Download - Solar Energy, the Atmosphere and Biomes
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Solar Energy, the Atmosphere and Biomes
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Earth-Sun Relationships
Earth’s Motions• Earth has two principal motions—rotation and
revolutionEarth’s Orientation (tilt)• Seasonal changes occur because Earth’s
position relative to the sun continually changes as it travels along its orbit
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Energy Transfer as HeatThree mechanisms of energy transfer:Conduction is the transfer of heat through matter
by molecular activityConvection is the transfer of heat by circulation
within a substance.Radiation is the transfer of energy (heat) through
space by electromagnetic waves that travel out in all directions
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What Happens to Solar Radiation?
• Scattering:–Clouds, dust and gas reflect and bend light
rays; light rays are sent out in all directions–Causes sky to appear blue (blue light is more
easily bent)– Sunsets appear red because longer
wavelengths (red) are able to reach the surface (we are looking through more atmosphere on the horizon)
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What Happens to Solar Radiation?
• Reflection:–20% of solar radiation is absorbed by the
atmosphere–50% is absorbed by the surface–30% is reflected back into space–Albedo: fraction of solar radiation that is
reflected back into space. – Earth’s albedo is 0.3
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What Happens to Solar Radiation?
Absorption & Infrared Energy:• As the surface absorbs radiation, it heats up and
releases IR radiation• IR radiation is trapped by water vapor and CO2 in
the atmosphere• This process is called the greenhouse effect
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What Happens to Solar Radiation?
Why Temperatures VaryFactors include:• latitude • heating of land and water, • altitude• geographic position• cloud cover• ocean currents
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Fig. 7-7, p. 145
Prevailing winds pick up moisture from an ocean.
On the windward side of a mountain range, air rises, cools, and releases moisture.
On the leeward side of the mountain range, air descends, warms, and releases little moisture.
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Latitude
Tropical Forest
Deciduous Forest
Coniferous Forest
Tundra (herbs, lichens, mosses)
Polar ice and
snow
Fig. 7-9, p. 147
ElevationMountain ice and snowTundra (herbs, lichens, mosses)Coniferous Forest
Deciduous ForestTropical Forest
Stepped Art
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Properties of Air
Density• At constant pressure, warm is less dense than
cold air• Therefore, warm air rises, cold air sinks
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Properties of Air
Water Vapor Capacity• Warm air has a higher capacity for water• Specific humidity is a measure of the amount of
water vapor in the air• Relative humidity is a ratio of the amount of
water present to the capacity• If RH = 100%, saturation occurs• Dew point is the temperature at which
saturation occurs
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Properties of Air
Adiabatic Heating and Cooling• As air rises in the atmosphere rises, P ↓, air
expands and cools• As air sinks toward the surface, P ↑, air
volume ↓ and warms
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Properties of Air
Latent Heat Release• As the sun warms surface water, it absorbs
and stores energy as it evaporates• As water vapor in the atmosphere condenses,
it releases this stored (latent) energy
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Factors Affecting Wind• Wind is the result of horizontal differences in air
pressure. Air flows from areas of higher pressure to areas of lower pressure
• The unequal heating of Earth’s surface generates pressure differences
• Three factors combine to control wind: pressure differences, the Coriolis effect, and friction
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Factors Affecting Wind
Pressure Differences• A pressure gradient is the amount of pressure
change occurring over a given distance• Isobars are lines on a map that connect places
of equal air pressure• Closely spaced isobars indicate a steep pressure
gradient and high winds
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Factors Affecting Wind
Coriolis Effect• The Coriolis effect describes how Earth’s
rotation affects moving objects. • In the Northern Hemisphere, all free-moving
objects or fluids, including the wind, are deflected to the right of their path of motion.
• In the Southern Hemisphere, they are deflected to the left
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Factors Affecting Wind
Friction • Friction acts to slow air movement, which
changes wind direction• Jet streams are fast-moving rivers of air that
travel in a west-to-east direction (120 - 240 km/hour); little friction
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Global Winds
• Convection Cells:–Warm air rises near the equator–Cooler air from the north replaces it at the
surface–The warm air that rose flows northward
and downward as it cools–The convection cells are called Hadley Cells
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Fig. 7-4, p. 143
Heat released radiates to spaceCool, dry
air
Condensation and precipitation
Falls, is compressed, warms
Rises, expands, cools
Warm, dry air
Hot, wet air
Flows toward low pressure, picks up moisture and heat
HIGH PRESSURE Moist surface warmed by sun
LOW PRESSURE
LOW PRESSURE HIGH PRESSURE
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Global Winds & Biomes
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Fig. 7-6, p. 144
Moist air rises, cools, and releases moisture as rainPolar cap
Arctic tundraEvergreen coniferous forest60°
Temperate deciduous forest and grassland
30°Desert
Tropical deciduous forest
Equator 0° Tropical rain forest
30° Desert
60°Temperate deciduous forest and grassland
Tropical deciduous forest
Polar cap
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Fig. 7-8, p. 146
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Fig. 7-10, p. 147
Cold Polar
TundraSubpolar
TemperateConiferous forest
Desert
Deciduous forest
GrasslandChaparral Tropical
Hot
DesertWet Rain forest Savanna
Tropical seasonal forest
Dry
Scrubland
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Biomes
• Tundra• Boreal forest• Temperate rainforest• Temperate seasonal forest• Woodland/shrubland• Tropical rainforest• Subtropical desert
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CURRENTS
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Fig. 7-2, p. 142
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Fig. 7-5, p. 143
Warm, less salty, shallow current
Cold, salty, deep current
Thermohaline Circulation
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El Nino Southern Oscillation
• 3 – 7 year cycle• Surface currents in the tropical Pacific reverse
direction (trade winds weaken)• Warm water moves westward, suppressing the
upwelling of nutrients off the coast of S. America• Fish populations are hurt• Global impact: cooler, wetter conditions in SE US;
drier in S Africa, SE Asia
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Biomes
For your biome PowerPoint:• Describe vegetation and animal life• Describe general climate; include global
location(s)• Include a climate diagram (annual
temperature & rainfall)• 3 – 5 slides; keep it simple!
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AQUATIC BIOMESCategorized by salinity, depth, water flow
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Streams & Rivers
• Flowing fresh water• Originate from springs or runoff• Rapid flow = few producers; rely on terrestrial
biomes (leaves)• Slow rivers: nutrients settle and provide
substrate for plants• Rapids: high O2 content
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Lakes and Ponds
• Contain standing water• Divided into distinct zones:• Littoral Zone: shallow area of soil & water
near shore; rooted plants, photosynthesis• Limnetic Zone: rooted plants cannot survive;
phytoplankton photosynthesize• Profundal Zone: deep lakes; low O2 due to
decomposers; muddy bottom: benthic zone