Diurnal Water Content Changes in the Bare Soil of a Coastal Desert
The deposition of dew is a common meteorological phenomenon that has been recognized as an important ecosystem element, especially in arid areas. There is some evidence that indicates that there is an increase in the water content of the topsoil during nights in which no dew deposition was observed....
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Veröffentlicht in: | Journal of hydrometeorology 2004-10, Vol.5 (5), p.922-933 |
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Hauptverfasser: | , |
Format: | Artikel |
Sprache: | eng |
Online-Zugang: | Volltext |
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