0
of
HA
OREG
SCIENCE CENTER
YE UNIVERSITY
97365
I"
twC
MAR,
365
8 1986
OCEANOGRAPHY
MOORED TEMPERATURE AND
CONDUCTIVITY OBSERVATIONS
DURING AIWEX
by
Murray D. Levine
Steve A. Gard
Jay Simpkins
Office of Naval Research
N00014-84-C-0218
NR-083-102
College of Oceanography
Oregon State University
OREGON STATE UNIVERSITY
Reference 86-9
June 1986
Data Report 123
Reproduction in whole or part Is permitted for any
purpose of the United States Government.
Unclassified
SECURITY CLASSIFICATION OF
"i
PAGE
fl I M I
1.1!'. I
COMPLETING FORM
REPORT NUMBER
I
NO. 3.
2.
86-9
.
TITLE (end Subtitle)
4.
RECIPIENTS CATALOG NUMBER
S. TYPE OF REPORT 8 PERIOD COVERED
MOORED TEMPERATURE AND CONDUCTIVITY
OBSERVATIONS DURING A I WEX
Data Report
PERFORMING ORG. REPORT NUMBER
7
I. CONTRACT OR
MURRAY D. LEVINE
NUMBER(.)
N0004-814-C-0218
STEVE GARD
JAY SIMPKINS
9. PERF
MING ORGANIZATION NAME AND
ID. PROGRAM ELEMENT, PROJECT, TASK
AREA 6 WORK UNIT NUMBERS
College of Oceanography
Oregon State University
OR
NRO831O2
97331
II. CONTROLLING OFFICE NAME AND ADDRESS
REPORT DATE
Office of Naval Research
Ocean Science & Technology Division
Arlinaton. VirQinia
June 1986
13. NUMBEROFPAGES
22217
$4. MONITORING AGENCY NAME & ADDRESS(sf dIIi.r.nt
195
lro.ii Controlltná Ottlc.)
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DISTRIBUTIoN STATEMENT (of
17.
th.
abetted
.nt.r.d In Block 20, Ii dlfI.r.nt trac% R.pert)
18. SUPPLEMENTARY NOTES
IS. KEY WORDS (Continue on
.10. If
end i0.nttty by block nionb.r)
Arctic Internal Wave Experiment (AIWEX)
Temperature and Conductivity
Internal Waves
2D.
ABSTRACT (Continu, on
r,,'.r.. aid.
If
end id.nsify br block
series are presented from 13 temperature and 5 conductivity sensors
(Sea—Bird Electronics) suspended below the ice during March—April 1985 near
Time
7140N,
11414°W as part of the Arctic Internal Wave Experiment (AIWEX)
The
were located between 80 and 508 m depth; horizontal separations
.
sensors
ranged from 150 to 1000 m.
DD
FORM
I
—
73 l4i3
Selected spectra and coherences are also included.
-__________________
EDITION OF I NOV 65 IS OISOLETE
S-/N 0i02-014- 6601
I
SECURITY CLASSIFICATION OF THIS PAGE
Znte,.
MOORED TEMPERATURE AND
CONDUCTIVITY OBSERVATIONS
DURING AIWEX
Murray D. Levine
Steve R. Card
Jay Simpkins
College of Oceanography
Oregon State University
Corvallis, OR 97331
Table of Contents
ACKNOWLEDGEMENTS
i
INTRODUCTION
1
INSTRUMENTATION
2
ANALYSIS
10
OBSERVATIONS
14
TABLE OF DAILY MEAN, STANDARD DEVIATIONS AND SKEWNESS
15
TIME SERIES OF TEMPERATURE, CONDUCTIVITY, AND PRESSURE
Fifteen-minute averages
29
TIME SERIES OF TEMPERATURE AND SALINITY
Fifteen-minute averages
32
TIME SERIES OF TEMPERATURE, CONDUCTIVITY, AND PRESSURE
One-minute averages
35
TIME SERIES OF TEMPERATURE AND SALINITY
One-minute averages
115
SPECTRA OF TEMPERATURE AND SALINITY
155
VERTICAL COHERENCES
175
HORIZONTAL COHERENCES
185
ACKNOWLEDGEMENTS
We
thank James Morison for providing enthusiasm and guidance in the
initial planning of AIWEX and for being an "Arctic hero" role model
throughout the experiment.
Special thanks are extended to Clayton
Paulson and Rick Baumann without whose expertise and muscle this project
would not have succeeded.
The excellent organization and administration
of the logistical support by Andy Heiberg, Allen Hielscher and Imants
Virsnieks, made the AIWEX camp a comfortable place to be, even though
"it's no picnic out there".
We appreciate the endless toil of Matt Valley
in running the mess hail and providing entertaining stories and philosophy.
The efforts of Ed Siefert in making preparations and Dennis Bartow
for calibration of the instruments are much appreciated.
The cover illus-
tration and AIWEX logo were kindly provided by Barbara Levine.
The support for this research by the Office of Naval Research through
contract N00014-84-C-0218 code 420 P0 (this project) and code 425 AR
(logistical support) is gratefully acknowledged.
INTRODUCTION
This report presents observations from moorings of temperature, conductivity and pressure, made during the Arctic Internal Wave Experiment (AIWEX)
in March-April 1985.
•
The main objectives of AIWEX were:
To make comprehensive measurements of internal waves and microstructure in the Arctic Ocean, and
•
To identify important processes that affect the Arctic internal
wave field.
To meet these objectives, observations at a variety of horizontal, vertical and temporal scales made by investigators from many institutions will
need to be analyzed.
The purpose of the temperature and conductivity measurements was to
provide time series from which inferences could be made about the vertical
displacement of the internal waves.
Specific goals of this project
include:
•
To verify the suspected low spectral level of the internal wave
field in the Arctic Ocean,
•
To estimate in detail the coherence structure of the highfrequency internal wave field from horizontal and vertical arrays
of sensors, and
•
To compare variations of the internal wave field with variations
in the surface stress, eddy field and dissipation.
2
INSTRUMENTATION
A total of 13 temperature (SBE-3), 5 conductivity (SBE-4) and 2 pressure (Digiquartz) sensors were deployed on 7 moorings (Figs. 1 and 2).
The locations and technical details of the sensors are given in Table 1.
Each mooring consisted of an individual 3-conductor, shielded electrical
cable (Belden #8771) for each sensor attached to a strength member of 1/4"
Samson Dura-Plex Braid (Composite Polyester/Polyolefin).
The moorings
were secured at the surface of the ice and kept taut by a steel weight at
the bottom.
A schematic of the data acquisition system is shown in Fig. 3.
The
output of each sensor is a frequency that was fed into a 20-channel SBE
11/20 (Sea-Bird Electronics) Deck Unit.
The Deck Unit digitized the
frequency signal using a highly accurate hybrid period counting technique.
A PDP 11/23 computer acquired the data through an RS-232 line and averaged
values over 1 minute intervals.
The data were then written on 8" flexible
disks and displayed on a terminal and printer.
For limited periods data
were also recorded at a 1 s sampling rate.
There was significant data loss during the first week of operation,
apparently due to a bad electrical contact on a board in the SBE 11/20
Deck Unit.
After cleaning the contacts, the problem did not reoccur.
Small gaps in data throughout the experiment were due to power interruptions (both scheduled and unexpected).
Noise spiking was present on some
channels due to a timing error in the Deck Unit; we believe this did not
significantly degrade the observations in the internal wave frequency
band.
Calibration
All the temperature and conductivity sensors were calibrated in
November 1984 at the Northwest Regional Calibration Center (NRCC).
The
conductivity calibrations are referenced to the Practical Salinity Scale
(1978) which defines the conductivity at 35 ppt, 15°C, 0 pressure to be
4.2914 Siemens/meter.
The factory calibrations of the new pressure
AIWEX CAMP
AIWEX CAMP
I
I
700
I
I
I
I
I
I
I
I
I
I
I
I
I
I
700
+S13
'03
500-
500--
N
N
300--
300-100--
100--
0
a)
a)
4-I
-
.01
a)
E —100 -
E—ioo-
.11
c.f+PA
-
+Pl
+DI
•
—300
—500
+MP
'02
—500-
02
—700
—700
Fig.
a)
.
Location of the 7 temperatureconductivity moorings:
1
central
(C)
inner (H, (2,
3 outer (01, 02,
3
(3),
03).
1.
.
•
-
I
—700--500—300--100 100 300 500 700
meters
.01
(2
-
—300
+sw
MK
-
I
I
I
I
I
I
I
I
—700---500—300—100 100 300 500 700
meters
Plan view of AIWEX ice camp
b). Location of moorings in relation to
measurements made by other investigators.
The labels are abbreviations of the names
of the P1's.
MO -
Morison
P1
—
Pinkel
DI
-
Dillon
PA MP -
Paulson
Morison/Pinkel
EW
P0
SW
MK
- Ewart
- Podney
— Swift
- McPhee/Kolle
)T,C(80m)
)T,C(185m)
()T(249m)
)T(242m)
I
?T,C(257m)
''T(262m)
01,02,03,
13
C)T,C(303m)
11,12
SATELLITE
MOORINGS
(508m)
CENTRAL
MOORING
Fig. 2.
Schematic of temperature-conductivity moorings indicating
the depths of temperature (T) , conductivity (C), and
pressure (P) sensors.
5
Table
1.
Depth
Mooring
m
*
Information about the 20 sensors deployed during AIWEX,
including location and calibration data.
