Temperature

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Weather & Water Cycle

Donna Barrett, MRESA

Wet Jeans

Wet Jeans

• Read your handout and then on NOTEBOOK paper, record the single answer you feel is correct.

• Then provide an explanation for your answer.

Wet Jeans

The best response is C – it is in the air in an invisible form.

The invisible form is water vapor.

Water does not immediately go up into the clouds.

Wet Jeans

• The best responses is C – it is in the air in an invisible form.

• Water may not immediately go up to the clouds as depicted in water cycle diagrams.

• Humid weather is an example of water in the air.

• Wet dew on the grass, fog, and condensation of water on the outside of a glass holding cold liquid confirms that water exists in the air around us.

The Water Cycle

http://ga.water.usgs.gov/edu/waterproperties.html

Water is Stored

• The oceans are a major storehouse of water

• Lakes, rivers and glaciers are also storehouses of water http://ga.water.usgs.gov/edu/watercyclesummary.html

Evaporation

http://ga.water.usgs.gov/edu/watercyclesummary.html

• Evaporation is the process by which water changes from a liquid to a gas or vapor.

– 90% - oceans, lakes

– 10% - plants

• Heat (energy) is necessary for evaporation to occur.

• Energy is used to break the bonds that hold water molecules together, which is why water easily evaporates at the boiling point (212° F, 100° C) but evaporates much more slowly at the freezing point.

Condensation

• Condensation is the process in which water vapor in the air is changed into liquid water.

• Precipitation is the primary route for water to return to the Earth's surface within the water cycle.

• Condensation is responsible for ground level fog, for your glasses fogging up when you go from a cold room to the outdoors on a hot, humid day, etc.

http://ga.water.usgs.gov/edu/watercyclesummary.html

Evapotranspiration

• The process by which moisture is from plants released to the atmosphere.

• About 10 percent of the moisture found in the atmosphere is released by plants through transpiration.

• Plant transpiration is an invisible process.

• A large oak tree can transpire 40,000 gallons

(151,000 liters) per year.

http://ga.water.usgs.gov/edu/watercyclesummary.html

Explore: The Incredible Journey

• Where will the water you drink this morning be tomorrow?

• You are going to become water molecules moving through the water cycle .

• Water can move through: Clouds, Plants,

Animals, Oceans, Rivers, Lakes,

Ground Water, Soil, and Glaciers. http://www.earthsciweek.org/forteachers/incrediblejourney_cont.htm

Sublimation

http://ga.water.usgs.gov/edu/watercyclesummary.html

• Sublimation is process of snow and ice changing into water vapor without first melting into water.

• Sublimation occurs more quickly at low relative humidity and dry winds.

• Occurs more at higher altitudes , where the air pressure is less than at lower altitudes.

• Energy is needed.

Atmosphere

• Not a great storehouse of water

• Superhighway used to move water around the globe.

• There is always water in the atmosphere. Clouds are a visible form atmospheric water

• If all of the water in the atmosphere rained down at once, it would only cover the ground to a depth of 2.5 centimeters, about

1 inch.

http://ga.water.usgs.gov/edu/watercyclesummary.html

How would the following factors effect rates of transpiration?

• Temperature

• Humidity

• Wind

• Soil Moisture Availability

• Type of Plant

Atmospheric Conditions Affecting

Transpiration

up, especially during the growing season, when the air is warmer due to stronger sunlight and warmer air masses.

Relative humidity: As the relative humidity of the air surrounding the plant rises the transpiration rate falls. It is easier for water to evaporate into dryer air than into more saturated air.

Wind and air movement: Increased movement of the air around a plant will result in a higher transpiration rate.

Soil-moisture availability: When moisture is lacking, plants can begin to senesce (premature ageing, which can result in leaf loss) and transpire less water.

Type of plant: Plants transpire water at different rates. Some plants which grow in arid regions, such as cacti and succulents, conserve precious water by transpiring less water than other plants. http://ga.water.usgs.gov/edu/watercyclesummary.html

What are clouds made of?

• Keeley, Page. “Uncovering Student Ideas” Vol.

3

What are clouds made of?

• Best response: Glenda – “I think clouds are made of tiny drops of water or tiny ice crystals.”

