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机构地区:[1]山东省气象科学研究所,山东济南250031 [2]山东省气象台,山东济南250031 [3]山东省气候中心,山东济南250031
出 处:《热带气象学报》2008年第3期273-278,共6页Journal of Tropical Meteorology
基 金:山东省气象局重点课题(2006sdqxz04)“山东省气象预警预报业务平台研究”;山东省科技厅攻关项目(2004GG2208142)“山东省短期集合数值预报系统的研究”共同资助
摘 要:利用1979~2006年月平均OLR、850hPa、200hPa风场等资料,分析了山东4月降水异常年的前期秋、冬季热带地区对流活动特征,发现前冬12月的热带西太平洋地区对流活动异常与山东4月降水的关系最为密切,进一步分析其与东亚大气环流关系,结果表明西太平洋暖池上空的对流活动异常与冬春季东亚大槽、东亚局地的Hadley环流以及Walker环流的强弱紧密相连,且对流活动强(弱)年相伴随的东亚大气环流异常特征恰与山东4月降水异常少(多)年的特征相吻合,因此,12月热带西太平洋对流活动强弱可作为山东4月降水预测的一条重要依据。Using OLR and 850 hPa and 200 hPa wind fields data(1979-2006),the characteristics of previous convection over the tropical area in Autumn and Winter of April precipitation anomaly in Shandong are diagnosed. The main conclusions are as follows. Previous convection anomaly over the Western Pacific Warm Pool in December has close relationship with the April precipitation in Shandong. Further analysis of the relationship of convection with the general circulation over the East Asia shows that the convection anomaly over the Western Pacific Warm Pool has close relationship with the East Asian Trough, the Hadley cell over East Asia and the Walker cell. The characteristics of East Asian atmospheric circulation accompanied by stronger(weaker) convection are identical to that accompanied by less(more) April precipitation in Shandong. Therefore, the convection anomaly over the tropics in December may be an important basis for April precipitation in Shandong.
分 类 号:P434.4[天文地球—大气科学及气象学]
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