Energy Biosphere Flashcards

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

A

wavelength

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
Q

Net Result of Forest Canopy

A

forests are cooler during the day and warmer at night

26
Q

Radiation

A

function of temp; can estimate canopy temp by sensing radiant flux at some wavelength

27
Q

Evapotranspiration

A

amount is directly related to available energy; evaporation if surface is wet, none if dry

28
Q

Land Management Effect

A

forests are most efficient at using available energy for evapotranspiration; clear cuts and meadows are much less efficient

29
Q

Evapotranspiration and Biosphere

A

vegetated zone; has movement, processes, and storage capabilities; water may move between atmosphere and soil

30
Q

Interception

A

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
Q

Interception and Redistribution Cycle

A

precipitation falls, intercepted water is evaporated, drips, throughfall, stemflow…repeat

32
Q

Interception Mechanics

A

slows down fall velocity, protects soil from eroding, high canopies could reproduce tall velocities

33
Q

Erosion Effects

A

fine particles clog pores, raindrop impacts or overland flow initiate erosion, soil aggregates break down

34
Q

Forest Litter

A

leaves > wet leaves > decomposition > soil (top to bottom); stores tons of water

35
Q

Increase Interception

A

conversion to pine/fir; decreases amount reaching ground

36
Q

Decrease Interception

A

thinning of forest; increases amount reaching ground