• Clouds are formed when water vapor in the air cools, condenses, and becomes tiny droplets of water (or ice crystals)

Rainfall

• Keeley, Page. “Uncovering Student Ideas” Vol.

3

Rainfall

• Best answer: Marcus – “ I think rainfalls when water drops in the cloud get too heavy.”

• Middle School students are gaining a more conceptual understanding of the processes of the water cycle AND the relationship between the mass of an object, the upward force of air and downward force of gravity.

Precipitation

• The discharge of water, in liquid or solid state, out of the atmosphere

• Rain, freezing rain, sleet, snow, or hail

• Delivery of atmospheric water to the Earth

• Most precipitation falls as rain

• Water droplets must condense on tiny dust, salt, or smoke particles, which act as a nucleus

• Water droplets grow as a result of condensation of water vapor when the particles collide.

• Millions of cloud droplets are required to produce a single raindrop http://ga.water.usgs.gov/edu/watercyclesummary.html

What do raindrops look like?

• Spherical – less than 1 mm

• Bottom starts to flatten out as they grow 2 – 3 mm

• At 4 – 5 mm they look like a parachute and begin to fall apart http://ga.water.usgs.gov/edu/watercyclesummary.html

Infiltration

http://ga.water.usgs.gov/edu/watercyclesummary.html

Factors Affecting Infiltration

• Precipitation

• Soil

Characteristics

• Soil Saturation

• Land Cover

• Slope of the Land

• Evaporation http://ga.water.usgs.gov/edu/watercyclesummary.html

Water Cycle Placemat

http://ga.water.usgs.gov/edu/watercycleplacemat.html

3 x 3 Vocabulary

Condensation Clouds

Evaporation Lakes

Runoff

Infiltration

Precipitation Transpiration Groundwater

3 x 3 Vocabulary

Condensation Ground water Runoff

Evaporation Rain

Transpiration Lake

Precipitation

Water Cycle

Water Cycle Manipulative

Water Cycle Bracelet

Oceans

Seas

Lakes

Streams

Ponds

River

Semantic Grid Analysis

Fresh Stag Moving Salt Fresh Stag Moving Salt

Puddle

Dams/

Reservoir

Marshes

Estuaries

(brackish)

Spring

Ground

Water

(Aquifer)

1 new idea you learned

2 factors affecting infiltration of groundwater

3 sources of water storage

Blast

Off!

Differentiate instruction

Activities to Enhance the Development of

Nonlinguistic

Representations

Creating graphic representations/organizers

– Descriptive patterns

Fact

Fact

Fact

TOPIC

Fact Fact

Differentiate instruction

Find a new partner at a different table.

• Get comfortable.

A will face the screen

B will face

A

.

A / B

A has the task of getting

B to guess the mystery word.

Only non-linguistic representations will be shown. Feel free to skip and go back if necessary. When all answers have been given stand up and give a shout !

1 .

2 .

3

4.

5.

6 .

Using only a piece of paper and pen, draw and get your partner to say these words

Groundwater

Evapotranspiration

Precipitation

Water Cycle

Heat Energy

• The Sun’s energy is the origin of weather

Temperature

• Related to thermal energy

• Temperature is the average kinetic energy of a system

• Use standard units for measuring temperature

– Celsius

– Kelvin

– Fahrenheit temperature illustration

Common Temperature Scales

• The degree Celsius (°C) scale was devised by dividing the range of temperature between the freezing and boiling temperatures of pure water at standard atmospheric conditions (sea level pressure) into 100 equal parts.

• The degree Fahrenheit (°F) nonmetric temperature scale was devised and evolved over time so that the freezing and boiling temperatures of water are whole numbers; 0 is the freezing point of salt water http://en.wikipedia.org/wiki/Fahrenheit http://lamar.colostate.edu/~hillger/temps.htm

Making Sense of Celsius

• Look for patterns in the chart.

• What do you notice?

• Let’s graph the “points” from the chart on the coordinate grid.

• What would be the best increments to use on the x axis and y axis?

• Extension: Questions 1 – 4 at the bottom of the page.

