30
9.20
9.87
9.53
9.62
Height 05 Feet
Period 08 Sec.
30.92
32.08
23.93
24.73
32.38
25.01
32.63
25.19
Station D-3
Wind Direction 09°
Latitude 44 42.5 N
Longitude 124 09.4
Wind Velocity 05 Knots
Time 0900 (Jan. 4)
Swell Direction 32°
Height 04
Period 07
0
9.01
10
20
30
9.75
10.01
10.07
30.92
32.08
32.38
32.63
23.96
24.75
24.93
25.11
Station D-4
Wind Direction 08°
Latitude 44 42.7 N
Wind Velocity 08 Knots
Longitude 124 10.5 W
Time 1340 (Jan. 4)
Swell Direction 31°
10
8.93
9.52
20
9.77
30
9.92
0
Height 02 Feet
Period 07 Sec.
30.83
23.90
32.42
32.67
32.73
25.05
25.20
25.22
Station D-5
Latitude 44 44.9 N
Longitude 124 08.9 W
Time 1947 (Jan. 4)
0
10
20
30
40
8.88
9.25
9.54
10.01
10.42
Station D-6
Latitude 44 40.1 N
Longitude 124 12.0 W
Time 0310 (Jan. 5)
0
10
20
30
9.00
9.16
10.20
10.17
Wind Direction
Wind Velocity 07 Knots
Swell Direction 31°
Height 04 Feet
Period 08 Sec.
30.82
31.27
32.36
32.80
30.85
23.90
24.19
25.00
25.26
23.68
Wind Direction 19
Wind Velocity 10 Kn ots
Swell Direction 31°
Height 04 Feet
Period 07 Sec.
30.82
31.27
32.36
32.80
23.88
24.21
24.89
25.23
Station D-7
Wind Direction 25
Latitude 44 41.0 N
Wind Velocity 14 Knots
Swell Direction 31
Height 03 Feet
Period 07 Sec.
Longitude 124 10.1W
Time 0930 (Jan. 5)
0
10.11
10
20
30
10.20
10.21
9.78
Station D-8
Latitude 44 43.5 N
Longitude 124 07.4 W
Time 1410 (Jan. 5)
0
10
20
30
8.69
9.05
32.95
32.78
32.60
25.36
31.71
24.45
25.21
25.07
Wind Direction
Wind Velocity 12 Knots
Swell Direction 31°
Height 03 Feet
Period 07 Sec.
10.08
31.36
31.79
32.35
24.35
24.63
24.89
10.19
32.83
25.25
Station D-9
Latitude 44 40.4 N
Longitude 124 10.1 W
Time 2010 (Jan. 5)
0
10
20
30
8.69
9.69
10.23
10.13
Wind Direction
Wind Velocity
Swell Direction 29°
Height 03 Feet
Period 06 Sec.
31.28
31.92
32.58
32.75
24.28
24.62
25.05
25.20
0
i
11
I
u
n
Il
to