On the Changing Snow Contribution to Runoff Across Turkiye

Furkan Yunus Emre Cevahi̇r, M. B. Duygu
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Abstract

Contribution of snowfall to runoff is especially important in snow-dominated regions where hydrological processes are mostly influenced by snowmelt. In this study, the contribution of snowfall to runoff in Turkey for the last 21 years was examined in the light of the observed data and hydrological model results globally provided by NASA. The snow dominant regions of Turkey for the last twenty-one years were revealed, and the ratio of the spatially averaged maximum snow water equivalent to runoff (Rsr) values, an indicator showing snowmelt contribution to runoff, were calculated for two separate periods (2000-2010, 2012-2022). These Rsr values were compared across Turkey to see if they are decreasing in snow-dominated regions. According to the results of the analysis, it was concluded that Rsr values are decreasing in all snow-dominated regions except Aras and Çoruh basins. Rsr values decreased by up to 50 percent in the last 11-year period in regions with high snowfall, such as the upper Euphrates basin.
关于变化的雪对土耳其径流的贡献
降雪对径流的贡献在积雪为主的地区尤为重要,因为这些地区的水文过程主要受融雪的影响。在本研究中,根据NASA提供的全球观测数据和水文模型结果,研究了土耳其过去21年降雪对径流的贡献。揭示了近21年来土耳其的积雪优势区,并计算了2000-2010年和2012-2022年两个不同时期的空间平均最大雪水当量与径流之比(Rsr)值,该指标反映了融雪对径流的贡献。这些Rsr值在土耳其各地进行了比较,看看它们是否在积雪覆盖的地区下降。分析结果表明,除阿拉斯区和Çoruh流域外,其余地区的Rsr值均呈下降趋势。在过去的11年里,在幼发拉底河上游等降雪量大的地区,Rsr值下降了50%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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