| 摘要: |
| 本文讨论准地转ω—方程在中低纬地区的应用问题,认为考虑了潜热加热的湿ω—方程可以比干ω—方程更好地反映大尺度垂直运动的概况。在湿ω—方程中,同时考虑三维平流的加热作用比只考虑垂直平流的加热作用效果好,尤其能较好地确定出与降水有关联的较强的上升和下沉运动的区域和量值。 |
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| THE ROLE OF RELEASED LATENT HEAT IN VERTICAL MOTION OF THE ω-EQUATION |
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Gao Shaofeng1, M. A. Pedder2
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1.Zhongshan University;2.University of Reading, U. K.
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| Abstract: |
| The application of the quasi-geostrophic ω-equation to mid-lower latitudes is discussed. Its wet version, when warmed with latent heat, better describes the reality, with 3-d ad-vection heating, it performs better than only with horizontal heating. |
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