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首页> 外文期刊>TAO: Terrastrial, atmospheric, and oceanic sciences >Toward a multi-decadal climatology of north pacific polar lows employing dynamical downscaling
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Toward a multi-decadal climatology of north pacific polar lows employing dynamical downscaling

机译:利用动态降尺度对北太平洋极地低压进行多年代气候研究

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摘要

The North Pacific is an area where sub-synoptic Polar Lows frequently form during the cold season, especially over the Bering Sea, Gulf of Alaska and Japan Sea. So far, a multi-decadal climatology of such Polar Lows based on individual cases has not been assembled. Here, we consider dynamical downscaling method for realistically constructing the formation and life cycles of such lows over the past 6 decades without exploiting sub-synoptic information in initial fields. To do so, a regional climate model is conditioned by large-scale information of NCEP re-analyses. We test the approach by examining its skill in simulating ten known cases of North Pacific Polar Lows. Three of these are discussed in some detail. The signatures of all storms emerge in the simulations with additional sub-synoptic details. The tracks of the simulated Polar Lows closely follow the tracks derived from satellite imagery. We conclude that the suggested method is suitable for constructing multi-decade climatologies, including trends and variability, of Polar Lows in the North Pacific by dynamically downscaling NCEP re-analyses.
机译:北太平洋是寒冷季节经常形成亚天气异常的低气压的区域,特别是在白令海,阿拉斯加湾和日本海上空。到目前为止,还没有建立基于个别情况的极地低潮的多年代气候学。在这里,我们考虑采用动态降尺度方法来现实地构建过去6年中这种低谷的形成和生命周期,而无需在初始领域中利用亚天气信息。为此,要以NCEP重新分析的大规模信息为条件建立区域气候模型。我们通过检查其模拟北太平洋极地低点的十个已知案例的技巧来测试该方法。其中三个进行了详细讨论。所有风暴的特征都带有附加的亚天气细节出现在模拟中。模拟的极地低地的轨迹紧随卫星图像得出的轨迹。我们得出结论,建议的方法适用于通过动态缩减NCEP重新分析来构造北太平洋极地低压的数十年气候,包括趋势和变异性。

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