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Environmental Science

chapter 7

Terms

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Relative humidity
amount of water vapor as a percentage of what the air can hold at a particular
Infiltration
when precipitation is soaked into groundwater
Global Convection currents
sun heats earth over equator- air rises
Capillary water
held in soil- returns via evaporation or transpiration
Runoff
when flows into streams and rivers
Humidity
amount of water vapor in the air
Precipitation pattern
depends on rising or falling air currents
Nonrenewable groundwater
when recharge rate is centuries or more
Condensation
When water molecules become liquid again
Surface runoff loop
water becomes part of surface water system
Green water
watervapor
Rain Shadow
Moisture filled air meets mountains
Land subsidence
water filled spaces in ground lose their water
Sinkholes
underground cavern
Developing
water is untreated to downstream people are left with contaminated water
renewable groundwater
replenished by percolation of precipitation water
Purification
as percolates, removes bacteria and debris, may dissolve and leach minerals
Evapotranspiration loop
water evaporates and returns by precipitation
Aquifer exploitation
ground water use exceeds aquifer
Surface waters
all ponds, lakes, streams, rivers on earth
Nonconsumptive
water remains available to humans for other users
Consumptive
water does not return to other water resource
Recharge
area where water enters an aquifer
Blue water
liquid water
groundwater loop
water perlocates and moves through
Watershed
all land area that contributes to a particular stream or water

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