Warming trend in northern East China Sea in recent four decades

Xiaohui Tang; Fan Wang; Yongli Chen; Mingkui Li

doi:10.1007/s00343-009-9238-4

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Warming trend in northern East China Sea in recent four decades

Updated：2023-05-16

- Warming trend in northern East China Sea in recent four decades
- Journal of Oceanology and Limnology Vol. 27, Issue 2, Pages: 185-191(2009)
- Affiliations：
  
  1. Institute of Oceanology Chinese Academy of Sciences
  2. Graduate School of Chinese Academy of Sciences
  3. Key Laboratory of Ocean Circulation and Waves (KLOCAW) Chinese Academy of Sciences
- Author bio：
- Funds：
- DOI：10.1007/s00343-009-9238-4
  CLC：
- Online First：12 July 2009，
  
  Published：2009
- Accepted：
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Tang, X., Wang, F., Chen, Y. et al. Warming trend in northern East China Sea in recent four decades., Chin. J. Ocean. Limnol. 27, 185–191 (2009). https://doi.org/10.1007/s00343-009-9238-4
DOI：

Tang, X., Wang, F., Chen, Y. et al. Warming trend in northern East China Sea in recent four decades., Chin. J. Ocean. Limnol. 27, 185–191 (2009). https://doi.org/10.1007/s00343-009-9238-4 DOI：

摘要

Abstract

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 0.46°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 0.53°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.

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Keywords

references

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