全球陆地蒸发转化趋势最近有所下降,原因是水分供应有限
Martin Jung1, Markus Reichstein, Philippe Ciais
1Max Planck Institute for Biogeochemistry, 07745 Jena, Germany. mjung@bgc-jena.mpg.de
Nature
|October 12, 2010
概括
全球陆地蒸发转化量从1982年到1997年增加,然后在2008年停滞不前. 这一转变是由土壤水分的下降推动的,特别是在南半球,影响了全球的水循环.
科学领域:
- 地球系统科学 地球系统科学
- 气候科学 气候科学
- 水文学的水文学
背景情况:
- 蒸发转化 (ET) 是全球水循环的关键组成部分,影响气候和生态系统服务.
- 预计气候变化将加剧水文循环,改变全球的ET模式.
- 关于外星变化的直接全球观测数据是有限的,这阻碍了准确的气候变化评估.
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