Type of
MeasureManument
facturer t
Serial
Number
Calibration Differences*
Absolute (Units: xlO 30C
or xlO 4S/m)
Sens itivity**
Mean
S.Dev.
(% chance)
C
80
T
SBE
612
9.1
1.6
1.4
C
80
C
SEE
208
5.7
8.8
1.0
C
185
T
SBE
609
11.0
1.7
1.0
C
185
C
SEE
209
-2.3
15.7
1.7
C
242
T
SBE
611
9.0
1.5
1.0
C
257
T
SBE
613
13.0
1.3
0.9
C
257
C
SEE
211
7.2
6.1
1.0
C
262
T
SBE
614
1
1.7
0.3
C
303
T
SBE
616
12.4
1.2
0.8
C
303
C
SBE
212
10.9
7.3
0.9
C
508
T
SEE
615
10.7
1.5
0.6
C
508
C
SEE
210
4.4
7.5
1.0
C
508
P
PARO
Ii
249
T
SBE
428
2.1
1.8
0.5
12
249
T
SEE
416
-5.1
1.8
1.3
13
253
T
SBE
610
13 7
1.2
0.6
13
253
P
PARO
01
249
T
SBE
424
02
249
T
SBE
436
3.6
2.1
0.2
03
249
T
SEE
435
-4.1
2.2
0.6
21432
.
21449
Based on the difference between pre-AIWEX calibrations and post-AIWEX
interconiparisons.
** Sensitivity
is defined to be the change in temperature or conductivity per
change in sensor frequency.
t
SBE
PARO
=
Sea-Bird Electronics
Paroscientific,
Inc.
Cent ra
a'
Sate! ii te
Mooring
Fig. 3. Schematic of data acquisition system located
in a hut over the central mooring.
7
sensors were used as supplied by the manufacturer (Paroscientific, Inc.).
Pressures were converted to depth assuming a constant water density of
1028.13 kg/rn3 in order to be consistent with the measurements made with
the Arctic Profiling System (APS) by James Morison (University of Washington, Seattle).
After AIWEX the behavior of the temperature and conductivity sensors
were compared by placing all the sensors in the OSU calibration tank.
While this comparison was not directly traceable to an absolute standard,
the sensors could be compared with two SBE-3 sensors (#544 and #607) that
are used routinely in the OSU calibration lab as secondary standards.
The
differences between the pre-AIWEX calibrations and post-AIWEX intercomparison are given in Table 1 for each sensor.
The difference in sensitivity between pre- and post-AIWEX calibrations was small for all sensors
--
less
than 2%.
Sensitivity is defined
to be the change in temperature or conductivity per change in sensor frequency; the values in Table 1 were estimated by measuring the change in
the sensor frequency over the range in temperature from -0.0392 to
0.0396°C or over the range in conductivity from 2.7360 to 2.8766 S/rn.
The difference in the absolute calibration varied with the sensor but
was no larger than 0.015°C or 0.0011 S/rn.
For each sensor the difference
between the NRCC calibrations and the post-AIWEX intercomparison were
calculated.
The mean and standard deviation of these calibration differ-
ences based on 6 calibration points are given in Table 1.
The new temper-
ature sensors with serial numbers 6xx were very consistent with each other
and measured 0.009 to 0.013°C higher in post-calibration.
The earlier
model temperature sensors with serial numbers 4xx differed by -0.005 to
+0.004°C; sensor #424 failed upon recovery and could not be recalibrated.
The apparent systematic calibration differences between old and new sensors has not yet been explained.
8
Even though temperature sensor #615 moored at 508 m performed consistently in both pre- and post-AIWEX calibration, a very significant offset
in calibration was observed when the sensor was in situ.
reproduce this behavior in the laboratory have failed.
All attempts to
It does appear,
however, that the relative temperature fluctuations measured by the sensor
are reasonable.
Comparisons with the temperature at 508 m measured by the
APS throughout AIWEX indicate that the temperature offset was +0.11°C.
Therefore, this constant offset has been removed in all the data from
#615.
and Recovery
The moorings were deployed in and around the AIWEX ice camp located
about 350 km north of Prudhoe Bay, Alaska.
The position of the camp as a
function of time determined from satellite navigation is shown in Fig. 4.
Deployment of the central mooring began on 19 March CMT from inside a
hut.
A 200 lb. weight was first lowered through a 16-inch diameter hole
in the 2.5 in
thick
ice.
The wire and sensors were then attached to the
strength member with plastic cable ties.
The satellite moorings were
installed through an 8 inch diameter hole by first unspooling on the ice
the entire length of the preassembled strength member, wire, and sensors.
The top end of the mooring was attached to a snowmobile, and a 100 lb.
weight and the rest of the mooring was lowered by driving the snowmobile
toward the hole.
An oil drum lying on its side near the hole provided a
smooth surface over which the mooring could slide.
Recovery of the satellite moorings began on 26 April; the central
mooring was recovered on 29 April.
Since the satellite moorings were left
to freeze into the ice, recovery was made through a new hole that was
drilled within a few feet of the mooring line.
A hook on the end of an
L-shaped pole was used to snag the line, and the mooring was pulled up
with the aid of the snowmobile.
The hole for the central mooring was kept
free of ice by adding heat from the oil-burning hut heater with a heat
exchanger.
A small electric winch was used to retrieve this mooring.
AIWEX CAMP POSITION
74.254
MAR 27
z0 74.15-ci)
-o
74,05- -
13
MAR 25
-I-)
73.95APR 22
73.85
APR 3Q
73.75-——147
—146
Fig.
Position
—144
Longitude (°E)
—145
—143
of AIWEX ice camp as a function of time determined
from sateflite navigation.
The line width changes at midnight
each day.
—142
10
ANALYSIS
Calculating Salinity
Time series of salinity can be calculated from measurements of temperature and conductivity.
Unfortunately the response times of the sen-
sors are not the same; the temperature sensor has a 200 ms time constant
while the response of the conductivity sensor is controlled by the flushing rate of the water through a tube 0.2 m long and ranging from 4 to 7 mm
in diameter.
A simple model was developed to try to predict the tempera-
ture inside the conductivity cell, T1(t), that could then be used with the
conductivity measurement to calculate salinity.
Assume in time At the
heat that leaves the cell is given by C b Iw(t)I T1(t) At where C is the
heat capacity/volume, b is the cross-sectional area of the cell, and
Iw(t)I is the speed of the water flushing through the cell.
During this
same time the heat entering the cell is C b tw(t)I T0(t) At where T0 is
the temperature outside the cell measured by a nearby temperature probe.
Hence the change of total heat inside the cell is equal to the heat entering minus the heat leaving:
[T1(t-4-At)
-
T1(t)]
=b Iw(t)I [T(t)-T1(t)] At
where 2 is the length of the cell.
well-mixed and w(t)
Assuming that the water in the cell is
constant,
dT1(t)
+
dt
1
—
T1(t)
=
1
—
T(t)
(1)
r
r
where r = bw/2 is a flushing time.
The frequency response of T1 to a
fluctuating outside temperature of the form T
= exp [iwt] can be expres-
sed by
T(t)2
I
T(t)
with T1 lagging T
by a phase
=
1
(l+w2r2)
(2)
11
9 =
Atan
wr
(3)
Equation (1) is easily applied to T(t) (measured) using finite-difference
methods to calculate the temperature inside the cell, T1(t), once r is
determined.
To determine r, the T and C measurements from 257 m are used.
It is
anticipated from historical data that salinity is linearly related to
temperature over a small range around 257 m, and can be expressed by
S=A1T+A+e
(4)
where e is the error in S due to violation of this assumption.
The
empirical equation relating T and C to S is nearly linear over the small
range of T and C that is observed from the sensor at 257 m and can be
written
S=aT+fiC
where a
-1.11 ppt/°C and
(5)
13.51 ppt/(S m1).
Therefore a linear
relationship between T and C can be written from (4) and (5):
(A-a)
C=
A
T+
(6)
fi
We
therefore assume that C(t) is linearly related to the temperature
measured inside the cell, T1(t), and that the observed phase between C(t)
and T(t) is representative of the phase between T1(t) and T0(t)
(Fig. 5).
In order to interpret the phase in the context of (3) the coherence
must be 1, that is
must be small.
At high frequency the coherence is
lower indicating that e may be significant, and the interpretation of the
phase is more complicated.
At low frequency the phase can be reasonably
reproduced by (3) with r = 4 minutes (Fig. 5).
To confirm this, the T
12
1.00
1
I
_L
II
t
.—
_i_
i
I
I
I_I
I
0.75
ci)
0
ci)
0.50
ci)
0
0
0.25
0.00- —
10—1
I
U
10°
I
I
I
I
I
I I
101
102
101
102
cph
9
U)
(I)
U
—9
—180
10—1
100
cph
Fig. 5.
Coherence and phase between conductivity and temperature measured at
Phase between conductivity
257 m on the central mooring (solid line).
and
8 minutes is plotted with
2,
if,
and filtered temperature using T =
Phase
modeled
by
equation
(3)
with T = if minutes is
a dashed line.
shown by a dotted line.
13
time series was filtered using (1) for a range of values of r, and the
phase between C and the filtered T
value of r
estimated (Fig. 5).
As expected, the
4 minutes reduces the phase difference at low frequency.
The
phase difference at high frequency may be due to a breakdown in the linear
T-S assumption (4) and/or in the simple filtering model (1).
