【摘要】 <正> 一、前 言 海雾是海上的重要危险性天气之一.国内外关于海雾生消机制、气侯特征及短期预报方面研究成果甚多,而中期分析及预报方面的研究甚少,这是海洋气象中值得探索的课题.作者曾分析了黄海北部海区春季海雾过程生消、持续规律,指出海雾与中期环流形势演变及南支槽活动有密切关系.本文在上述工作基础上,利用1962-1973年4、更多还原

【Abstract】 The article is analysed the formation, dissipation and persistence regularities of the spring sea fog over the middle arid northern Huanghai Sea areas according to data observed during 1962-1973 years. The authors are of the opinion that two short wave troughes located in the middle and lower latitudes transmit eastward, and often add each other under the particular large scale circulation back-ground, thus we can find that westly trough in the lower latitude develops and moves by north. During the eastward movement of the short wave shoughes the southwest air current in the front of the troughs continuously brings warm and wet air over the southeastern Xizang Plateau to the northeast direction and this is an important condition for the formation and development of sea fog. We have constructed relation between activities of the upper cut-off cold eddy (in the Caspian Sea-Aral Sea or the northern Indian ocean), the blocked high pressure (in the northern Atlantic Ocean the Ural areas)and activities of the short wave trough,finally also given out mid-range sea fog forecasting method in dtail.更多还原