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Summary Of: Evapotranspiration

Evapotranspiration is an important part of the... that contributes to evapotranspiration can be called an... is a representation of the environmental demand for evapotranspiration and represents the evapotranspiration rate of a short green crop... Evapotranspiration is said to equal potential evapotranspiration when there is ample water... Evapotranspiration and the water cycle... Evapotranspiration and the water cycle... Evapotranspiration and the water cycle... Evapotranspiration is a significant water loss from a watershed... and will contribute almost nothing to evapotranspiration in the spring... Factors that affect evapotranspiration include the plant... actual evapotranspiration is usually no greater than... If potential evapotranspiration is greater than actual precipitation... Evapotranspiration can never be greater than PET... Evapotranspiration be measured or estimated using several methods... Evapotranspiration may be estimated by creating an equation of the water balance of a catchment... To convert the reference evapotranspiration to actual crop evapotranspiration... A third methodology to estimate the actual evapotranspiration is the use of the energy balance... be calculated and the energy available for actual evapotranspiration can be solved... The most direct method of measuring evapotranspiration is with the eddy covariance technique in which fast fluctuations of vertical wind speed are... Monthly estimated potential evapotranspiration and measured pan evaporation for two locations in Hawaii... Monthly estimated potential evapotranspiration and measured pan evaporation for two locations in Hawaii... Monthly estimated potential evapotranspiration and measured pan evaporation for two locations in... Potential evapotranspiration is usually measured indirectly... Often a value for the potential evapotranspiration is calculated at a nearby climate station on a reference surface... and can be converted to a potential evapotranspiration by multiplying with a surface coefficient... The difference between potential evapotranspiration and precipitation is used in...

Encyclodia Page On: Evapotranspiration

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Water cycle of the earth's surface, showing the individual components of transpiration and evaporation that make up evapotranspiration. Other closely related processes shown are runoff and groundwater recharge. | | runoff | groundwater recharge | evaporation | plant | transpiration | atmosphere | soil | canopy interception | waterbodies | plant | stomata | leaves | water cycle | energy | wind | atmosphere | herbaceous | woody | Conifer | deciduous | citation needed | dubious | discuss | solar radiation | humidity | temperature | wind | cloud forests | precipitation | percolation | water tables | capillary action | irrigation | Pan evaporation | groundwater recharge | Penman equation | Penman-Monteith | Food and Agriculture Organization | Blaney-Criddle equation | United States | scintillometer | Eddy covariance | Monthly estimated potential evapotranspiration and measured pan evaporation for two locations in Hawaii, Hilo and Pahala. | | Hawaii | water | summer | lakes | oceans | soil | vegetation | irrigation scheduling | aridity index | ISBN 92-5-104219-5 | 2007 | 10-08 | Hydrologic Evaluation of Landfill Performance | Soil plant atmosphere continuum | Categories | Hydrology | Climatology | Agronomy | Ecological processes | All articles with unsourced statements | Articles with unsourced statements since February 2007 | All pages needing cleanup | Articles with disputed statements from March 2008 |
This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Evapotranspiration".