We believe
the latter effect is dominant, primarily due to the variability of r.
Therefore, calculated salinity is less reliable at higher frequency.
At the depths of the other four pairs of T-C sensors, a constant,
linear T-S relationship clearly does not exist, and this method cannot be
used to estimate r.
Hence the same value of r = 4 minutes was used to
estimate T1 at all depths.
There is some interest in knowing how well S can be inferred from T.
One method of determining this relationship is by linear regression analysis.
The data were first averaged over 15 minutes to minimize any error
in estimating r.
The best-fit values of A
from (4), the percent
and
of the S variance that can be explained from T, and the correlation coefficient between T and S are given below for each pair of T-C sensors:
Depth
% S variance
explained
Correlation
coefficient
A1±90% conf.lim.
(ppt/°C)
A ±90% conf.lim.
(m)
80
-1.1530 ± 0.0790
30.424 ± 0.104
19.0
-0.44
185
1.2030 ± 0.0630
35.000 ± 0.095
28.0
0.53
257
0.7310 ± 0.0070
34.659 ± 0.004
93.0
0.97
303
0.3084 ± 0.0143
34.554 ± 0.001
34.0
0.58
508
-0.0874 ± 0.0202
34.889 ± 0.010
2.0
-0.14
(ppt)
Spectral Analysis and Coherences
Spectra and coherences were calculated by combining separate estimates at high and low frequencies.
The high frequency spectrum was calcu-
lated from the one-minute averaged data by dividing the series into segments of 5.6 h length.
The low frequency spectrum was estimated from a
single time series of one-hour averages.
14
OBSERVATIONS
Tables of the daily mean, standard deviation and skewness for each
sensor are given on pages 15 to 27.
In order to see the entire time series at a glance, 15-minute averages are plotted for the entire experiment on pages 30 and 31.
Salinity,
calculated from temperature and conductivity, are plotted with temperature
on page 33.
The entire data set sampled at 1 minute intervals is presented on
pages 36 to 113.
116 to 154.
Plots of salinity and temperature are found on pages
Density was not plotted since it is usually indistinguishable
from salinity.
Average spectra of temperature and salinity are plotted on pages 156
to 173.
Selected coherence and phase between vertically and horizontally
separated sensors are presented on pages 186 to 195.
15
STATI S TI C S
Tables of the daily mean, standard deviation and skewness for each
sensor.
16
MAR 22
JD 81
MAR 23
JD 82
MAR 24
JD 83
MAR 25
JD 84
MAR 26
JD 85
MAR 27
JD 86
MAR 28
JD 87
01(249)
-0.8449 -0.8197 -0.8685 -0.8955 -0.9189 mean
0.0209 0.0286 0.0374 0.0267 0.0264 std.
-0.0654 -0.2932 0.5399 0.0866 -0.0063 skew
02(249)
-0.8827 -0.8963 -0.9231 -0.9195 mean
0.0327 0.0244 0.0255 std.
0.0369
0.0030 0.0827 -0.1065 -0.1082 skew
03(249)
-0.8285 -0.8388 -0.8992 -0.9240 -0.9262 mean
0.0180 0.0298 0.0336 0.0275 0.0221 std.
0.0253 0.3917 -0.0033 -0.3043 -0.1483 skew
11(249)
-0.8291 -0.8363 -0.8904 -0.9197 -0.9246 mean
0.0093 0.0294 0.0360 0.0277 0.0238 std.
0.4155 -0.2272 0.3206 -0.1685 0.0592 skew
12(249)
-0.8586 -0.9005 -0.9286 -0.9322 mean
0.0270 0.0346 0.0291 0.0243 std.
-0.2201 0.2058 -0.0967 0.0449 skew
13(253)
-0.8460 mean
0.0229 std.
-0.1418 skew
13(253)
248.9
248.5
0.0397 0.3851
-1.6009 -0.4242
m
249.2
0.3788
0.0573
249.8 mean
249.7
0.0449 0.0517 std.
1.0404 -1.3984 skew
C(242)
-1.0716 -1.0595 -1.0275 -1.0101 -1.0356 -1.0467 -1.0287 mean
0.0102 0.0191 0.0345 0.0467 0.0272 0.0266 0.0222 std.
0.6279 0.2739 0.1029 -0.1836 -0.0567 0.3372 0.0875 skew
C(262)
-0.6319 -0.6190 -0.5865 -0.5916 -0.6356 -0.6465 -0.6390 mean
0.0170 0.0182 0.0273 0.0429 0.0332 0.0267 0.0287 std.
-0.2629 -0.7939 -0.0069 -0.1244 -0.3661 0.0394 -0.1720 skew
o
C
C(508)
m
508.0
----
507.9
0.1419
-1.8810
507.3 mean
507.4
507.4
0.0584 0.0646 0.0623 std.
-0.2155 -0.1164 -0.0328 skew
17
MAR 22
JD 81
C(80)
C(80)
S/rn
MAR 23
JD 82
MAR 24
JD 83
MAR 25
JD 84
MAR 26
JD 85
MAR 27
JD 86
MAR 28
JD 87
-1.3330 -1.3314 -1.3298 -1.3307 -1.3309 -1.3089 -1.3077 mean
0.0035 0.0071 0.0063 0.0045 0.0080 0.0057 0.0060 std.
-0.6918 -0.4078 -0.7362 -0.4173 1.1796 -0.3921 -0.3838 skew
2.5766 2.5774 2.5712 2.5632 2.5674
0.0009 0.0011 0.0039 0.0031 0.0042
0.4098 -0.4432 -0.2191 -0.0868 -0.1360
2.5724 2.5730 mean
0.0019 0.0015 std.
0.0259 -0.0008 skew
C(185)
-1.5265 -1.5122 -1.5113 -1.5053 -1.5242 -1.5088 -1.4969 mean
0.0079 0.0055 0.0147
0.0165 std.
0.0205 0.0065 0.0138
0.0194 -1.9704 0.6063 0.0048 -0.5215 0.7372 0.7712 skew
C(185)
2.6512 2.6520
0.0008 0.0007
-0.0285 -0.2179
S/rn
2.6515
0.0015
0.4925
2.6507
0.0030
0.0778
2.6478
0.0013
0.0878
2.6493
0.0014
0.2976
2.6501 mean
0.0020 std.
0.6675 skew
C(257)
-0.7455 -0.7670 -0.7213 -0.6940 -0.7317 -0.7418 -0.7400 mean
0.0135 0.0121 0.0274 0.0398 0.0328 0.0272 0.0240 std.
0.1535 0.4817 0.3331 -0.0883 0.0020 0.0117 -0.0817 skew
C(257)
2.7868
0.0015
-0.3491
S/rn
C(303)
o
C
C(303)
S/rn
C(508)
o
C
C(508)
S/rn
2.7838
0.0017
0.3708
2.7891
2.7926 2.7880 2.7874 2.7874 mean
0.0034 0.0054 0.0044 0.0024 0.0026 std.
0.3622 -0.1790 -0.0258 -0.1127 -0.5384 skew
-0.1184 -0.1048 -0.0849 -0.0717 -0.0929 -0.1010 -0.0894 mean
0.0067 0.0124 0.0213 0.0288 0.0256 0.0167 0.0168 std.
-0.0759 0.5336 -0.7879 -0.1891 0.9214 -0.4549 -0.1339 skew
2.8727
2.8723 2.8737 2.8751
0.0013 0.0012 0.0022 0.0032
-0.7929 -0.0166 -0.6365 -0.1655
2.8729 2.8724 2.8742 mean
0.0028 0.0016 0.0016 std.
0.9753 -0.9066 -0.3509 skew
0.4791 0.4817
0.0042 0.0025
0.7725 -0.6452
0.4700 0.4807 0.4737
0.0057 0.0053 0.0063
0.2360 -0.8392 -0.0609
0.4711
0.0025
0.3914
2.9584
0.0010
0.0183
2.9563 2.9557
2.9555
0.0005 0.0005 0.0006
0.1850 -0.9713 -0.3973
2.9559
0.0007
2.9567
0.0004
2.5561
0.4704 mean
0.0023 std.
0.5482 skew
2.9566 mean
0.0007 std.
1.4606 -0.5632 skew
18
MAR 29
JD 88
MAR 30
JD 89
MAR 31
JD 90
APR 1
JD 91
APR 2
JD 92
APR 3
JD 93
APR 4
JD 94
01(249) -0.9157 -0.8974 -0.8873 -0.8809 -0.8876 -0.8800 -0.8942 mean
0.0235 0.0187 0.0175 0.0198 0.0143 0.0157 0.0166 std.
-0.2958 0.2894 0.0758
0.5767 0.3101 0.3847 -0.3748 skew
02(249) -0.9164 -0.8992 -0.8908 -0.8814 -0.8820 -0.8819 -0.8849 mean
0.0192 0.0199 0.0169 0.0134 0.0138 0.0136 0.0171 std.
0.0911 0.2489 -0.3050 0.1562 0.4235 0.4263 -0.3904 skew
03(249) -0.9143 -0.9036 -0.8986 -0.8884 -0.8895 -0.8915 -0.8898 mean
0.0203 0.0161 0.0152 0.0111 0.0138 0.0127 0.0162 std.
