ロード中...
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...
保存先:
主要な著者: | , , |
---|---|
フォーマット: | Artigo |
言語: | Inglês |
出版事項: |
Wiley
2011-11-01
|
シリーズ: | Vadose Zone Journal |
オンライン・アクセス: | https://doi.org/10.2136/vzj2011.0014 |
タグ: |
タグ追加
タグなし, このレコードへの初めてのタグを付けませんか!
|