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The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

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Page 1: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

The Climate System

GEOL 3100

Earth’s Climate and Environment:

Past, Present, and Future

Page 2: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 3: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 4: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 5: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 6: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Uneven deliveryof Sun’s heat toEarth

Page 7: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Uneven reflection ofSolar radiation onEarth’s surface

Page 8: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

What is the definition ofAlbedo?

The percentage ofincoming radiationreflected by asurface

Albedo = = reflectivity

Page 9: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Greenhouse EffectA. Why don’t

the red arrows add up?

B. Without the GH effect, what would Earth’s avg. T be?

C. What are the main GH gases?

D. Do clouds trap or reflect heat?

A) Multiple absorption/radiation cycles, B) -16 C, C) H20 1-3%, CO2 0.035%, D) both

Page 10: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Uneven heatingof Earth’ssurface provideskey to understandingEarth’s weatherand climate

Heat deliveredvaries with1) Latitude

Page 11: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

2) Season

Page 12: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Incoming Solar Radiation (Short Wave)

Page 13: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Heat reflected varies with season

Page 14: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Heat absorbedvaries with surface

Page 15: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Outgoing Radiation (Long Wave)

Page 16: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Incoming, Outgoing and Net Radiation

Page 17: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
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Page 19: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Given theobservedvariations indelivery and reflection of solar radiation,does the variation in thelatitudinal temperatureprofile seem too big or too small?

Page 20: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Incoming, Outgoing and Net Radiation

Page 21: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Mechanisms of heat transfer in the atmosphere

• Conduction– Moves sensible heat through diffusion

• Convection– Moves sensible heat through movement of air– Moves latent heat through movement of water

• Average parcel of water travels 1000 km (LA to Denver)

Page 22: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 23: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 24: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 25: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Convection Cell

Page 26: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Is this the summer or winter monsoon?

Page 27: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 28: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 29: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Why do pollutants accumulateat high latitudes?

Page 30: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

80% of atm

99.9% of atm

Miles

31

11

5

Feet

164K

60K

26.4K

If the Earthwas thesize of abasketball,how thickwould theatmospherebe?

a fruitroll-up

Page 31: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

•Where is most of the latent heat in the atmosphere stored?•How far does the average parcel of water vapor travel?

Page 32: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 33: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Water vapor feedback

• Activity:– Work with your

neighbor to list the four steps of the water vapor feedback

• Does this feedback include clouds and the effects of latent heat?

Page 34: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 35: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

•What hemisphere is this?•How do you know?•How many of you have studied the Coriolis effect?

Eckman Spiral

Page 36: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

1000 m/hr!!

Activity:Plot the path of a parcel of air traveling 20 mph from 30N towards the equator, marking the progress each hour for 5 hoursPlot the amount of rotation of the earth for each of these points during that hour assuming that the Earth is rotating 800 mphDoes the atmosphere rotate with the Earth?If the atmosphere couldn’t quite keep up with the Earth, how would the air appear to move from the Earth’s surface

Page 37: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 38: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
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Page 40: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 41: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Water piles up2 m higher!

Circulation PenetratesTo 600-1000 mdeep

Page 42: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 43: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Surface ocean circulation

Where are the boundary currents?

Page 44: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Oceanic circulation and climate

• Water has a high heat capacity

• One third of the Earth’s heat transport from the equator toward the poles is transported by the ocean!

• Without the Gulf Stream current, Europe would be 10 – 20 °F colder

Page 45: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

What drives ocean circulation?

• Like in the atmosphere, density differences

• What changes the density of water?– Temperature: colder water is more dense– Salinity: saltier water is more dense

Page 46: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

The Gulf Stream Current• What causes the

surface ocean water to move?

• What happens to the water as it goes through the Caribbean and past Florida?

• What happens to the water as it goes towards Greenland?

• Where is most of the ocean’s deep water formed?

Page 48: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 49: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 50: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Which is the densest ocean water mass?

Page 51: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

If water goes into the deep ocean in the high latitudes, where does it come back up?

Page 52: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 53: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Are Duluth winters colder or warmer if the lake freezes over?

Page 54: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 55: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Equilibrium line

Mean annual T at Equil. line mtn glaciers = 0 CMean annual T at Equil. line ice sheets = -10 C

Page 56: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

What is an ice stream?

What is the best place to core an ice sheet?

Page 57: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 58: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 59: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

What proportion of the atmosphere, vegetation, deep ocean, and rock record exchange each year? Quickest and slowest to change?

Page 60: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 61: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
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Page 64: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Which biome has the highest albedo?Which biome has the lowest albedo?

Page 65: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 66: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future
Page 67: The Climate System GEOL 3100 Earth’s Climate and Environment: Past, Present, and Future

Where do you see theeffect of vegetation on The carbon cycle?