陈隆勋,刘洪庆,王文,王予辉,山崎信雄. 1999. 南海及其邻近地区夏季风爆发的特征及其机制的初步研究[J]. 气象学报, 57(1):16-29, doi:10.11676/qxxb1999.002
南海及其邻近地区夏季风爆发的特征及其机制的初步研究
PRELIMINARY STUDY ON THE CHARACTERISTICS AND MECHANISM OF SUMMER MONSOON ONSET OVER SOUTH CHINA SEA AND REGION ADJACENT TO IT
投稿时间:1997-03-19  修订日期:1997-06-25
DOI:10.11676/qxxb1999.002
中文关键词:  南海夏季风爆发  海温异常  高原热状况  海陆温差
英文关键词:Summer monsoon onset over South China Sea  Sea temperature anomaly Thermal regime over  Tibetan Plateau  Temperature difference between land and sea
基金项目:国家自然科学基金会49375245项目;“中日亚洲季风机制合作研究”项目
作者单位
陈隆勋 中国气象科学研究院, 北京, 100081 
刘洪庆 中国气象科学研究院, 北京, 100081 
王文 中国气象科学研究院, 北京, 100081 
王予辉 中国气象科学研究院, 北京, 100081 
山崎信雄 气象研究所, 筑波, 日本 
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中文摘要:
      利用OLR和TBB资料,提出一个指标,确定了1975~1993年间南海夏季风爆发日期,发现与风向转变的日期比较一致。在此基础上,讨论了南海夏季风爆发的过程。随后,还讨论了南海夏季风爆发与海温异常、高原热状况和海陆温差变化的关系,发现它与4月份南海、东太平洋赤道以及30~40°NSSTA有关,与海陆温差由冬季的冷陆暖海转变到热陆冷海有关。
英文摘要:
      Employing OLR and TBB data,we presented an index and decided the date of summer monsoon onset over South China Sea(SCS) during the period from 1975-1993, which is consistent with the date ofrecurvature of wind.On the basis of this,we discussed the pro cesses of summer monsoon over SCS.Furthermore,the relationship between summer monsoo nonsetover SCS and sea temperature anomaly,thermal regime over Tibetan Plateau as wellas variation of temperature difference between land and sea was discussed.we found it relates to SSTA in SCS,equatorial east Pacific and region between 30-40°N in Apriland it relates to changing of temperature difference land and sea from status of cool land and warm sea into status of warm land and cool sea in winter.
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