| 31. | Precipitation is well in excess of potential evapotranspiration, except for about a month in midsummer.
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| 32. | These trees still contribute to evapotranspiration, but often collect more water than they evaporate or transpire.
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| 33. | The average annual precipitation is about 635 mm, while annual potential evapotranspiration is about 1623 mm.
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| 34. | Evapotranspiration is the combination of water loss through atmospheric evaporation and through the life processes of plants.
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| 35. | In hydrology, evaporation and transpiration ( which involves evaporation within plant stomata ) are collectively termed evapotranspiration.
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| 36. | As such, virtually all rainfall occurring within this area must be removed through either evapotranspiration or pumping.
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| 37. | Where PET is the potential evapotranspiration and P is the average annual precipitation ( UNEP, 1992 ).
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| 38. | Trees have adapted to the dry climate by shedding leaves in the dry winter season to limit evapotranspiration.
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| 39. | Potential evapotranspiration supplements the measurement of precipitation in providing a scientific measurement-based definition of a desert.
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| 40. | Land use areas are delineated as a time series, with corresponding evapotranspiration rates and water management parameters.
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