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Abstract
A land-process scheme has been incorporated in a vertical one-dimensional time-dependent atmospheric model and numerical experiments have been performed with the coupled model to examine influences of soil wetness and vegetation on climate changes associated to thermal forcing.It is showed that response of land-surface temperature to the thermal forcing becomes small with increase of soil water content and vegetation cover.Furthermore,the response is more obvious in arid climate region than in humid one.The result also shows that there exist two patterns of corresponding relation between variations in air temperature and humidity on the land surface in response to hydrologic and thermal focing.
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Citation
Liu Yongqiang, Ye Duzheng, Ji Jinjun. 1992: INFLUENCE OF SOIL MOISTURE AND VEGETATION ON CLIMATE CHANGES INDUCED BY THERMAL FORCING*. Journal of Meteorological Research, 6(1): 58-69.
Liu Yongqiang, Ye Duzheng, Ji Jinjun. 1992: INFLUENCE OF SOIL MOISTURE AND VEGETATION ON CLIMATE CHANGES INDUCED BY THERMAL FORCING*. Journal of Meteorological Research, 6(1): 58-69.
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Liu Yongqiang, Ye Duzheng, Ji Jinjun. 1992: INFLUENCE OF SOIL MOISTURE AND VEGETATION ON CLIMATE CHANGES INDUCED BY THERMAL FORCING*. Journal of Meteorological Research, 6(1): 58-69.
Liu Yongqiang, Ye Duzheng, Ji Jinjun. 1992: INFLUENCE OF SOIL MOISTURE AND VEGETATION ON CLIMATE CHANGES INDUCED BY THERMAL FORCING*. Journal of Meteorological Research, 6(1): 58-69.
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