Warming trend in northern East China Sea in recent four decades

doi:10.1007/s00343-009-9238-4

IOCAS-IR > 海洋环流与波动重点实验室

	Warming trend in northern East China Sea in recent four decades
	Tang Xiaohui 1,2,3; Wang Fan1,3 ; Chen Yongli 1,3; Li Mingkui 1,3; [email protected]
	2009-06-01
发表期刊	CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
卷号	27 期号:2 页码:185-191
文章类型	Article
摘要	Global warming has become a notable trend especially since an abrupt climate change in 1976. Response of the East China Sea (ECS) to the global warming trend, however, is not well understood because of sparse long-term observation. In this paper, hydrographic observation data of 1957-1996 are collected and reviewed to study climatological variability in northern ECS. Significant warming trends are found in both summer and winter. In summer, the average SST is about 0.46A degrees C higher during the period of 1977-1996 than that of 1957-1976, and the Taiwan Warm Current Water (TWCW) was strengthened. In winter, despite of the cooling effect in the coastal areas adjacent to the Changjiang (Yangtze) River Estuary (CRE), the average SST increase was about 0.53A degrees C during the same period. The causes of this SST warming up in summer are different from in winter. The warming trend and intensification of the TWCW in summer were primarily influenced by the strengthening of the Kuroshio transport, while the warming in winter was mainly induced by the variability of the climate system.; Global warming has become a notable trend especially since an abrupt climate change in 1976. Response of the East China Sea (ECS) to the global warming trend, however, is not well understood because of sparse long-term observation. In this paper, hydrographic observation data of 1957-1996 are collected and reviewed to study climatological variability in northern ECS. Significant warming trends are found in both summer and winter. In summer, the average SST is about 0.46A degrees C higher during the period of 1977-1996 than that of 1957-1976, and the Taiwan Warm Current Water (TWCW) was strengthened. In winter, despite of the cooling effect in the coastal areas adjacent to the Changjiang (Yangtze) River Estuary (CRE), the average SST increase was about 0.53A degrees C during the same period. The causes of this SST warming up in summer are different from in winter. The warming trend and intensification of the TWCW in summer were primarily influenced by the strengthening of the Kuroshio transport, while the warming in winter was mainly induced by the variability of the climate system.
关键词	Global Warming Climate Change East China Sea Sea Surface Temperature Long-term Variability
DOI	10.1007/s00343-009-9238-4
收录类别	SCI
语种	英语
WOS记录号	WOS:000267970300001
引用统计	被引频次：41[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.qdio.ac.cn/handle/337002/117
专题	海洋环流与波动重点实验室
通讯作者	[email protected]
作者单位	1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China 3.Chinese Acad Sci, Key Lab Ocean Circulat & Waves KLOCAW, Qingdao 266071, Peoples R China
第一作者单位	中国科学院海洋研究所; 海洋环流与波动重点实验室
推荐引用方式 GB/T 7714	Tang Xiaohui,Wang Fan,Chen Yongli,et al. Warming trend in northern East China Sea in recent four decades[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2009,27(2):185-191.
APA	Tang Xiaohui,Wang Fan,Chen Yongli,Li Mingkui,[email protected].(2009).Warming trend in northern East China Sea in recent four decades.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,27(2),185-191.
MLA	Tang Xiaohui,et al."Warming trend in northern East China Sea in recent four decades".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 27.2(2009):185-191.

条目包含的文件
文件名称/大小	文献类型	版本类型	开放类型	使用许可
Warming trend in nor（533KB）			限制开放	--	浏览