• Linear relationship

• Slope = rise/run or change in y/change in x

• Used to derive the conversion formulas we use

• Many cell phone apps with conversions

degree Fahrenheit / degree

Celsius conversions

• F = C x 9/5 + 32

• F = (C x 1.8) + 32

• C = 5/9(F – 32)

• C = (F - 32) / 1.8

Temperature Benchmarks

Common Temperature

Comparisons

Boiling point of water

Hot bath

Average human body temperature

Nice day at the beach

Average room temperature

Cool day

Melting point of ice

Very cold day

Celsius

Prediction degree

Fahrenheit

212

104

98.6

86

70

50

32

0

Temperature Benchmarks

Common Temperature

Comparisons

Boiling point of water

Hot bath

Average human body temperature

Nice day at the beach

Average room temperature

Cool day

Melting point of ice

Very cold day

Celsius

Prediction

100

40

37

30

21

10

0

-18 degree

Fahrenheit

212

104

98.6

86

70

50

32

0

Temperature Mnemonics

When it's zero it's freezing, when it's 10 it's not, when it's 20 it's warm, when it's 30 it's hot!

Thirty is hot

Twenty is nice

Ten is cool

Zero is ice http://lamar.colostate.edu/~hillger/temps.htm

Anticipation Guide

___ 1. Heat energy from the sun drives the weather system

___ 2. Land heats up faster than water.

___ 3. Winds blow as a result of the ___ movement of air from low to

___

___ high pressure

___ 4. Warm air rises and cool air sinks ___

___ 5. The evaporation of moisture from ___ oceans causes hurricane

Camping Trip, Vol. 4

• Which friend do you most agree with?

Camping Trip, Vol. 4

• The best answer is Emma’s. The coldest part of the day is generally right around the dawn, actually right after the sunrise while the Sun is still very low on the horizon.

• During the night, the Earth’s surface radiates the heat it has absorbed back into space, allowing the temperature to drop.

Heat Transfer

• Radiation – energy from the sun travels to the earth via radiation

• Conduction – direct transfer of heat from one substance to another – air heated by the ground

• Convection – transfer of heat in a fluid – warm air rises and cool air sinks

Heat Transfer:

• Radiation – heat is transferred through electromagnetic waves

• Do not need a medium to travel

– Radiant energy (light)

– Microwaves

– Radiowaves

Heat Transfer: Conduction

• Conduction – direct contact; heat moves from the warmer to the cooler object

Heat Transfer: Convection

Hot water rises, cools, and falls.

Heated air rises, cools, then falls. Air near heater is replaced by cooler air, and the cycle repeats.

What if coils were at the bottom? http://sol.sci.uop.edu/~jfalward/heattransfer/heattransfer.html

Heat, Temperature & Thermal

Energy

• Temperature measures how hot or cold something is or the average motion of the molecules

• Thermal energy – the total energy of all of the molecules (large pot of soup vs. small pot of soup – which one has move TE?

• Heat – the movement of thermal energy – warm to cool

Air Movement - Wind

• Winds are formed by the movement of air from one place to another

• Air moves from high pressure to low

• 2 Types:

– Local – blow in any direction and cover short distances

– Global – blow in same direction and cover long distances

– Name of the wind tells you the direction it is blowing FROM

• Convection currents

Warm vs. Cold Air

Warm Air

•Molecules are less dense; spread out; rise

LOW pressure

•Wet, rainy, warm

Cold Air

•Molecules are sinking; getting pushed together; more dense

HIGH pressure

•Warm air rises and is replaced by colder air which causes local winds

•Air moves from high to low pressure

Land Breeze

http://www.dlt.ncssm.edu/resources/images/seabreeze_day.jpg

Sea Breeze

http://www.dlt.ncssm.edu/resources/images/seabreeze_night.jpg

Wind & Pressure Stations

• Beaufort Scale

• Why Winds Whirl

• Just A Gust

• Pressure Points

Global Winds

•Air near the equator is heated rapidly and pushed toward the poles as polar air sinks back toward

•Because the earth is rotating and is greater in diameter near the middle causing different rotation speeds, the winds change speed and direction, this accounts for the movement of air on a global scale.