-0.5584 0.3261 0.2704 0.2225 0.3370 0.1753 -0.0029 skew
11(249) -0.9114 -0.8982 -0.8905 -0.8776 -0.8870 -0.8842 -0.8885 mean
0.0259 0.0186 0.0153 0.0123 0.0136 0.0120 0.0152 std.
-0.3238 0.2493 0.3345 0.4171 0.3500 0.2129 -0.0951 skew
12(249) -0.9210 -0.9075 -0.8972 -0.8859 -0.8952 -0.8903 -0.8963 mean
0.0228 0.0152 0.0152 0.0113 0.0140 0.0146 0.0150 std.
-0.2826 0.1370 0.0120 -0.6578 0.0401 0.4764 0.2555 skew
13(253) -0.8386 -0.8246 -0.8176 -0.8084 -0.8091 -0.8102 -0.8064 mean
0.0231 0.0152 0.0155 0.0142 0.0129 0.0116 0.0199 std.
-0.5591 -0.0209 -0.0801 0.0514 0.1761 0.2537 0.6552 skew
13(253)
m
249.8
249.8
249.9
0.0507 0.0468 0.0516
-0.1970 -0.5220 -0.1295
249.9
0.0362
0.0895
249.9
0.0469
0.5811
250.0 mean
249.9
0.0472 0.0514 std.
0.6944 -0.0261 skew
C(242)
-1.0264 -1.0123 -0.9966 -0.9940 -0.9937 -1.0104 -1.0108 mean
0.0168 0.0143 0.0160 0.0179 0.0110 0.0142 0.0135 std.
-0.3362 0.1137 0.1636 0.6682 -0.7238 0.1377 0.0507 skew
C(262)
-0.6393 -0.6267 -0.6218 -0.6125 -0.6058 -0.6091 -0.6105 mean
0.0235 0.0204 0.0208 0.0099 0.0133 0.0114 0.0157 std.
-0.1393 0.1530 0.3146 0.4343 0.0973 -0.1045 0.5005 skew
o
C
C(508)
m
507.3
0.0555
0.0194
507.4
0.0572
0.1383 -0.0907
507.3
0.0590
507.4
507.4
0.0620
0.0495
0.2233 -0.1088
507.4 mean
507.3
0.0823 0.0869 std.
0.1057 -0.0975 skew
19
MAR29 MAR30 MAR31 APR
JD 88
JD 89
JD 90
1
JD 91
APR 2
JD 92
APR 3
JD 93
APR 4
JD 94
C(80)
-1.3045 -1.3029 -1.2996 -1.2978 -1.2981 -1.3020 -1.3310 mean
0.0044 0.0028 0.0030 0.0009 0.0025 0.0081 0.0042 std.
-0.4473 -0.3931 -0.0851 -0.3169 0.3312 -2.7174 2.0363 skew
C(80)
2.5727
0.0013
-0.2967
S/rn
2.5724 2.5713 2.5722
2.5717 2.5706
0.0010 0.0009 0.0004 0.0009 0.0014
0.5435 -0.0457 -0.4906 -0.2046 -1.0873
2.5689 mean
0.0013 std.
0.0905 skew
C(185)
-1.4733 -1.4756 -1.4991 -1.4712 -1.4634 -1.4917 -1.5065 mean
0.0113 0.0114 0.0230 0.0049 0.0029 0.0154 0.0086 std.
-1.1552 -0.5587 0.1815 -0.5020 -1.1744 -0.0129 1.7300 skew
C(185)
2.6516
2.6524
0.0011 0.0014
-0.4091 -0.3958
S/rn
C(257)
C(257)
S/rn
C(303)
o
C
C(303)
S/rn
C(508)
o
C
C(508)
S/rn
2.6507
0.0017
0.4563
2.6530 2.6549 2.6513
0.0005 0.0010 0.0014
0.2483 -0.6844 -0.1694
2.6501 mean
0.0007 std.
0.5137 skew
-0.7431 -0.7270 -0.7200 -0.7235 -0.7012 -0.7051 -0.7121 mean
0.0219 0.0190 0.0157 0.0094 0.0137 0.0145 0.0155 std.
0.0637 -0.2185 0.1614 -0.1025 -0.2326 -0.2109 0.0131 skew
2.7871
0.0023
0.0981
2.7898
0.0019
0.0646
2.7906
0.0016
0.2550
2.7896 2.7928
2.7916
0.0008 0.0017 0.0018
0.0713 -0.1586 -0.3115
2.7906 mean
0.0017 std.
0.0210 skew
-0.0948 -0.0890 -0.0709 -0.0622 -0.0455 -0.0613 -0.0884 mean
0.0124 0.0109 0.0229 0.0093 0.0103 0.0181 0.0093 std.
0.3376 1.2073 -0.2821 -0.3445 -0.7645 -0.3054 0.1729 skew
2.8733
0.0011
-0.1492
2.8745 2.8765 2.8770 2.8787 2.8760 2.8735 mean
0.0010 0.0025 0.0007 0.0014 0.0018 0.0010 std.
1.1022 -0.2623 -0.5925 -0.5659 -0.1366 -0.2604 skew
0.4748 0.4803 0.4768
0.0048 0.0038 0.0075
0.7692 -2.1002 -0.4485
0.4701
0.0041
1.6730
0.4735
0.0069
0.7434
0.4729 0.4656 mean
0.0083 0.0027 std.
0.3766 -0.2075 skew
2.9571 2.9572
0.0006 0.0012
0.2341 -0.2205
2.9561
0.0003
0.6159
2.9563
0.0007
0.0906
2.9556
0.0008
2.9565
0.0007
0.3350
2.9550 mean
0.0003 std.
0.4654 -0.4682 skew
20
APR 5
JD 95
APR 6
JD 96
APR 7
JD 97
APR 8
JD 98
APR 9
JD 99
APR 10
JD 100
APR 11
JD 101
01(249) -0.8727 -0.8628 -0.8619 -0.8574 -0.8513 -0.8376 -0.8511 mean
0.0148 0.0143 0.0130 0.0178 0.0133 0.0111 0.0143 std.
-0.4854 -0.2254 0.1856 -0.2091 0.5332 0.6688 0.6733 skew
02(249) -0.8757 -0.8675 -0.8602 -0.8620 -0.8547 -0.8330 -0.8475 mean
0.0154 0.0155 0.0138 0.0117 0.0136 0.0134 0.0137 std.
0.0355 0.2444 0.0655 -0.2442 0.4154 0.4323 -0.1018 skew
03(249) -0.8755 -0.8704 -0.8649 -0.8685 -0.8623 -0.8383 -0.8500 mean
0.0145 0.0149 0.0116 0.0108 0.0109 0.0105 0.0147 std.
-0.0945 0.1156 -0.3683 -0.2573 -0.2485 -0.3748 -0.1100 skew
11(249) -0.8717 -0.8628 -0.8620 -0.8610 -0.8559 -0.8347 -0.8469 mean
0.0145 0.0171 0.0109 0.0123 0.0146 0.0116 0.0139 std.
-0.0857 -0.0225 -0.2650 -0.0688
0.5417 -0.1741 0.1629 skew
12(249) -0.8795 -0.8723 -0.8685 -0.8709 -0.8627 -0.8400 -0.8554 mean
0.0137 0.0177 0.0136 0.0123 0.0116 0.0131 0.0140 std.
0.1333 0.1577 -0.0770 -0.0358 0.7039 -0.2919 0.0879 skew
13(253) -0.7950 -0.7812 -0.7776 -0.7889 -0.7769 -0.7579 -0.7718 mean
0.0135 0.0161 0.0115 0.0097 0.0141 0.0126 0.0167 std.
0.1093 -0.0391 0.2063 0.1675 -0.3081 -0.6568 0.2267 skew
13(253)
m
C(242)
o
C
C(262)
o
C
C(508)
m
250.0
250.1
0.0554 0.0504
0.1245 -0.3828
250.1
0.0368
0.9230
250.1
0.0372
0.0080
249.9 mean
250.1
250.1
0.0410 0.0537 0.0698 std.
1.0357 -0.4715 -0.2377 skew
-1.0024 -0.9964 -0.9898 -0.9859 -0.9735 -0.9797 -0.9753 mean
0.0148 0.0106 0.0126 0.0116 0.0115 0.0108 0.0164 std.
-0.6668 -0.1173 0.2582 0.0961 0.1577 0.1284 0.3304 skew
-0.5930 -0.5919 -0.5779 -0.6039 -0.5732 -0.5639 -0.5746 mean
0.0176 0.0152 0.0128 0.0123 0.0137 0.0158 0.0189 std.
-0.1706 -0.4065 0.4342 0.5555 0.2200 -0.1362 -0.0858 skew
507.5
0.0878
-0.6509
507.6
0.0613
0.0640
507.6
0.0595
0.1040
507.6
0.0610
0.1512
507.3 mean
0.1329 std.
0.1717 -1.7320 -1.1606 skew
507.6
0.0557
507.6
0.0873
21
APR 5
JD 95
APR 6
JD 96
APR 7
JD 97
APR 8
JD 98
APR 9
JD 99
APR 10
JD 100
APR 11
JD 101
C(80)
-1.3059 -1.3208 -1.3346 -1.3006 -1.2989 -1.3070 -1.3288 mean
0.0066 0.0117 0.0096 0.0033 0.0032 0.0151 0.0032 std.
