Vertical influence of temperature and precipitation on snow cover variability in the Yarlung Zangbo River basin, China

• Published in: International journal of climatology Vol. 41; no. 2; pp. 1148 - 1161
• Main Authors: Ban, Chunguang, Xu, Zongxue, Zuo, Depeng, Liu, Xiaowan, Zhang, Rui, Wang, Jing
• Format: Journal Article
• Language: English
• Published: Chichester, UK John Wiley & Sons, Ltd 01.02.2021; Wiley Subscription Services, Inc
• Subjects: Altitude; CHIRPS; Climate change; Climate control; Correlation analysis; Elevation; Future climates; Global warming; High altitude; Hydrologic data; Mountainous areas; Northern Hemisphere; Precipitation; Precipitation-temperature relationships; Regions; Remote sensing; River basins; Rivers; Snow; Snow cover; temperature; threshold elevation; Variability; Water resources; Yarlung Zangbo River; Yarlung Zangbo River
• ISSN: 0899-8418; 1097-0088
• DOI: 10.1002/joc.6776

Seasonal snow cover in mountainous areas is a key source of water for downstream regions. The snow cover area (SCA) in the Northern Hemisphere has significantly decreased during the past decades in response to global warming. Therefore, it is necessary to investigate the primary factors controlling the spatiotemporal variabilities in the SCA in high altitude regions. In this study, based on remote sensing data of SCA, temperature, and precipitation in the Yarlung Zangbo River basin, Pearson's correlation analysis was used to identify the relative importance of temperature and precipitation on the SCA variability with altitude. The results showed that temperature played a more dominant role for the SCA than precipitation at all elevation during the period 2001–2017; three threshold altitudes at high, moderate, and low elevation were identified, and these threshold altitudes are dynamic and vary with time; the threshold altitude at high elevation was 5,925 ± 125 m, below which temperature (precipitation) was negatively (positively) correlated and above which temperature (precipitation) was positively (negatively) correlated with the SCA; the threshold altitude at moderate elevation was 3,200 ± 300 m, below which temperature (precipitation) was positively (negatively) correlated and above which temperature (precipitation) was negatively (positively) correlated with the SCA; the threshold altitude in low elevation regions was 2,100 ± 200 m. This study sheds light on the dominant climatic control factors on the variability in SCA in high altitude regions. These results have major implications for SCA and water resources availability under future climate change. The boundary, river network, meteorological stations in the Yarlung Zangbo River basin.