作者: Benjamin R. Lintner , Pierre Gentine , Kirsten L. Findell , Fabio D’Andrea , Adam H. Sobel
DOI: 10.1175/JCLI-D-11-00561.1
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摘要: AbstractA process-based, semianalytic prototype model for understanding large-scale land–atmosphere coupling is developed here. The metric quantifying the sensitivity of precipitation P to soil moisture W, . For a range parameters typical conditions found over tropical or summertime continents, measure exhibits broad minimum at intermediate values. This attributed trade-off between evaporation (or evapotranspiration) E and convergence across states. water-limited, low conditions, dominated by evaporative , reflecting high potential Ep arising from relatively warm surface moisture-deficient atmospheric column under dry conditions. By contrast, energy limited) becomes slightly negative as decreases. However, because increase strongly wi...