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冬季东海黑潮海-气热量交换对长江中下游汛期降水的影响
THE INFLUENCE OF THE SEA—AIR HEAT EXCHANGE OVER THE KUROSHIO IN THE EAST CHINA SEA IN WINTER ON THE PRECIPITATION IN THE MIDDLE AND LOWER REACHES OF CHANGJIANG RIVER IN FLOOD SEASON
【摘要】 <正> 黑潮海区的海-气热量交换,表层水温及热含量的变异对大气环流和大陆旱涝的影响已有论述。本文的目的在于分析东海黑潮海区的海-气热量交换特征及其与整个黑潮的关系,探讨它与长江中下游降水的联系,进而计算比较东海嵊山站多年海-气热量交换的特性,得到了有预报意义的指标。一、东海黑潮冬季海-气热量交换的年际变化特性及其与整个黑潮的关系作者在分析东海黑潮海区的海-气热量收支的年平均状况和季节变化特征时指出,10—3月海-气之间的热量比较显著,特别是在严冬季节。据此,本文只着重讨论东海黑
【Abstract】 In this paper, the sea-air heat exchange over the Kuroshio in the East China Sea during the winters of 1954—1972 was computed and analysed. The results indicate that the year to year anomalies of sea-air heat exchange is obvious and the values are mainly controlled by the intensity of the cold air at the same time. The authors have found a close relationship between sea-air heat exchange and precipitation in the region of the Changjiang River during the early summer. Finally, the predicting indication for forcasting this precipatation around the middle and lower reaches of Changjiang River in June has been given.
- 【文献出处】 海洋与湖沼 ,Oceanologia Et Limnologia Sinica , 编辑部邮箱 ,1983年03期
- 【被引频次】26
- 【下载频次】107