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Spatio-temporal changes in atmospheric precipitation over south-western Poland between the periods 1891-1930 and 1981-2010

机译:1891-1930年至1981-2010年期间波兰西南部大气降水的时空变化

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摘要

In this paper, we quantify the changes in precipitation distribution in south-western Poland between the periods 1891-1930 and 1981-2010. The average monthly precipitation totals available for 368 and 245 stations, respectively, are spatially interpolated and processed to calculate maps of differences and pluvial continentality indices for both periods. The maps are analysed against changes in atmospheric circulation and take into account the potential role of the mountain barrier of the Sudetes. The main findings are (1) winter totals generally increased in conjunction with a higher frequency of zonal circulation; it is more pronounced in the upper parts of the Sudetes due to orographic effects; (2) a decreased frequency of zonal circulation together with an increased frequency of southern flows has likely led to the reduction of precipitation in spring and autumn. These changes have led to a significant modification of the region's pluvial regime, mostly by decreasing continentality features (especially in the Sudetes and the western lowlands). In addition, the strong sheltering influence of the mountain barrier is observed, driving the preservation or even the enhancement of the continental pluvial characteristics in the north-eastern to eastern foregrounds of the Sudetes. This leads to the conclusion that in areas where long-term observed trends or future projections of precipitation are ambiguous, there may occur significant modifications in regional characteristics, especially as a result of changes in atmospheric circulation modified by local orography.
机译:在本文中,我们量化了1891-1930年至1981-2010年期间波兰西南部降水的分布变化。分别对368个和245个台站的平均月降水总量进行空间插值和处理,以计算两个时期的差异图和冲积洲指数。对地图进行了分析,以应对大气环流的变化,并考虑到了Sudetes山脉障碍的潜在作用。主要发现是:(1)冬季总数总体上随区域循环频率的增加而增加;由于地形的影响,它在苏德特人的上部更为明显; (2)地带环流频率的降低以及南方水流的频率增加可能导致了春季和秋季降水的减少。这些变化导致了该地区的河流域统治格局发生了重大变化,主要是通过减少了大陆性特征(尤其是在苏德特人和西部低地地区)。此外,还观察到了山壁屏障的强大遮挡作用,从而推动了苏德特山脉东北至东部前景中大陆性河流特征的保存甚至增强。得出的结论是,在长期观测到的降水趋势或未来的预测不明确的地区,区域特征可能会发生重大变化,特别是由于当地地形改变了大气环流的结果。

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  • 来源
    《Theoretical and applied climatology》 |2019年第2期|505-518|共14页
  • 作者单位

    Univ Wroclaw, Inst Geog & Reg Dev, Pl Uniwersytecki 1, PL-50137 Wroclaw, Poland;

    Univ Wroclaw, Inst Geog & Reg Dev, Pl Uniwersytecki 1, PL-50137 Wroclaw, Poland;

    Sch Complex 2 Krotoszyn,Pl Szkolny 19, PL-63700 Krotoszyn, Poland;

    Univ Wroclaw, Inst Geog & Reg Dev, Pl Uniwersytecki 1, PL-50137 Wroclaw, Poland;

    Univ Wroclaw, Inst Geog & Reg Dev, Pl Uniwersytecki 1, PL-50137 Wroclaw, Poland;

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