首页> 外文会议>International symposium on atmospheric and ocean optics: atmospheric physics >Climate changes in the Southern Hemisphere subtropical jet stream during the second half of the ⅩⅩ century and at the beginning of the (ⅩⅪ) century
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Climate changes in the Southern Hemisphere subtropical jet stream during the second half of the ⅩⅩ century and at the beginning of the (ⅩⅪ) century

机译:在九世纪的下半年和(ⅹⅺ)世纪初期,气候变化在南半球亚热带射流

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Subtropical jet stream is a narrow stream of strong wind at 200-hPa level, characterized by large vertical and horizontal wind shift and one or more maxima speed, reaching values of 70-100 m/s. The subtropical jet stream is located on the border of the "warm" and "medium" temperature zones in the Southern Hemisphere. The average annual trend of wind speed of the Southern subtropical jet stream is significant and is equal -0.47±0.10 m/s per decade. The subtropical jet stream is shifting southward (0.87°S ±0.08°S per decade) in the Southern Hemisphere.
机译:亚热带射流流是200-HPA水平的窄风流,其特征在于垂直和水平的风移和一个或多个最大速度,达到70-100m / s的值。亚热带喷射流位于南半球的“温暖”和“中等”温度区的边界上。南部亚热带射流的平均风速的年平均趋势是显着的,平均值相等-0.47±0.10米/秒。亚热带喷射流在南半球向南移动(每十年0.87°S±0.08°S)。

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