http://ww2010.atmos.uiuc.edu/(Gh)/wwhlpr/hurricane_globalwinds.rxml

Beaufort Scale – Wind Speed

Beaufort number

0

7

8

5

6

9

1

2

3

4

10

11

12-17

Wind speed

(km/hr)

<1

1-5

6-11

12-19

20-28

29-38

39-49

50-61

62-74

75-88

89-102

103-117

>117

International description

Calm

Light Air

Light Breeze

Gentle Breeze

Moderate Breeze

Fresh Breeze

Strong gale

Fresh Breeze

Fresh gale

Stong gale

Whole gale

Storm

Hurricane http://www.windows.ucar.edu/tour/link=/earth/Atmosphere/wind_speeds.html

Air Pressure

• Measure of the force of air pressing down on the Earth’s surface

• Approximately 800 km deep

• Depends on the density of air

• Greater density leads to greater pressure

• Measured in Hectopascals or Millibars; previously in inches

• Measured with a barometer

Factors Affecting Air Pressure

• Altitude of elevation

• Water vapor

• Temperature

• Uneven heating is due to many factors such as: angle of suns radiation, differences in absorption and reflection of material, & regional climate

• The shifting causes great swirling air masses called high or low pressure cells

High & Low Pressure

• Convection & uneven heating of the Earth causes north to south winds and rotation turns the winds east or west depending on the hemisphere

Highs and Lows

Highs

• Fair

• Wind circulation is clockwise in northern hemisphere & counterclockwise in southern

• Winds are light

• Warm or cold for relatively long periods without

Lows

• Generally cloudy, with rain of snow

• Wind circulation is counterclockwise in the northern hemisphere & clockwise in the southern hemisphere

• Winds are strong

Where Did the Water Come

From?

• Choose your answer.

• Making a Human Scatter plot

• Stand in line with the letter you most closely agree with – determine how strongly you feel your answer is correct.

• Source: Uncovering Student Ideas – Page Keeley

Where did the water come from?

• The best response is A: a gas in the air – the phenomenon described is condensation that occurs on the outside of a cold object when the object comes in contact with warmer air that contains water vapor.

The Water Cycle

http://ga.water.usgs.gov/edu/waterproperties.html

Recycled Water: The

Hydrological Cycle

• Source: Project Earth Science:

Meteorology

Water Cycle Placemat

http://ga.water.usgs.gov/edu/watercycleplacemat.html

Wet Jeans

• Which student do you most agree with?

Wet Jeans, Vol. 1

• The best response is C – it is in the air in an invisible form. The invisible form is water vapor. Water does not immediately go up into the clouds as students often think.

What are clouds made of?

• Which friend do you most agree with?

• Source: Uncovering Student Ideas in Science, Page

Keeley

What are clouds made of?

• The best response is Glenda’s

• Clouds come in a variety of shapes and sizes. All are formed when water vapor in the air cools, condenses and becomes tiny drops of liquid water or tiny ice crystals.

Moisture

• Sun’s energy turns liquid water into a gas

( EVAPORATION )

• Leads to the formation of CLOUDS

• Wind transports moisture all over the world

• HUMIDITY – a measure of the amount of water held in the air

• Relative Humidity – percentage of moisture air holds compared to the amount it could hold

• Psychrometer – measures relative humidity

• Air will hold water vapor until saturated or until

100% relative humidity

Moisture Stations

• Make Dew

• Make Frost

• Make Clouds

• Cloudy Logic

• Marlee’s unit for 4 th grade

• http://discoverwater.org

Dew Point – Just Dew It!

• Temperature at which water condenses (gas is converted to a liquid)

• The capacity of air to hold water vapor depends on temperature. Warm air holds more moisture than cold air.

• Alternative:

– Fill a beaker half with water. Allow the water to reach room temperature.

– Add 3 – 4 ice cubes to the beaker. Stir.

– Continue stirring until moisture appears on the outside.

Record temperature.

– Temp. of Room____Initial___ Dew Point____

Dew Point

• Analysis of Class Data

• Questions:

– What does dew point measure?

– If the temperature of the air is close to the dew point, what type of weather will most likely be experienced?

– Why do we see dew in the morning? Where did the water come from?

