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Long‐Term Soil Water Trends across a 1000‐m Elevation Gradient

There is a general consensus among climate models that the direct influence of increasing temperature on evaporative demand will result in drier soils, reduced water supply, and more frequent drought conditions. The data available to evaluate long‐term soil water trends that may result from climate...

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Bibliographic Details
Main Authors: Mark Seyfried, David Chandler, Danny Marks
Format: Artigo
Language:Inglês
Published: Wiley 2011-11-01
Series:Vadose Zone Journal
Online Access:https://doi.org/10.2136/vzj2011.0014
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