The role of dew in the water and heat balance of bare loess soil in the Negev Desert: quantifying the actual dew deposition on the soil surface
During nighttime, latent heat fluxes to or from the soil surface are usually very small and the absolute amounts of dew deposition are accordingly very small. The detection of such small fluxes poses serious measurement difficulties. Various methods for measuring dew have been described in the liter...
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Veröffentlicht in: | Atmospheric research 2002-09, Vol.64 (1), p.323-334 |
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Sprache: | eng |
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