Energy Biosphere Flashcards

(36 cards)

1
Q

Sun

A

ultimate source of energy for movement and storage of water and for its change of state throughout hydrologic cycle

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2
Q

Measure Energy

A

in calories

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3
Q

Calorie

A

energy required to raise 1g of water at standard temp and pressure 1 degree C

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4
Q

Langley

A

how we measure energy we recieve from the sun in cal/cm^2

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5
Q

Solar Constant

A

2.0 langly/min (Ly/min)

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6
Q

Evaporation

A

cooling process, quite slow

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7
Q

Bodies

A

recieve and transmit energy

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8
Q

Black Body

A

absorbs all wavelength or incoming energy and reflect/transmit none

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9
Q

As Bodies Absorb Energy

A

tends to heat up as long as it doesn’t change state; emit more energy at shorter wavelength and reverse as it cools

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10
Q

Sun vs. Earth: Sun

A

emits a lot of energy in short wavelength range

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11
Q

Sun vs. Earth: Earth

A

much cooler; emits longer wavelength radiation

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12
Q

Wavelengths

A

terrestrial emissions are very long compared to solar emissions; we see is a very small band

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13
Q

Color

A

what we see is what is being reflected and everything else is absorbed

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14
Q

Albedo

A

ability of a body to absorb energy; % incident radiation reflected

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15
Q

High Albedo

A

large % is reflected, not absorbed

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16
Q

Albedo Varies With

17
Q

Sun’s Shortwave Incident Radiation

A

reflected by atmosphere, some absorbed, and some transmitted

18
Q

Transmitted Energy

A

can again be transmitted, absorbed, or reflected by bodies

19
Q

Sensible Heat

A

heat we feel; moves by conduction (s & l) or convection (g)

20
Q

Latent Heat

A

potential heat; accounts for evaporation, liquefaction, etc.

21
Q

Evapotranspiration Surface

A

factors that effect the evaporation/transpiration potential of the surface

22
Q

Evapotranspiration Surface Characteristics

A

field, mature growth, clear-cut, color, etc.; moisture at surface

23
Q

Solid Forest Canopy

A

type of black body (good absorber) and good radiator; great effect on shortwave, little on longwave

24
Q

Greenhouse Effect

A

longwave emitted from canopy may be captured by atmosphere due to high moisture and CO2

25
Net Result of Forest Canopy
forests are cooler during the day and warmer at night
26
Radiation
function of temp; can estimate canopy temp by sensing radiant flux at some wavelength
27
Evapotranspiration
amount is directly related to available energy; evaporation if surface is wet, none if dry
28
Land Management Effect
forests are most efficient at using available energy for evapotranspiration; clear cuts and meadows are much less efficient
29
Evapotranspiration and Biosphere
vegetated zone; has movement, processes, and storage capabilities; water may move between atmosphere and soil
30
Interception
results in an amount of precipitation being prevented as it attempts to reach the ground; can be redistributed; depth, not volume; referred to as a loss
31
Interception and Redistribution Cycle
precipitation falls, intercepted water is evaporated, drips, throughfall, stemflow...repeat
32
Interception Mechanics
slows down fall velocity, protects soil from eroding, high canopies could reproduce tall velocities
33
Erosion Effects
fine particles clog pores, raindrop impacts or overland flow initiate erosion, soil aggregates break down
34
Forest Litter
leaves > wet leaves > decomposition > soil (top to bottom); stores tons of water
35
Increase Interception
conversion to pine/fir; decreases amount reaching ground
36
Decrease Interception
thinning of forest; increases amount reaching ground