西太平洋副热带高压的年代际变化 及其气候影响
收稿日期: 2001-07-10
修回日期: 2001-10-10
网络出版日期: 2002-03-25
基金资助
国家重点基础研究发展规划项目(G1998040900)和国家自然科学基金项目(40105007)
Interdecadal Change in Western Pacific Subtropical High and Climatic Effects
Received date: 2001-07-10
Revised date: 2001-10-10
Online published: 2002-03-25
Supported by
National Key Project for Basic Research, No.G1998040900; National Natural Science Foundation of China, No.40105007
龚道溢,何学兆 . 西太平洋副热带高压的年代际变化 及其气候影响[J]. 地理学报, 2002 , 57(2) : 185 -193 . DOI: 10.11821/xb200202008
Western North Pacific Subtropical High is a very important atmospheric circulation system influencing the summer climate over eastern China. Its interdecadal change is analyzed in this study. There is a significant decadal shift in about 1979/1980. Since 1980, the Western North Pacific Subtropical High has enlarged, intensified, and shifted southwestward. This change gives rise to an anti-cyclonic circulation anomaly over the region from the South China Sea to Western Pacific and thus causes wet anomalies over the Yangtze River valley. During the summers of 1980-1999, the precipitation is 63.9 mm above normal, while during 1958-1979 it is 27.3 mm below normal. The difference is significant at the 99% confidence level as a t - test shown. The southwestward expanding of the Western North Pacific Subtropical High also leads to a significant warming in the southern China, during the 1980-1999 the summer mean temperature is 0.37oC warmer than that of the period 1958-1979. The strong warming is primarily due to the clearer skies associated with the stronger downward air motion as the Western North Pacific Subtropical High expanding to the west. It is also found that the relative percentage of tropical cyclones in the regions south of 20oN has been decreasing since the 1980s, but that in the regions north of 20oN has been increasing during the same period. The Western North Pacific Subtropical High responds significantly to sea surface temperature of the tropical eastern Pacific with a lag of one-two seasons and simultaneously to sea surface temperature of the tropical Indian Ocean. The changes in the sea surface temperatures are mainly responsible for the interdecadal variability of the Western North Pacific Subtropical High.
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