-1.5671 0.4889 -0.0293 -1.9827
0.3120 -0.4399 1.0880 skew
C(80)
2.5722
0.0010
-0.2835
S/rn
C(185)
C(185)
S/rn
2.5709 2.5684 2.5710 2.5704 2.5685
0.0018 0.0012
0.0008 0.0007 0.0018
0.6421 -0.8470 -0.1906 -0.0278 -0.3873
2.5675 mean
0.0012 std.
1.2683 skew
-1.4800 -1.4812 -1.4831 -1.4645 -1.4662 -1.4948 -1.5171 mean
0.0123 0.0097 0.0135 0.0038 0.0112 0.0150 0.0055 std.
-0.4131 0.5247 -0.4667 0.3142 -2.0428 0.0692 0.1419 skew
2.6533
0.0013
0.2095
2.6530 2.6531
0.0008
0.0012
0.2789 -0.2438
2.6549 2.6549
0.0010 0.0012
1.1512 -0.6521
2.6525
0.0016
0.0715
2.6505 mean
0.0008 std.
0.1599 skew
C(257)
-0.6983 -0.6865 -0.6788 -0.6931 -0.6797 -0.6575 -0.6712 mean
0.0144 0.0136 0.0131 0.0131 0.0134 0.0133 0.0155 stcl.
0.2423 -0.6606 0.0222 -0.1465 0.3480 -0.3064 0.1349 skew
C(257)
S/m
2.7920 2.7941
0.0016 0.0013
-0.3049 -0.6174
C(303)
-0.0980 -0.0946 -0.0907 -0.0756 -0.0825 -0.0783 -0.0660 mean
0.0068
0.0062 0.0073 0.0099 0.0075 0.0078 0.0139 std.
0.1426 -0.3666 0.2300 0.3282 0.2315 0.1593 0.0255 skew
2.7955
0.0013
0.2926
2.7940 2.7949 2.7967
0.0016
0.0013 0.0017
0.0939 -0.0890 -0.1697
2.7960 mean
0.0020 std.
0.0671 skew
C(303)
S/m
2.8730
0.0011
0.4411
2.8738
0.0008
0.0068
2.8746
0.0011
0.0843
2.8754 2.8750
0.0013 0.0010
0.3759 -0.2078
2.8751
0.0007
0.1809
2.8760 mean
0.0015 std.
0.0480 skew
C(508)
0.4670
0.0014
-0.7507
0.4668
0.0018
0.8163
0.4650
0.0009
1.2277
0.4644 0.4716
0.0017 0.0029
0.1016 -0.7062
0.4658
0.0024
1.5319
0.4764 mean
0.0143 std.
0.4979 skew
2.9561
0.0011
0.9821
2.9567
0.0007
0.2465
2.9564
0.0008
0.0012
2.9555
0.0006
0.8975
2.9568
0.0012
0.3285
2.9552
0.0002
1.0448
2.9561 mean
0.0013 std.
0.4894 skew
o
C
C(508)
S/rn
22
APR 12
JD 102
APR 13
3D 103
APR 14
JD 104
APR 15
3D 105
APR 16
3D 106
APR 17
3D 107
APR 18
3D 108
01(249) -0.8129 -0.8092 -0.8070 -0.8096 -0.8010 -0.7896 -0.7787 mean
0.0201 0.0165 0.0155 0.0142 0.0152 0.0163 0.0213 std.
0.1717 -0.2528 -0.0411 -0.1490 -0.0797 -0.1704 0.3040 skew
02(249) -0.8077 -0.8077 -0.8076 -0.8057 -0.7962 -0.7850 -0.7833 mean
0.0176 0.0152 0.0142 0.0142 0.0173 0.0173 0.0238 std.
-0.2222 0.1716 0.0693 -0.0942 0.2151 0.0715 0.2267 skew
03(249) -0.8148 -0.8085 -0.8171 -0.8158 -0.8085 -0.7846 -0.7854 mean
0.0162 0.0153 0.0150 0.0150 0.0167 0.0176 0.0242 std.
0.0372 0.1406 0.7175 -0.1181 0.7626 -0.0584 0.1148 skew
11(249) -0.8100 -0.8045 -0.8027 -0.8109 -0.8008 -0.7799 -0.7797 mean
0.0175 0.0166 0.0144 0.0145 0.0170 0.0172 0.0217 std.
0.1711 0.1176 0.0076 0.2568 0.0206 -0.1459 -0.1009 skew
12(249) -0.8160 -0.8162 -0.8098 -0.8143 -0.8070 -0.7931 -0.7860 mean
0.0183 0.0139 0.0155 0.0144 0.0165 0.0195 0.0210 std.
-0.1025 -0.1839 -0.0979 0.0815 0.3909 0.2482 0.1042 skew
13(253) -0.7353 -0.7283 -0.7293 -0.7307 -0.7230 -0.7055 -0.7102 mean
0.0184 0.0151 0.0127 0.0150 0.0147 0.0205 0.0207 std.
0.1854 0.1633 0.1265 -0.1343 0.2184 -0.2643 -0.0501 skew
13(253)
m
C(242)
o
C
C(262)
o
C
250.0
0.0633
-0.5292
250.1
0.0386
1.0775
250.1
0.0464
0.7641
249.8
249.7 mean
250.1
250.0
0.0534 0.1418 0.2166 0.2370 std.
0.3521 -1.3896 -1.6728 -0.9433 skew
-0.9542 -0.9432 -0.9411 -0.9595 -0.9501 -0.9262 -0.9163 mean
0.0181 0.0192 0.0160 0.0153 0.0163 0.0212 0.0226 std.
0.2475 -0.6595 -0.6159 -0.3500 0.3150 -0.6698 -0.0514 skew
-0.5265 -0.5287 -0.4906 -0.5019 -0.5086 -0.5385 -0.5338 mean
0.0225 0.0173 0.0204 0.0174 0.0141 0.0160 0.0260 std.
0.2232 0.1807 -0.2394 -0.6464 0.4951 0.0276 0.2224 skew
C(508)
507.5
m
0.0910
-1.1281
506.7 mean
506.7
507.3
507.6
507.6
507.6
0.0555 0.0583 0.0828 0.3804 0.6239 0.7877 std.
0.2198 -0.0823 -0.2570 -1.3859 -1.4915 -0.9415 skew
23
APR 12
JD 102
APR 13
JD 103
APR 14
JD 104
APR 15
JD 105
APR 16
JD 106
APR 17
JD 107
APR 18
JD 108
C(80)
-1.3234 -1.3283 -1.3299 -1.3233 -1.3235 -1.3211 -1.3223 mean
0.0034 0.0049 0.0041 0.0042 0.0051 0.0046 0.0067 std.
-0.3505 0.0167 1.2406 -0.5481 0.3348
2.0660 0.4975 skew
C(80)
2.5706 2.5710 2.5709 2.5703 2.5681
0.0012
0.0010 0.0007 0.0012 0.0012
-0.8748 -0.1414 -0.1733 -0.3448 -0.5133
S/rn
C(185)
C(185)
S/rn
2.5691 2.5708 mean
0.0022
0.0020 std.
0.4790 -0.2177 skew
-1.5131 -1.5153 -1.5149 -1.5146 -1.5042 -1.4809 -1.5242 mean
0.0031 0.0028 0.0024 0.0036 0.0063 0.0146 0.0092 std.
0.7965
0.5415 0.2100 1.2117 1.3081 -0.8231 -0.3233 skew
2.6523
0.0007
0.6017
2.6525 2.6525
0.0006 0.0006
0.3154 -0.3775
2.6536
0.0008
2.6552
2.6510 mean
0.0015 0.0013 std.
0.3296 -0.0993 -0.3904 -0.2519 skew
2.6528
0.0009
C(257)
-0.6336 -0.6238 -0.6180 -0.6197 -0.6129 -0.6208 -0.6214 mean
0.0182 0.0170 0.0164 0.0173 0.0160 0.0189 0.0256 std.
-0.5808 -0.3370 0.0969 -0.1093 -0.0885 0.1039 0.6454 skew
C(257)
S/m
2.8019
2.8031
0.0022 0.0021
-1.1234 -0.5718
C(303)
-0.0640 -0.0734 -0.0737 -0.0401 -0.0421 -0.0601 -0.0644 mean
0.0177 0.0066 0.0081 0.0203 0.0147 0.0123 0.0149 std.
0.5353 -0.1876 -0.5904 -1.2286 -1.3125 0.1552 -0.5173 skew
C(303)
S/rn
C(508)
o
C
C(508)
S/rn
2.8770 2.8767
0.0017 0.0010
0.5001 -0.1305
2.8029
0.0018
2.8034
0.0024
0.1323 -0.1861 -0.3904 -0.2940
2.8025
0.0019
2.8032
0.0019
2.8765 2.8793
2.8789
0.0009 0.0021 0.0014
0.1551 -1.2942 -1.1301
2.8030 mean
0.0034 std.
0.5905 skew
2.8777 2.8770 mean
0.0014 0.0018 std.
0.2733 -0.5875 skew
0.5004 0.5006 0.4992
0.0016
0.0013 0.0014
-1.1055 -0.6888 -0.1332
0.4994 0.4998
0.0010 0.0012
0.5490 -1.1989
0.4974 0.5002 mean
0.0021 0.0020 std.
0.4780 -0.1849 skew
2.9587
0.0004
-0.0741
2.9585 2.9583
0.0003 0.0002
1.5914 -1.7735
2.9581 mean
2.9579
0.0002 0.0002 std.
