Warming trend in northern East China Sea in recent four decades
文献类型：期刊论文
| 作者 | Tang Xiaohui1,2,3; Wang Fan1,3 ; Chen Yongli1,3; Li Mingkui1,3; fwang@ms.qdio.ac.cn
|
| 刊名 | CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
 |
| 出版日期 | 2009-06-01 |
| 卷号 | 27期号:2页码:185-191 |
| 关键词 | Global Warming Climate Change East China Sea Sea Surface Temperature Long-term Variability |
| DOI | 10.1007/s00343-009-9238-4 |
| 文献子类 | Article |
| 英文摘要 | 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. |
| 语种 | 英语 |
| WOS记录号 | WOS:000267970300001 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/118]  |
| 专题 | 海洋研究所_海洋环流与波动重点实验室 |
| 通讯作者 | fwang@ms.qdio.ac.cn |
| 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 |
| 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,&fwang@ms.qdio.ac.cn.(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. |
入库方式： OAI收割
来源：海洋研究所
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