Readings Flashcards

1
Q

depression storage

A

water temporarily stored on the land surface as ice and snow or water in puddles

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2
Q

infiltration

A

If the surface soil is porous some rain or melting snow will seep into the ground.

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3
Q

vadose zone

A

zone of aeration.

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4
Q

interflow

A

water flows laterally into the vadose zone

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5
Q

Excess vadose water is pulled downward by gravity through a process known as

A

gravity drainage

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6
Q

capillary fringe

A

the pores are filled with capillary water so the saturation approaches 100%, however the water is held in place by capillary forces.

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7
Q

The top of the zone of saturation is called…

A

the water table.

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8
Q

Water stored in the zone of saturation

A

ground water

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9
Q

Ground-water flow

A

water stored in the zone of saturation moves through the rock and soil layers of the earth until it discharges as a spring or as seepage into a pond, lake, stream, river or ocean.

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10
Q

baseflow

A

Ground water contribution to a stream.

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11
Q

Surface water

A

water stored in ponds, lakes, rivers, and streams

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12
Q

magmatic water

A

water contained within magmas deep in the crust. If the magma reaches the surface of the earth or the ocean floor, the magmatic water is added to the water in the hydrologic cycle. (ex- steam seem in some volcanic eruptions)

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13
Q

Types of water that can be located in the vadose zone

A

vadose water, capillary water, intermediate vadose water, soil water.

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14
Q

ground-water basin

A

the subsurface volume through which ground water flows towards a specific discharge zone.

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15
Q

hydrologic inputs to an area may include

A

precipitation, surface-water inflow (run off and overland flow), ground water-inflow, artificial import of water into the area through pipes and canals.

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16
Q

hydrologic outputs from an area may include

A

evapotranspiration, evaporation of surface water, surface water runoff, ground water outflow, artificial export of water through pipes and canals.

17
Q

Since diversions have started in Mono lake how has the surface elevation changed.

A

It has declined substantially. A historic low was reach in the 90s, and then through rain and court orders it began to rise again. However even without the diversions it continued to decline. In the 90s it finally began to rise again.

18
Q

absolute humidity

A

the number of grams of water per cubic meter of air

19
Q

saturation humidity

A

At any given time the maximum moisture and air mass can hold.
Directly proportional to temperature

20
Q

Condensation occurs when

A

An air mass is cooled and the saturation humidity value drops and the air mass can no longer hold all of it’s humidity.

21
Q

Dew point

A

the temperature at which condensation will begin.

22
Q

What errors could occur when using a class A land pan

A
Splash caused by heavy rainfall
 drinking of birds
Wind movemement
Pan warming up faster than land
loss of heat from sides and bottom.
23
Q

potential evapotranspiration

A

equal to “the water loss which will occur if at no time there is a deficiency of water in the soil for the use of vegetation”
An upper limit to the amount of water an ecosystem will loose by evapotranspiration.

24
Q

When does the majority of evapotranspiration take place?

A

In the summer months

25
Q

Why could the actual evapotranspiration be less than the potential

A

If the soil water storage capacity is limited. In months when the potential evapotranspiration is less than the rainfall, some of the demand will be met by drawing upon moisture stored in the soil. When available soil water is depleted, the actual evapotranspiration will be limited to the monthly precipitation.

26
Q

Under what conditions would potential evapotranspiration be close to the actual evapotranspiration

A

If precipitation is constant throughout the year