西苏台德地区的雪水当量及其在气候变化中的变化

IF 4.7 2区 地球科学 Q1 WATER RESOURCES
Grzegorz Urban
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引用次数: 0

摘要

研究地区西苏台德地区。研究重点本文描述了西苏台德地区雪水当量(SWE)的变化特征。雪水当量与研究地区的暴露程度和海拔高度有关。根据波兰和捷克共和国的 16 个测量站,对 1961-2020 年冬季(11 月至 4 月)的雪水当量进行了分析。所采用的通过简单回归方程估算 SWE(SWEi)的方法是一种良好且易于应用的气候 SWE 研究方法。该方法与实际 SWE 值的点平均差异范围为 3-29%。平均积雪深度及其 SWEi 在季节中逐渐增加,在二月或三月达到最大值,之后会明显减少。同时,积雪密度通常在四月份达到月平均最大值。季节性 SWEi 平均值和最大值呈现负值趋势,分别约为-0.1 至-1.3 厘米/十年和-0.2 至-2.5 厘米/十年。这在许多地点都有显著的统计学意义。在海拔相似的地点,南部宏观暴露站点的 SWEi 值要大于北部站点。在具有北部和南部宏观暴露的斜坡上,SWEi 随海拔变化的速率相似。SWEi 值的特点是与实际 SWE 值的差异呈正不对称。因此,实际 SWEi 值略低于估算值,雪盖对环境的贡献水量减少。这些结果与欧洲其他山区的结果一致,表明由于雪盖厚度和持续时间呈下降趋势,SWEi 值也在减少。这表明气候正在变暖,近几十年来尤为严重。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Snow water equivalent in the Western Sudetes and its changes in the light of a changing climate

Study region

The Western Sudetes.

Study focus

This paper characterises changes in snow water equivalent (SWE) in the Western Sudetes. SWE was linked to the exposure and altitude of the study area. The analysis was made for the winter seasons (November-April) 1961–2020, based on 16 measurement stations from Poland and the Czech Republic.

SWE is strongly positively correlated with snow depth (HS). The adopted method for estimating SWE (SWEi) by simple regression equations is a good and easily applicable method for climatological SWE studies. The method shows point average differences from actual SWE values in the range of 3–29 %. The overall average difference was 16.8 % and is comparable to the average difference for other mountain areas in Europe.

New hydrological insights for the region

The average snow depth and its SWEi gradually increase during the season, reaching maximum values in February or March, after which they decrease markedly. Meanwhile, snow density usually reaches an average monthly maximum in April. The mean and maximum seasonal SWEi values show negative trends, ranging from approximately −0.1 to −1.3 cm / decade and −0.2 to −2.5 cm / decade, respectively. These are statistically significant at many locations. SWEi values, at locations at similar altitudes, are greater at stations with a southern macro-exposure than a northern one. The rate of change of SWEi with altitude is similar on slopes with northern and southern macro-exposure. SWEi values are characterised by a positive asymmetry of differences with respect to the actual SWE. Hence, the actual SWE values are slightly smaller than the estimated values and the amount of water contributed to the environment by the snow cover decreases.

The results correspond with those from other mountainous areas in Europe, indicating decreasing SWE due to decreasing trends in snow cover thickness and duration. They are symptomatic of a warming climate, particularly intense in recent decades.

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来源期刊
Journal of Hydrology-Regional Studies
Journal of Hydrology-Regional Studies Earth and Planetary Sciences-Earth and Planetary Sciences (miscellaneous)
CiteScore
6.70
自引率
8.50%
发文量
284
审稿时长
60 days
期刊介绍: Journal of Hydrology: Regional Studies publishes original research papers enhancing the science of hydrology and aiming at region-specific problems, past and future conditions, analysis, review and solutions. The journal particularly welcomes research papers that deliver new insights into region-specific hydrological processes and responses to changing conditions, as well as contributions that incorporate interdisciplinarity and translational science.
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