1.0450 -0.4624 skew
2.9591
0.0008
0.7535
2.9586
0.0004
1.1964
24
APR 19
JD 109
APR 20
JD 110
APR 21
JD 111
APR 22
JD 112
APR 23
JD 113
APR 24
JD 114
APR 25
JD 115
01(249) -0.8035 -0.8078 -0.7780 -0.7747 -0.8276 -0.8384 -0.5294 mean
0.0209 0.0157 0.0184 0.0158 0.0236 0.0487 0.0773 std.
0.1172 -0.8505 -0.0676 -0.0962 0.2433 1.5335 -0.4861 skew
02(249) -0.8082 -0.8095 -0.7736 -0.7725 -0.8245 -0.8216 -0.5521 mean
0.0215 0.0211 0.0205 0.0226 0.0269 0.0470 0.0673 std.
0.0580 -0.2675 -0.1072 -0.0241 -0.1003 1.3875 -0.4092 skew
03(249) -0.7941 -0.7984 -0.7759 -0.7694 -0.8202 -0.8325 -0.5733 mean
0.0196 0.0203 0.0183 0.0185 0.0263 0.0298 0.0809 std.
-0.2053 -0.1871 0.1677 -0.2012 0.3581 0.9666 -0.4069 skew
11(249) -0.7940 -0.8006 -0.7732 -0.7649 -0.8228 -0.8354 -0.5404 mean
0.0196 0.0211 0.0202 0.0153 0.0236 0.0453 0.0746 std.
-0.0228 -0.6161 -0.0454 0.5971 0.2515 1.1281 -0.6026 skew
12(249) -0.8046 -0.8145 -0.7816 -0.7787 -0.8290 -0.8388 -0.5509 mean
0.0217 0.0197 0.0210 0.0162 0.0239 0.0444 0.0708 std.
-0.2354 -0.1567 0.1673 0.2150 0.1549 1.3994 -0.5287 skew
13(253) -0.7228 -0.7255 -0.7018 -0.6937 -0.7328 -0.7402 -0.4900 mean
0.0193 0.0183 0.0190 0.0119 0.0215 0.0450 0.0703 st&
0.0111 0.2822 -0.2668 0.0810 0.0473 1.0551 -0.5286 skew
13(253)
m
C(242)
o
C
C(262)
o
C
C(508)
m
250.0
250.1
250.0
249.5 mean
250.1
250.2
250.0
0.2526 0.0568 0.0591 0.0464 0.1737 0.1135 0.6604 std.
-1.5942 -0.1142 -0.0560 -0.4111 -0.9724 -0.8585 -1.6829 skew
-0.9248 -0.9553 -0.8904 -0.9359 -0.9534 -0.9632 -0.6357 mean
0.0179 0.0249 0.0308 0.0232 0.0254 0.0450 0.0895 std.
0.2572 0.3065 -1.0103 0.4980 0.2610 0.9698 -0.6329 skew
-0.5390 -0.5492 -0.5226 -0.5224 -0.5571 -0.5607 -0.3452 mean
0.0179 0.0176 0.0175 0.0110 0.0179 0.0426 0.0508 std.
-0.1473 0.1175 -0.0442 -0.3046 -0.1284 1.2241 -0.3145 skew
507.1 mean
507.4
507.3
507.6
507.7
507.4
507.6
0.7340
std.
0.2445
0.4487
0.0528
0.1145
0.1274
0.5302
-1.7871 -1.9813 -1.9102 -0.2232 -1.2399 -1.8395 -2.4892 skew
25
APR 19
JD 109
APR 20
JD 110
APR 21
JD 111
APR 22
JD 112
APR 23
JD 113
APR 24
JD 114
APR 25
JD 115
C(80)
-1.3485 -1.3951 -1.3420 -1.3836 -1.3661 -1.3530 -1.3653 mean
0.0496 0.0623 0.0185 0.0472 0.0230 0.0125 0.0225 std.
-3.5235 -0.9822 -4.0670 -2.0986 -1.5101 -0.7131 0.1459 skew
C(80)
S/m
2.5741 2.5723 2.5771 2.5759 2.5791 2.5825
0.0041 0.0054 0.0021 0.0037 0.0026 0.0017
-2.3090 -1.0449 -1.9783 -1.7958 -1.6524 -0.6577
C(185)
-1.5187 -1.5151 -1.5104 -1.5112 -1.5086 -1.5064 -1.3857 mean
0.0154 0.0109 0.0097 0.0106 0.0116 0.0131 0.0673 std.
0.0998 0.6232 1.3114 0.9415 -1.9244 -0.7981 0.0482 skew
C(185)
S/nt
C(257)
C(257)
S/rn
2.6517
2.6532 2.6548
0.0014 0.0013
0.1392 -0.0806 -0.1780
0.0018
2.5663 mean
0.0109 std.
0.0490 skew
2.6560
2.6590 2.6851 mean
0.0014 0.0019 0.0129 std.
0.3527 -2.0959 -0.0731 -0.0330 skew
2.6555
0.0013
-0.6284 -0.6333 -0.6055 -0.6069 -0.6408 -0.6491 -0.4138 mean
0.0189 0.0149 0.0168 0.0115 0.0199 0.0465 0.0647 std.
0.1618 -0.1887 -0.5039 0.0340 -0.4764 1.0707 -0.5156 skew
2.8023
0.0024
0.1092
2.8019 2.8065
0.0017 0.0019
0.0283 -0.3928
2.8064 2.8009
0.0014 0.0028
0.2503 -0.4424
2.8002 2.8324 mean
0.0062 0.0087 std.
1.1084 -0.5569 skew
C(303)
-0.0800 -0.0826 -0.0893 -0.1144 -0.1065 -0.0784 0.0366 mean
0.0137 0.0109 0.0096 0.0217 0.0204 0.0310 0.0325 std.
-0.0324 0.3981 0.9280 0.1089 0.0038 -0.2825 -0.6188 skew
C(303)
2.8755
0.0016
-0.0615
2.8753
2.8760
0.0012 0.0010
0.2514 -0.6405
2.8735 2.8732 2.8759
2.8894 mean
0.0020 0.0019 0.0033 0.0037 std.
0.2562 -0.0812 -0.2040 -0.6619 skew
C(508)
0.5023
0.0007
-6.6563
0.5031 0.5060
0.0021 0.0017
1.1165 -1.5671
0.5076
0.0010
0.6826
0.5024 0.5048
0.0028 0.0026
0.1184 -0.3336
C(508)
2.9585
0.0003
0.9329
2.9585
0.0002
0.4958
2.9596
0.0006
0.0448
2.9582 2.9584 2.9589 mean
0.0003 0.0003 0.0003 std.
0.4100 -0.4400 -0.5408 skew
S/rn
S/rn
2.9596
0.0011
0.4536
0.5068 mean
0.0018 std.
1.0282 skew
26
APR 26
JD 116
APR 27
JD 117
APR 28
JD 118
APR 29
JD 119
APR 30
JD 120
01(249) -0.5966
0.0415
0.3088
mean
02(249) -0.6116
0.0251
-0.4568
mean
03(249) -0.6117 -0.6651 -0.6983 -0.7378
0.0347 0.0231 0.0211 0.0184
-0.3947 0.1714 0.2237 -0.4893
mean
11(249) -0.6003 -0.6593
0.0355 0.0164
0.0704 0.8854
mean
12(249) -0.6209 -0.6825 -0.7158
0.0325 0.0189 0.0193
0.0172 0.0765 -0.0150
mean
13(253) -0.5360 -0.5987 -0.6306 -0.6546
0.0356
0.0198 0.0199 0.0070
0.0003 -0.0742 0.1462 1.1103
mean
13(253)
250.1
0.0498
0.4452
mean
-0.7343 -0.7916 -0.8313 -0.8829
0.0359 0.0265 0.0252 0.0148
0.3151 -0.7195 0.2328 0.2294
mean
-0.3954 -0.4644 -0.4918 -0.4951
0.0319 0.0177 0.0156 0.0119
-0.8707 0.0727
0.1662 -0.3749
mean
506.4
507.2
0.9655 0.6378
-1.5632 -0.7315
mean
m
C(242)
o
C
C(262)
o
C
C(508)
m
std.
skew
std.
skew
std.
skew
std.
skew
249.4
250.0
250.2
0.8185 0.2085 0.0447
-1.8088 -0.5538 -0.7491
std.
skew
507.7
507.7
0.0586 0.0601
0.0483 -0.0362
std.
skew
std.
skew
std.
skew
std.
skew
std.
skew
27
APR 26
JD 116
C(80)
C(80)
S/m
C(185)
C(185)
S/m
C(257)
C(257)
S/rn
C(303)
o
C
C(303)
S/rn
C(508)
o
C
C(508)
S/rn
APR 27
JD 117
APR 28
JD 118
APR 29
JD 119
APR 30
JD 120
-1.3493 -1.3409 -1.3410 -1.3479
0.0166 0.0112 0.0026 0.0081
-0.1385 -2.7417 -0.6283 -1.7161
mean
2.5754 2.5779
0.0054 0.0021
-1.7354 -0.6345
2.5799
2.5813
0.0009 0.0006
0.1221 -0.4422
mean
-1.4675 -1.5095 -1.5205 -1.5228
0.0413 0.0150 0.0082 0.0028
1.0047 -0.3389 0.4990 0.5288
mean
2.6680
0.0094
0.7924
2.6570
0.0019
0.0783
std.
