CollectHomepage AdvertisementContact usMessage

Arid Land Geography ›› 2025, Vol. 48 ›› Issue (10): 1760-1770.doi: 10.12118/j.issn.1000-6060.2024.776

• Climatology and Hydrology • Previous Articles     Next Articles

Spatio-temporal variation of glacial albedo and its influencing factors in the Muz Tag Peak area

ZHANG Yujiao1(), HUAI Baojuan2, WANG Shengjie1(), CHE Yanjun3, ZHANG Mingjun1   

  1. 1. College of Geography and Environmental Science, Northwest Normal University, Lanzhou 730070, Gansu, China
    2. College of Geography and Environment, Shandong Normal University, Jinan 250300, Shandong, China
    3. Department of Geographical Science, Yichun University, Yichun 336000, Jiangxi, China
  • Received:2024-12-19 Revised:2025-02-22 Online:2025-10-25 Published:2025-10-27
  • Contact: WANG Shengjie E-mail:geozhangyj@163.com;geowang@126.com

Abstract:

Glacier albedo is a key factor influencing the rate of glacier melting and associated environmental changes. In this study, Landsat OLI images with high spatial resolution and MOD10A1 albedo products with high temporal resolution were used to analyze the spatiotemporal variations of glacier albedo and its influencing factors in the Muz Tag Peak area, Xinjiang, China from 2015 to 2020. The results show that: (1) The albedo values derived from Landsat OLI and MOD10A1 are highly consistent, with a strong correlation (R2=0.92). (2) Seasonally, the lowest albedo occurs in summer, while higher values are observed in early autumn. In winter and spring, reduced snowfall and densification of surface snow lead to decreasing albedo. (3) Spatially, glacier surface albedo increases with elevation, following an exponential relationship (R2=0.23 in the ablation area and 0.25 in the accumulation area). (4) Air temperature and precipitation are the primary factors affecting glacier albedo, as higher temperatures and reduced snowfall result in lower albedo. Topography also exerts a significant effect, with gentler slopes exhibiting lower albedo and steeper slopes showing higher albedo. This study provides a scientific basis for understanding glacier change mechanisms in the Muz Tag Peak area and for predicting future climate change.

Key words: glacial albedo, spatio-temporal variation, Landsat OLI, MOD10A1, Muz Tag Glacier