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UNIT 08 The WATER CYCLE and CLIMATES

REVIEW for VOCABULARY

AB
evapotranspirationthe combination of evaporation and transpiration
condensationthe change of water vapor into (liquid or solid) clouds
precipitationany form of water falling from the sky and reaching the earth
runoffin the water budget, SURPLUS water that cannot infiltrate into the soil
capillaritythe ability of soil to draw water upward into tiny pore spaces
zone of aerationthe portion of the soil above the water table in which the interconnected pores are filled with air
zone of saturationthe portion of the soil below the water table in which the pores are filled with ground water
regoliththe loose material (soil) at the earth surface
permeabilitythe ability of a soil to allow water to pass thru it
porositythe percentage of empty space within the soil
water retentionwater which stays (is retained) in the zone of aeration as capillary water
water tablethe top of the zone of saturation
infiltrationwater seeping into the ground
ground waterwater that infiltrates the ground, moves into zone of saturation
moisture usagewater from storage that is used for evapotranspiration occurring when P is less than PE and St>0
moisture rechargewithin the water budget: infiltrating water that enters storage occurring when P>PE and St<100
moisture surpluswithin the water budget: extra water that becomes runoff occurring when P>PE and St=100 (maximum)
moisture deficitwithin the water budget: shortage of water occurring when P is less than PE and St=0
climatethe condition of the atmosphere over a long period of time
continental climateclimate with cooler winters and warmer summers (larger yearly temperature variations)
marine climateclimate with cooler summers and warmer winters (smaller yearly temperature variations)
arid climateclimate with a P/PE ratio less than 0.4
semiarid climateclimate with a P/PE ratio of 0.4 to 0.8
subhumid climateclimate with a P/PE ratio of 0.8 to 1.2
humid climateclimate with a P/PE ratio greater than 1.2

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