skew
std.
skew
std.
skew
2.6559 2.6554
0.0010 0.0005
0.7157 -0.6130
mean
-0.4661 -0.5302 -0.5521 -0.5781
0.0338 0.0152 0.0161 0.0176
-0.4689 -0.1231 0.2729 -0.2243
mean
2.8252
2.8173
0.0044 0.0022
-0.4608 -0.2268
2.8143 2.8100
0.0023 0.0022
0.2727 -0.2458
mean
-0.0011 -0.0432 -0.0997 -0.0949
0.0304 0.0256 0.0202 0.0133
-0.0017 -0.1675 -0.1117 0.6342
mean
2.8851
0.0033
-0.0723
2.8755
0.0011
0.7612
mean
0.5040 0.5054
0.0028 0.0025
0.5574 -0.2750
0.5020 0.5026
0.0014 0.0010
0.0109 -4.5794
mean
2.9585 2.9586
0.0002 0.0002
0.1994 -0.0412
2.9586
0.0004
2.7553
mean
2.8808 2.8755
0.0026 0.0019
0.0401 -0.0087
2.9589
0.0003
0.7445
std.
skew
std.
skew
std.
skew
std.
skew
std.
skew
std.
skew
std.
skew
29
TIME SERIES OF TEMPERATURE, CONDUCTIVITY, AND PRESSURE
On the following two pages are plots of 15-minute averages of
temperature, conductivity, and pressure of the entire experiment.
The
sensors are plotted with the same resolution except for the temperature
and conductivity at 508 ni.
30
'It'
I
I
I
I
I
I
I
I
F
I
I
F
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
00
250.
-4
rn
Lc)
V)
11
248.
fl
I
'-m—0.80
I
I
I
00
1
V"(
1.00
-4
(-)
-4
—1 .20F
I
I
I
I
-4
i
I
I
I
±-+--1---+ +
I
506.
m
504.
22 24 26 28 30
MAR
85
1
3
5
7
9
11
13 15 17
APR 85
19 21 23 25 27 29
CMT
31
C)
0
C)
co
0
C)
-S
co
01
C)
NJ
01
C)
N)
01
C)
0
C)
0
C)
01
0
+
I
I
I
I
I
I
I
S/rn
C)
2.96
22 24 26 28 30
85
1
3
5
7
9 11
13 15 17 19 21 23 25 27 29
AFR 85
CMI
2.95
32
TIME SERIES OF TEMPERATURE AND SALINITY
The plots on the adjacent page are 15-minute averages of
temperature and salinity measured by the 5 temperature-conductivity
sensor pairs on the central mooring.
Before salinity was calculated
temperature was filtered by equation (1) with time constant
r
= 4 minutes to try to match the time constant of the conductivity
sensors.
The sensors are plotted with the same resolution except for
the temperature and conductivity at 508 m.
33
1
I
I
I
I
—1.10 100
0
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
0
—1.50
0
0
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
03
0
0
I
0
0
I
I
I
I
I
I
I
11111
Fl II
I
I
I
0
liii
:°c
I
I
I
I
IF
1111
I
111111
I
I
I
:
•IIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIII
0
•%
0
0
34.70
.
''Il''III I
.
1111111111 11111111111 I
11111111
II
22 24 26 28 30 '1 '3 5 7 9 11 13 15 17 19 21 23 25 27 29
I
MAR 85
I
APR 85
I
I
I
I
I
I
I
I
GMT
I
34
35
TIME SERIES OF TEMPERATURE, CONDUCTIVITY, AND PRESSURE
The one-minute averages of temperature, conductivity, and pressure
are plotted at one day per page.
The series are plotted with the same
resolution of temperature, conductivity and depth.
36
0112
c\J
—0.60
00
(0
0068
—.
03
508.
0
506.
1
0
.1,1,1,1,1 TI 111111
2
4
6'
8'
10
Iii iii
12
22 MAR 85
JD(081)
14
I
I
16
,(,1,I,It •
18
20
GMT
22
37
I
I
I
I
'
I
'
I
I——'———f———'
I
I
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'
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—1.30
oc
—1.34
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j
j
1
t
j
I
j
I
I—
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j
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•138
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j
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j
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S/rn
2.59
:
-
1
I
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f
i
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I
2.58
2.57'
-—1.48
I
-1.52
-—1.56
i
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S/rn
-
2.66 o
2.65
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—
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3
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3—
f
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3
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2.64
---0.70
F-—l-——F-—-l--——I———I————f———i-——l-——+--—
00
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2.80 n
279
2.7'8
—0.08
oc
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I.
I
I
I
I
I
I
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I
I
-
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S/rn
0
2
4
12
22 MAR 85
14
16
18
20
GMT
22
2.86
o
38
I
I
I
t
t
I
i
i
I
I
}
I-
i
I
I
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1
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•
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f
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C
° 506.
-
m
F
0
I
I
2
F'
I
4
F
6
I
I
8
i-I-
10
I
F
I
I
F' f
12
23 MAR 85
JD(082)
I
14
I
I
I
'
16
F
'
F
I
18
I
I
20
GMT
I
22
39
—1.30
—1.34
00
—1
'-F
S/m
.38
2.59
2.58
CD
2.57
00
—1.56
2.66
-S
265 °'
c-ri
S/m
•
2.64
—0.72
N)
('I
I
I
I
'
r '
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Ui
H —0.80
r
I
I
I
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I
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I
I
2.79
C)
N)
278 (il
S/m
2.77
—0.14
2.88
c-)
(14
S/rn
L
I—
'
I
i—f— '—
I
I
I
'
I
'
I
I
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(14
-
2.86
I
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0.44
S/rn
-
I
2.97
(ji
96 °
H
0
2
4
6
8
10
12
23 MAR 85
JD(082)
14
16
18
20
G MT
22
GO
2.95
__
40
t
6—0.88
0)
Pt)
0—0.86
N0.82
—0.86
251.
to
N
250.
249.
N
0106
N
(0
0062
0
2
4
6
8
10
12
24 MAR 85
JD(083)
14
16
18
20
G MT
22
'41
1.28
1.32
C-)
0
1.36
2.58
2.57
2.56
1.48
1.52
C)
co
01
1.56
2.66 0
265co
(31
C)
N)
01
2.80 0
N)
2.79
(31
C)
0.08
0.12
(J4
0
c-i.'
2.88
287°
c-i.'
('4
2.86
0.52
0.48
C)
(31
0
0.44
2.97
01
296°
0
2
4
2.95
6
8
24 MAR 85
JD(083)
GMT
42
_0.88
N —0.86
251.
250.
249.
N
0_i 06
25 MAR 85
JD(084)
GMT
i43
1.30
1.34
1.38
2.57
2.56 o
4
LZJU
1.54
2.66
'x
01
c-)
265w01
2.64
0.74
C-)
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01
C)
0
(JJ
2.89
c•)
288°
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2.87
0.52
U. AC
t•0
0.44
C_Ti
cx
2.97 C)
6°
01
0
2
4
6
8
10
12
25 MAR 85
JD(084)
14
16
18
20
CMI
22
2.95
44
5—0.90
0)
o —0.94
251.
U,
('4
('4-.
0108
Co
0068
508.
0
506.
0
2
4
6
8
10
12
26 MAR 85
JD(085)
14
16
18
20
CMT
22
1.30
2.58
2.57 0
2.56
1.56
:::
2.64
2.80
2.79
.78
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C)
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01
C-)
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0
(J4
2.88
(-'4
g-7 0
L.. • ¼.)
2.86
0.44
2.97
01
0
4
6
8
10
12
26 MAR 85
JD(085)
14
16
18
20
GMT
22
2.95
46
0)
6 —0.94
0)
C"
0—0.96
—0.96
251.
250.
249.
C"J
C"'-.
0108
(0
C"'—.
0068
508.
507.
506.
0
2
4
6
8
10
12
27 MAR 85
JD(086)
14
16
18
20
GMT
22
147
1.26
1:30w
2.58
2.57 o
2.56
1.54
2.66
a
UI
2.64
§
0.78
2.80
279
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2.78
§
0.14
2.88
2870('4
2.86
§
0.44
2.97 o
UI
cx'
0
2
4
2.95
6
8
10
12
27 MAR 85
JD(086)
14
16
18
20
GMT
22
k8
0)
0—0.96
0)
0 —0.96
0)
0 —0.96
250.
249.
C'4
0106
c\J
(0
0068
508.
507.
0
2
4
6
8
10
12
28 MAR 85
JD(087)
14
16
18
20
GMT
22
1.26
1.30
1.34
2.58 0
2.57 0
2.56
1.46
C)
1.50
cx
1.54
01
2.66
C-)
2.65
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fl5
TIME SERIES OF TEMPERATURE AND SALINITY
The one-minute averages of salinity and filtered temperature are
plotted at one day per page.
(1) with time constant r
The temperature was filtered by equation
4 minutes to try to match the time constant
of the conductivity sensors.
The series are plotted with the same
resolution of temperature, conductivity and depth.
116
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4.84
1
0
i
I
I
I
2
4
I
I
I
6
I
I
I
I
8
I
I
I
10
I
I
I
I
12
8 APR 85
JD(098)
I
I
14
16
I
I
18
i
I
I
I
20
22
CMI
t
134
0134
31.94
31.86
to
03
0150
233.20
03
0
33.12
N
to
0072
0
0012
03
34.48
0.52
0
it)
0.44
03
03482
0
2
4
6
8
10
12
9 APR 85
JD(099)
14
16.