Patterns and Predictions (AIMS)

• Dew point temperature can be higher than air temperature.

No

• Dew point temperature can be the same as the

Yes air temperature.

Yes, most likely

• Dew point temperature can be lower than the air temperature.

Cloud Formation

Clouds

• Form when moisture in the air condenses on small particles of dust or solids in the air

• Warm air can hold more moisture than cold air

• 3 Basic Types

– Cumulus – puffy white clouds; can become tall

– Stratus – form smooth layers; low altitude; indicate fair weather or precipitation

– Cirrus – high altitude, appear feathery, wispy, fair weather clouds

• What does “nimbo” mean?

• Rain

• http://www.eo.ucar.edu/webweather/cloud3.html

Rainfall

• Which friend do you most agree with?

• Source: Uncovering Student Ideas in Science,

Page Keeley

Rainfall

• The best response is Marcus’s

• Precipitation is a complex process. A simple explanation begins with water vapor in the warm air rising in the sky, cooling to the dew point (where condensation occurs), and forming tiny drops of suspended liquid water.

• When there are enough of these tiny drops of suspending liquid water, they accumulate to form clouds. Some of the drops combine and form larger droplets. Eventually the large drops are too heavy to remain suspended and fall to the ground due to the force of gravity.

Precipitation

• Forms: Rain, Snow, Sleet, & Hail

• Must have clouds in order to form

• Each droplet forms around foreign particles such as dust, smoke, or salt in the cloud & the microscopic particle is known as a condensation nucleus

• The vapor in the cloud must have a place to condense in order to form precipitation

• These microscopic molecules run into each other in the cloud and combine until they become large and heavy and then gravity takes over.

Anticipation Guide

___ 1. Heat energy from the sun drives the weather system

___ 2. Land heats up faster than water.

_T_

_T_

___ 3. Winds blow as a result of the movement of air from low to high pressure

___ 4. Warm air rises and cool air sinks _T_

_F_

___ 5. The evaporation of moisture from _T_ oceans causes hurricane

1 new idea you learned about weather

2 types of winds

3 factors that effect weather

Blast

Off!

Weather Maps

http://pafc.arh.noaa.gov/tvwx.php?img=symbols

Isobars

• Atmospheric pressure is plotted on maps by the use of lines called isobars. Each isobar connects points having equal air pressure expressed in units of millibars (mb) in the

United States

Air Masses

• Large bodies of air with the same properties and cover thousands of kilometers

• Temperature & moisture are similar

• Take on the same temperature

& moisture properties of the area over which they form

• Classified based on where they form

• 4 Types:

– Warm (Tropical) – form in tropical areas

– Cold (Polar) – form in polar regions

– Wet (Maritime) – form over the oceans

– Dry (Continental) – form over land

Fronts

• Boundary between air masses

• Named according to direction of movement

Fronts

• Fronts are the transition zones between two air masses

• Cold front

• Warm Front

• Stationary Front

• Occluded Front

• Dry Line Front

Density of Water

• Is cold air denser than hot?

• Procedure:

– Fill plastic shoe box ¾ full of COLD water

– Fill a test tube with HOT water – color with red food coloring (water should not be too hot)

– Hold your finger over the bottle and place it horizontally at the bottom of the cold water

– Sketch the direction of flow of the HOT water

– Repeat the procedure using a large container of

HOT water and a small container of COLD water colored blue

Warm Front – warm air replaces cold

Warm Air

•Molecules are less dense; spread out

•Low pressure

•Wet, rainy, warm

Cold Air

•Molecules are sinking; getting pushed together; more dense

•High pressure http://www.physicalgeography.net/fundamentals/images/warmfront.GIF

Cold Front – cold air replaces warm – Stormy

Weather – followed by sunny, cool

Cold Air

•Molecules are sinking; getting pushed together; more dense

•High pressure

Warm Air

•Molecules are less dense; spread out

•Low pressure

•Wet, rainy, warm http://www.physicalgeography.net/fundamentals/images/warmfront.GIF

Front Symbols

Differentiated Stations

• 6 th Grade: Interpreting Weather Maps &

Hurricanes (AIMS)

• 4 th Grade: Fronting the Weather (AIMS) &

Making Instruments

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