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Circulation conditions of abnormally cold winter of 2005-2006 over Siberia

机译:2005-2006年西伯利亚异常寒冷的冬季的循环条件

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摘要

This work is aimed at studying circulation conditions of the abnormally cold winter of 2005-2006 over Siberia where the intensification of meridian air exchange was accompanied by a frequent invasion of cold air masses into temperate latitudes and their precipitation in lower layers of troposphere. Stratospheric warming and long-term blocking processes in troposphere over Europe and Yakutia preceded the development of deep high-latitude cyclones over Siberia and the Urals. High-latitude convergence over Siberia was accompanied by a strong cyclonic wind shift and intensification of jet stream. On the whole, weakening of western transfer within the significant layer of atmosphere, decrease of a number of deep cyclones in the Western Arctic, as well as stratospheric warming create a high level of predictability of short-period climatic changes over Siberia in winter.
机译:这项工作的目的是研究2005-2006年西伯利亚异常寒冷的冬季的循环条件,在该条件下,子午空气交换加剧,冷空气团块频繁侵入温带地区,并在对流层低层降水。欧洲和雅库特对流层的平流层变暖和长期阻塞过程先于西伯利亚和乌拉尔上空深空高空气旋的形成。西伯利亚上空的高纬度辐合伴随着强烈的气旋风变迁和急流的加剧。总体而言,西风在大气的重要层内的转移减弱,西北极的深层气旋的减少以及平流层变暖为冬季西伯利亚的短期气候变化提供了较高的可预测性。

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