18
20
GMT
22
135
31.92
0
0
.88
31.84
LU
CO
0
33.12
—0.62
N
LU
c\J-
°—0.70
N-
03412
C
°—0.12
03448
0.50
0.46
0.42
03
0
34.80
0
2
4
6
8
10
12
10 APR 85
JD(1 00)
14
16
18
20
C MT
22
136
0
0136
1.92
31.84
it)
03
0156
233.20
cc
0
33.12
N
LU
°—0.72
N
03412
N)
0
N)
03448
03
0
LU
0.52
0.48
0 0.44
34.88
cc
0
34.80
0
2
4
6
8
10
12
11APR85
JD(101)
14
16
18
20
CMT
22
137
C
,_..31.96
31.88
00
°—1.56
03
0
33.14
N
LI)
0068
N
0
0
0
34.48
0.54
0 0.50
0 0.46
0
0
0
2
4
6
8
10
12
12 APR 85
JD(1 02)
14
16
18
20
GMT
22
138
0
0
—1.36
31.98
0
0
31.90
if)
0156
0
34.16
0.54
0
0.46
0
0
34.80
0
2
4
6
8
10
12
13 APR 85
JD(1 03)
14
16
18
20
22
CMI
0
31.98
31.90
LU
03
0156
03
0
33.14
N
LU
('4—0.66
LI)
('4
0
34.14
0
0
0
0
2
4
6
8
10
12
14 APR 85
JD(1 04)
14
16
18
20
CMT
22
1140
0
5,—1.32
0136
31.96
31.88
10
4:0
0156
0
33.16
N
10
0066
p34.22
11)
N
0
§.34.54
34.50
0.54
0
It) 0.50
0 0.46
34.80
15 APR 85
JD(1 05)
CMT
0
0135
31.84
LU
03
0_154
it)
03316
N
('4-.
LU
—0.66
LI)
('4
0
34.14
0.00
0
°—0.08
p34.56
0
0
34.48
0.54
0
LI)
0.46
03
0
2
4
6
8
10
12
16 APR 85
JD(1 06)
14
16
18
20
CMT
22
0
31.94
0
0
0
LU
0
0
4
6
8
12
17 APR 85
JD(1 07)
14
16
18
20
22
CMI
C
0136
.96
31.88
U)
03
U)
0
0
0
0
0
0
2
4
6
8
10
12
18 APR 85
JD(1 08)
14
16
18
20
GMT
22
0
0138
32.04
31.96
tO
03
0156
03
0
66
N
0
0
0
0
0
0
2
4
6
8
10
12
19 APR 85
JD(1 09)
14
16
18
20
CMI
22
0
N
33.16
—0.60
c"J-.
0068
N
0
0
0
0
0
2
4
6
8
10
12
20 APR 85
JD(1 10)
14
16
18
20
22
CMT
146
0
0
0
32.00
LU
0156
LU
N
('4-.
LU
°—O.64
p34.26
LU
('4
0
34.18
N)
0
°—0.12
0N)
0
34.50
0.54
0
0.50
LU
0 0.46
0LU
0
34.80
0
2
4
6
8
10
12
21 APR 85
JD(111)
14
16
18
20
CMI
22
11+7
C
5.—1.38
0142
32.10
32.02
to
0156
0
0
0
0
0
0
34.80
0
2
4
6
8
10
12
22 APR 85
JD(112)
14
16
18
20
GMT
22
9f11
0
(3,
C),
C-)
i7VO0
0
9ct7c
v,r_ • r. 7
C)
98
£Z
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32,16
0
0
32.08
LC)
03
°—1.54
LO
03324
LI)
°068
p34.22
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0
34.14
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C
°012
4.56
C
N)
0
0.54
0.50
0.46
34.88
34.80
0
2
4
6
8
10
12
24 APR 85
JD(1 14)
14
16
18
20
C MT
22
0
.32
.36
.94
31.86
03
°142
LC)
N
°—0.46
N
N)
0.08
0
0.00
N)
03454
03
0.54
0
0.50
L()
0 0.46
In
03480
25 APR 85
JD(1 15)
GMT
151
N
C\i
0050
N
03428
0
0
60
0
2
4
6
8
10
12
26 APR 85
JD(1 1 6)
14
16
18
20
22
CMI
152
0
0
0
33.20
—0.50
N
LI)
(\4_
0.58
4.32
(N
(3
N)
aD
0.54
C
0.46
aD
03480
0
2
4
6
8
10
12
27 APR 85
J0(1 17)
14
16
18
20
22
CMI
153
:0
0
.30
—1.38
32.02
u-i
03
0156
03
0
33.20
N
060
26
22
06
10
03
0
2
4
6
8
10
12
28 APR 85
JD(1 18)
14
16
18
20
GMT
22
0
0
5,—1.34
—1.38
0
0
32.14
32.06
LC)
aD
0156
LI)
03320
N
LI)
0062
N
0
34.20
0
0014
p34.58
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N)
0
34.50
0.54
aD
0
0.50
LI)
0 0.46
0
LI)
0
34.80
0
2
4
6
8
10
12
29 APR 85
JD(119)
14
16
18
20
GMT
22
155
SPECTRA OF TEMPERATURE AND SALINITY
Spectra of temperature and salinity from all the sensors on the
central mooring are followed by temperature spectra from the satellite
moorings.
156
100
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102
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Frequency (cph)
c(185)
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102
159
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160
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Temperature
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161
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162
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102
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102
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102
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102
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Temperature
102
173
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03(249)
Temperature
102
175
VERTICAL COHERENCES
Selected coherences between vertically separated observations on
the central mooring.
176
10—s
10—2
101
10—2
10—1
100
101
102
101
102
1.00
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90
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c(257)
FREQUENCY
c(242)
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TEMPERATURE
177
10—s
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100
101
102
101
10°
FREQUENCY (cph)
102
1.00
Lu
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0.50
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180
90
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10—s
10—2
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C(242)
—
c(262)
TEMPERATURE
0
0
0
w
ci)
0
—90
—180
10—2
100
10—'
FREQUENCY (cph)
c(257)
—
c(262)
TEMPERATURE
102
0
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PHASE
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180
10—s
1.00
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0.75
0
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0.50
0.25
0.00
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(I)
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10—s
10—2
10—1
100
101
FREQUENCY (cph)
C(8o)
—
C(257)
SALINiTY
102
0
00
0
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0
PHASE
0
(0
0
00
0
0
0
COHERENCE
0
182
1.00
Li
0.75
C)
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LI
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=
0
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0.50
0.25
0.00
180
90
Li
I
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a-
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—180
10—2
100
10—1
101
FREQUENCY (cph)
C(257)
—
SALINITY
C(303)
102
183
10—2
100
101
102
100
101
102
10—1
1.00
w
0.75
0
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0
0.25
0.00
180
90
w
(I)
=
0
a-
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—180
10-s
10—2
10—1
FREQUENCY (cph)
C(303)
—
SALINITY
c(508)
1 85
HORIZONTAL COHERENCES
Selected coherences between horizontally separated temperature
observations.
1 86
10—s
1.00
hi
0.75
0
z
hi
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0
0.25
0.00
180
90
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a-
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—180
10—s
10—2
10—i
101
FREQUENCY (cph)
01(249)
—
c(257)
TEMP ERATU RE
102
10—s
10—2
1.00
0.75
0
0.50
0
0
0.25
0.00
w
I
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10—s
101
10°
FREQUENCY (cph)
10—2
10—1
01(249)
—
02(249)
TEMPERATURE
102
188
10—s
10—2
10—1
10—2
10—1
102
100
1.00
w
0.75
0
z
Ui
I0
Ui
0
0.50
0.25
0.00
Ui
(I)
—1
101
FREQUENCY (cph)
02(249)
—
TEMPERATU RE
102
189
10—s
10—2
10—1
10—2
10—1
100
101
102
101
102
1
w
0
z
Ui
Ui
0
0
Ui
(I)
I
—180
FREQUENCY (cph)
01(249)
—
03(249)
TEMPERATURE
190
10-s
1.00
LU
0.75
0
z
LU
I0
LU
0
0.50
0.25
0.00
1
LU
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100
101
FREQUENCY (cph
10—2
10—1
11(249)
—
C(257
102
191
10—s
1.00
w
0.75
0
z
w
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0
0.50
0.25
0.00
180
90
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10—i
10—2
10—1
10°
101
FREQUENCY (cph
12(249) — C(257
102
192
1
w
0
z
w
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w
180
90
Li
I
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0
—90
—180
100
101
FREQUENCY (cph
10—2
13(253)
—
102
193
10—s
101
102
100
101
FREQUENCY (cph)
102
10—2
10°
10—1
1.00
LU
0.75
0
z
LU
I00
LU
0.50
0.25
0.01
90
LU
=
a-
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—180
10—s
10—2
10—'
11(249)
TEM
—
12(249)
U
0
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z
U
I
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0
0
U
I
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0
—90
—180
10—s
10—2
10—1
100
101
FREQUENCY (cph)
12(249) —
102
195
10—s
1.00
LU
0.75
0
z
LU
a:
I0
LU
0
0.50
0.25
0.00
180
90
LU
I
(I)
0
—90
—180
10—s
101
10°
FREQUENCY (cph)
11(249) — 13(253)
10—2
10—1
TEMPERATURE
102