ISP217 Exam 1 Flashcards

1
Q

Polarity

A

H2O molecules are polar, meaning they have a more positive side and a more negative side, causing the molecules to connect to each other.
-best solvent for salt
-high surface tension
high latent heat

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2
Q

Specific Heat

A

Amount of energy required to raise temperature by 1 degree Celsius.

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3
Q

Infiltration

A

Precipitation seeps into the ground.

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4
Q

Evapotranspiration

A

Evaporation from ground and transpiration from plants.

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5
Q

Atmospheric Advection

A

Water transported from sea to land by wind.

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6
Q

Convection

A

Heat passed through contact.

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7
Q

Water Table

A

Layer of saturated soil above an unconfined aquifer.

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8
Q

Vadose Zone

A

Unsaturated soil above water table above unconfined aquifer.

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9
Q

Aquitard

A

Zone of clay/non-porous rock that stops flow from one aquifer to another.

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10
Q

Ogallala aquifer

A

Central U.S., recharge is 10% annual withdrawal. Porous material changing, limiting recharge permanently.

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11
Q

Visible Light

A

A small portion of the wavelength spectrum. 50% of all solar radiation.

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12
Q

UV Light

A

Vitamin D, sunburn/cataracts - damage at the molecular level, but most blocked by ozone and O2.

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13
Q

Infrared Light

A

Emanated by warm objects - rattlesnakes hunt.

Heats water by causing vibration.

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14
Q

Mexico City

A

Sinking a few inches every year because of depletion of water in aquifer.

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15
Q

Energy that drives weather

A

Radiation (Sun), thermal (heat air + water), mechanical (wind/water currents)

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16
Q

Condensation Level

A

Height at whig air becomes saturated because of cooling (due to expansion) and condenses into clouds.

17
Q

Convection

A

Rising air expands, cools, relative humidity rises until condensation of water vapor occurs above condensation level.

18
Q

Circulation Cell

A

Air heated most (equator), rises through troposphere, hits the stratosphere and starts moving laterally across the top of the troposphere, cools, sinks. Repeat.

19
Q

Factors that affect air density

A

Temperature and water content.

20
Q

Dense Air

A

Heavier, cooler, drier

21
Q

Attenuate

A

How water is less available through water.

Water/dissolved chemicals/particles (phytoplankton, suspended sediment).

22
Q

Attentuation Coefficient

A

K - how fast light attenuated - larger K = more attentuation

23
Q

Compensation Depth

A

Where there is neither an increase nor a decrease in O2 - where respiration and photosynthesis produce and consume the same amount of oxygen.

24
Q

Density of water

A

Mass per unit of volume.
Freshwater is densest at 1 degree C = 1 g/mL
Ice much less dense than water.
Warm water less dense than cold water.

25
Q

Temperature Profiles

A

Spring - isothermal, complete mixing
Summer - stratification
Fall - isothermal
Winter - stratification

26
Q

Ocean Water

A

Density at 4 degrees C is 1.028 g/mL

Freezes at -2 degrees (max density)

27
Q

Salinity

A

Lowest in arctic (cool/wet)
Highest at Tropic of Cancer (warm/dry)
Lower at the tropics (warm/wet)

28
Q

Spatial variation of density

A

Driven by temp

Highest in south, then north, then tropics

29
Q

Wave height

A

Due to wind speed, duration, fetch