Long-term changes in precipitation phase in Czechia

IF 0.9 4区 社会学 Q3 GEOGRAPHY Geografie-Sbornik CGS Pub Date : 2019-01-01 DOI:10.37040/geografie2019124010041
Martin Hynčica, R. Huth
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引用次数: 8

Abstract

Long-term changes in precipitation phase are investigated at ten stations in Czechia. Trends are calculated from 1983 to 2018 for the period between November and April. Daily SYNOP reports and daily precipitation totals are used at every station, where number and occurrence of specific codes in SYNOP report determine daily precipitation totals as solid, combined (which represents, to a large extent, category of mixed precipitation), or liquid. Thereafter, it is possible to calculate trends of all precipitation phases as well as the proportion of solid to total precipitation (S/P; in %). The average S/P trend over all Czech stations is significantly negative (−0.60%·year-1) and accompanied by a sharp decrease in solid precipitation (−1.66 mm·year-1) and an increase in combined precipitation (1.50 mm·year-1). Thus, our results show a ship of precipitation phase from solid to combined. Because of the dependence of S/P on air temperature, we suppose that the current S/P decline is a manifestation of rising air temperatures in the past decades.
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捷克降水阶段的长期变化
研究了捷克10个站点降水相位的长期变化。趋势是根据1983年至2018年11月至4月期间的数据计算的。每个站点使用每日SYNOP报告和每日降水总量,其中SYNOP报告中特定代码的数量和出现情况决定了每日降水总量为固体、组合(在很大程度上代表混合降水类别)或液体。此后,可以计算出所有降水阶段的趋势以及固体降水占总降水的比例(S/P;%)。捷克所有站点的平均S/P趋势显著为负(- 0.60%·年-1),并伴有固体降水的急剧减少(- 1.66 mm·年-1)和联合降水的急剧增加(1.50 mm·年-1)。因此,我们的结果显示了一个从固体到结合的沉淀相的船。由于S/P与气温的关系,我们认为当前S/P的下降是过去几十年气温上升的表现。
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来源期刊
Geografie-Sbornik CGS
Geografie-Sbornik CGS Social Sciences-Geography, Planning and Development
CiteScore
2.20
自引率
0.00%
发文量
12
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