Chapter 8: Circulation of the Atmosphere Part II and...
Transcript of Chapter 8: Circulation of the Atmosphere Part II and...
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Chapter 8:
Circulation of the Atmosphere Part II
and
Chapter 9:
Circulation of the Ocean Part I
1Photo from The Cloud Appreciation Society
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If the Earth’s latitude causes differences
in direct heating of the Earth,
what causes seasons?
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Temperature is lower at higher
latitudes:
1) Bigger area
2) More atmosphere
3) Reflection is higher (albedo)
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What drives Earth’s temperatures?
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Although average
temperature constant,
distribution not equal.
Oceans and atmosphere
move excess heat from
equator to poles.
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Movement of the Atmosphere
• Air always flows from high to low pressure.
• Wind – moving air
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Convection: heat transfer by moving fluids.
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Smaller scale examples of convection cells:
sea breezes (day)
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Smaller scale examples of convection cells:
land breezes (night)
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This is a cartoon of a very
simple model of
atmospheric circulation:
you would expect
air to rise at the Equator,
move to the poles,
and sink.
Thickness of the
atmosphere is not to scale!!
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Coriolis Effect
But that’s not what happens
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Coriolis force cause objects to move:
right in northern hemisphere
left in southern hemisphere
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http://www.classzone.
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Chapter 9:
Circulation of the Ocean
“Tropical” gardens on Britain’s Scilly
Isles. Only 48 kilometers (30 miles)
off the coast of Cornwall at 50° N,
these scenic islands lie in the path of
the warm waters of the Gulf Stream.
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Learning Goals:
Circulation of the Ocean
• Ocean circulation is driven by winds and by differences
in water density. Winds and ocean currents distribute
heat worldwide.
• Surface currents: driven by wind, they move in
circular patterns (gyres) around the edges of major
ocean basins. Surface = top 100 meters
• Thermohaline currents: slow, deep currents that affect
the bulk of seawater below the pycnocline.
• Upwelling supports the most productive fisheries.
• El Niño and La Niña affect ocean and atmosphere.
In El Niño years, the normal wind and current flow
changes near the coast of Peru (and influences the
whole world). 14
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Winds, driven by uneven
solar heating and Earth’s
spin, drive the movement
of the ocean’s surface
currents.
Two types of winds are
most important to ocean
circulation:
1) powerful westerlies
and
2) persistent trade winds
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Northern
Hemisphere:
Coriolis Effect moves
surface waters to
right of winds.
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Gyres –
surface currents
circulating around
ocean basins
Four processes
(or things)
create gyres:
1. Sun’s heat
2. Surface winds
3. Coriolis effect
4. Land
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For example,
the North
Atlantic Gyre
includes four
currents.
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Earth has 2 northern gyres, 4 southern.
North Pacific Gyre
North
Atlantic Gyre
South Pacific GyreSouth
Atlantic Gyre
Indian
Ocean Gyre
Circum - Antarctic Gyre
Surface currents can be illustrated by
sea surface temperature.
Red: 25°–28°Celsius (77°–82°F).
Yellow: 20°–25°C (68°–77°F);
Green: 15°–20°C (59°–68°F);
Blue: 0°–15°C (32°–59°F).
Purple: below the freezing point of fresh water.
Note the distortion of the temperature patterns we might expect
from the effects of solar heating alone—the patterns twist
clockwise in the Northern Hemisphere, counterclockwise in the
Southern.
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Waters brought from equator – warm-water current
“ “ “ poles – cold-water current
Surface currents, summarized with
names and usual directions.
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