极地研究 ›› 1990, Vol. 2 ›› Issue (1): 66-72.

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南极长城站潮汐观测与分析

孙洪亮   

  • 出版日期:1990-03-30 发布日期:1990-03-30

OBSERVATION AND ANALYSIS OF THE TIDE AT THE GREAT WALL STATION, ANTARCTICA

  • Online:1990-03-30 Published:1990-03-30

摘要:

从1987年1月5日开始,在南极长城站使用挪威安德拉公司生产的WLR—5型水位计对潮汐进行长期自动观测,取得60天,共8千多组数据。本文对这些实测资料进行了分析,初步得出南极长城站潮汐变化的一些基本特征。

关键词: 长城站;潮汐;半日潮波;水位

Abstract:

The long-term automotive observation of the tide has been carried out at the Great Wall Station in the Antarctica since 5 January 1987 with the Aanderaa tide gauge (Model WLR-5). The data covered 60 days and the 8000 groups of records were obtained. In this paper, the observation is described and the data analysed. The resultes are as follows. 1. The tide at the Great Wall Station is an irregular semidiurnal tide. Its daily inequality is quite remarkable, and mainly the inequality of the low tide. 2. During the observed period, the highest and the lowest water levels were respec-tivelly 4.222 m and 1.714 m, higher and lower than the mean water level by about 1 m and 1.5 m respectivelly. The variation range of the water level is 2.5 m. 3. During the observation time, the mean, the maximum and the possible maximum tidal ranges were 1.501 m, 2.242 m and 2.944 m, respectivelly. 4. The difference between the mean tropic high and low water intervals was about 8 hours, and high low water intervals was about 4 hours, which emerged inequality of the flood durations and of the ebb durations. The difference between the mean equinoctial high and low water intervals was about 6 hours, which displays the feature of a semi-diurnal tide.