The Spatiotemporal Patterns and Interrelationships of Snow Cover and Climate Change in Tianshan Mountains

To reveal the spatiotemporal patterns of the asymmetry in the Tianshan mountains' climatic warming, in this study, we analyzed climate and MODIS snow cover data (2001-2019). The change trends of asymmetrical warming, snow depth (SD), snow coverage percentage (SCP), snow cover days (SCD) and snow water equivalent (SWE) in the Tianshan mountains were quantitatively determined, and the influence of asymmetrical warming on the snow cover activity of the Tianshan mountains were discussed. The results showed that the nighttime warming rate (0.10 degrees C per decade) was greater than the daytime, and that the asymmetrical warming trend may accelerate in the future. The SCP of Tianshan mountain has reduced by 0.9%. This means that for each 0.1 degrees C increase in temperature, the area of snow cover will reduce by 5.9 km(2). About 60% of the region's daytime warming was positively related to SD and SWE, and about 48% of the region's nighttime warming was negatively related to SD and SWE. Temperature increases were concentrated mainly in the Pamir Plateau southwest of Tianshan at high altitudes and in the Turpan and Hami basins in the east. In the future, the western and eastern mountainous areas of the Tianshan will continue to show a warming trend, while the central mountainous areas of the Tianshan mountains will mainly show a cooling trend.

Automated summary

The analysis of the climatic warming in the Tianshan mountains showed a greater nighttime warming rate and a decrease in snow cover percentage. The asymmetrical warming trend has an impact on snow cover activity, which is expected to accelerate in the future.