1981-2020 年斯洛伐克塔特拉山地区部分雪盖特征的变化和趋势

Lenka Balážovičová, Cyril Siman, Katarína Mikulová
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引用次数: 0

摘要

据报道,在过去几十年里,欧洲的雪季越来越短,雪量越来越少。不过,在一些海拔较高的站点,发现积雪量在增加。斯洛伐克高山地区的情况也是如此,与积雪有关的一些研究显示,海拔高度会造成一些差异。在本研究中,我们报告了部分雪盖特征的变化趋势,如雪深 1 厘米、10 厘米和 20 厘米的雪盖天数 (DSC)、雪深总和 (SSD) 和平均雪深 (MSD)。本研究使用的数据由斯洛伐克水文气象研究所(SHMI)于 1981-2020 年的 39 个季节(01/07 至次年 30/06)在塔特拉山区的 8 个站点收集。在海拔 1100 米以上的站点观察到一些上升趋势,而海拔 1100 米以下的站点的估计值则普遍下降。1 厘米的 DSC 为 297 天,海拔 2635 米的站点为 297 天,海拔 640 米的站点为 25 天。除了全球变暖之外,其他因素也在起作用,而且这些因素在山区可能很复杂,使得任何趋势的解释都更加模糊。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Variability and trends of selected snow cover characteristics in the Tatra Mountains region in Slovakia 1981–2020
Over the last decades, snow seasons in Europe were reported to become shorter with lower abundance of snow. However, at some stations situated above certain elevation, the amount of snow cover was found to be increasing. This is also the case of high mountains in Slovakia, where number of snow-related studies showed some differences related to the elevation. In this study we report on the trends of selected snow cover characteristics such as the number of days with snow cover (DSC) for 1, 10 and 20 cm depths, summed snow depths (SSD) and mean snow depths (MSD). The data used in this study were collected by the Slovak Hydrometeorological Institute (SHMI) at eight stations in the Tatra Mountains region during the 39 seasons 1981–2020 (01/07 to 30/06 the following year). Some increasing trends were observed for stations above 1100 m while stations below this elevation had generally decreasing estimates. The DSC for 1 cm ranged from 297 days at station elevated at 2635 m a.s.l. to 25 days for station at 640 m a.s.l. The MSD ranged from 100 to 7 cm on average for the whole period. Apart from global warming, other factors play role, and these can be complex in the mountainous regions making any trends more ambiguous to interpret.
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