1950-2021年鄂霍次克海和日本海沿岸地区主要气温正异常形成特征

T. Shatilina, G. Tsitsiashvili, T. Radchenkova
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引用次数: 0

摘要

根据气象台网,考虑了1950-2021年鄂霍次克海和日本海沿岸地区的主要正气温异常。计算了1950-1979年和1980-2021年期间主要气温正异常发生次数和频率的年际变化。结果表明,1980-2021年各月份的异常发生频率明显高于1950-1979年。1980 ~ 2021年1 ~ 3月,鄂霍次克海北部异常次数最多。鄂霍次克海各站异常发生频率最高的月份为3月。位于日本海沿岸地区的台站呢?异常发生的最高频率显示在5月。结果表明,1950-1979年与1980-2021年的气候特征差异是由亚太地区大气活动中心环流型态的变化决定的。1980-2021年冬季,主要正异常的发生频率由亚洲东海岸附近的对流层通过区和鄂霍次克对流层气旋的位置决定,而1980-2021年暖期主要正异常的发生频率由亚洲低压区和夏威夷反气旋的环流区变率决定,其强度较1950-1979年有所增加。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Feature of the formation of major positive air temperature anomalies in the coastal areas of the Sea of Okhotsk and the Sea of Japan in 1950—2021
Major positive air temperature anomalies in the coastal areas of the Sea of Okhotsk and the Sea of Japan in 1950—2021 are considered according to the meteorological network. The intra annual variation in the number and frequency of occurrence of major positive air temperature anomalies in the periods 1950—1979 and 1980—2021 are calculated. It is shown that the frequency of occurrence of these anomalies in all months of the year in 1980—2021 is much higher than in 1950—1979. The maximum number of the anomalies was indicated through January to March of 1980—2021 in the northern part of the Sea of Okhotsk. The maximum frequency of occurrence of the anomalies was in March for all stations of the Sea of Okhotsk. What about the stations situated in the coastal areas of the Sea of Japan, the maximum frequency of occurrence of the anomalies was indicated in May. It is shown that the difference between the climatic peculiarities of 1950—1979 and 1980—2021 were determined by changes of the circulation regime in the centers of action of the Asia-Pacific region atmosphere. During winter periods of 1980—2021, the frequency of occurrence of major positive anomalies was determined by the tropospheric through regime near the eastern coast of Asia and by the position of the Okhotsk tropospheric cyclone while in warm periods of 1980—2021 it was determined by the circulation regime variability in the area of the Asia depression and of the Hawaiian anticyclone, their intensity being increased as compared to those of 1950—1979.
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