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| 本文在前人工作的基础上,通过对30年(1954—1984年)以来水文资料的分析,找出东海黑潮的变异与青岛的降水及其与日本以南黑潮出现大弯曲之间的关系,得到了一些有意义的结果。 |
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| RELATIONSHIP OF VARIATION OF AXIAL POSITION OF THE KUROSHIO IN THE EAST CHINA SEA AND ITS MEANDERS SOUTH OF JAPAN WITH THE PRECIPITATION IN QINGDAO |
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| Abstract: |
| The characteristics of the variation of axial position of the Kuroshio in the East China Sea and its relationship to the meanders south of Japan ate analysed, based on the JMA’s temperature and GEK data (1954-1984) and the precipitation data (1900-1985) published by the Central Bureau of Meteorology of China. Some main results are as follows: 1. The axial position of the Kuroshio in the East China Sea is quite stable, its average deviation is about 9 n mile. 2. The mean distance of the seasonal variation of the axis is 8, 9 and 1-0 n miles in spring, summer and winter, and autumn, respectively. 3. When anticyclonic wind occurred in northwest of the Iriomote-jima and Tokara-kaikyo after 1-2 years, the meanders south of Japan will appear. 4. When the axial position of the Kuroshio in the East China Sea shifted to the southeast (northwest) the velocity and volume transport increases (decreases), but the precipitation in Qingdao decreases (increases), the meanders south of Japan will appear (disappear). Add, when the minimum (maximum) precipitation occurred in Qingdao, the meanders south of Japan will appear (disappear). |
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