| 地形及冷热源扰动不同分布对南沙海域西南大风形成过程影响的数值试验 |
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| 引用本文： | 张翔,周学群.地形及冷热源扰动不同分布对南沙海域西南大风形成过程影响的数值试验[J].应用气象学报,1995,6(2):163-170. |
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| 作者姓名： | 张翔 周学群 |
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| 作者单位： | 1.南海舰队气象区台 |
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| 摘 要： | 利用一个p-σ混合坐标五层原始方程模式，进行了地形及冷热源扰动的不同分布对南沙海域西南大风过程形成作用的数值试验。结果表明，亚洲南部特殊的地形及海陆分布是形成南沙海域西南大风过程的基本条件，但它造成的最大风速只能达8m/s，比观测值要小。试验中发现，在有地形作用的前提下，澳大利亚冷空气的向北爆发及菲律宾附近热源扰动的作用均可各自在南沙海域形成12m/s以上的大风过程，而孟加拉湾附近的热源扰动则对南沙海域西南大风过程的形成无明显作用。
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| 关 键 词： | 冷热源扰动 西南大风 数值试验 |
The Numerical Experiments of Southwesterly Formation over the Nansha Sea Area with the Effects of Terrain and Heat Perturbation |
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| Zhang Xiang,Zhou Xuequn.The Numerical Experiments of Southwesterly Formation over the Nansha Sea Area with the Effects of Terrain and Heat Perturbation[J].Quarterly Journal of Applied Meteorology,1995,6(2):163-170. |
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| Authors: | Zhang Xiang Zhou Xuequn |
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| Institution: | 1.(Meteorological Observatory of South China Sea Naval Fleet, Zhanjiang 524001) |
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| Abstract: | By using a five layer limited area primitive equations model, the terrain, heating perturbation over South Asia and a cooling perturbation over Australia are incorporated, respectively in the numerical model to discuss their effects on the southwesterly formation over the Nansha Sea area. The experiments of terrain show that the topographic effect is necessary on the southwesterly formation, but the topographic effect is not strong enough to make the southwest wind velocity reach 12 m/s. Furthermore, with the help of the effect of terrain, the experiment results including heating perturbation over the Philippines and the cooling perturbation over Australia, respectively, show that they can both make the southwesterly formation of above 12 m/s over the Nansha sea area. However, the heating perturbation over the Bay of Bengal has no effect on the formation of southwesterly over the Nansha Sea area |
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| Keywords: | Heating and cooling perturbation Southwesterly Numerical experiment |
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