Arid Zone Research ›› 2025, Vol. 42 ›› Issue (11): 2058-2070.doi: 10.13866/j.azr.2025.11.09

• Land and Water Resources • Previous Articles     Next Articles

Impact of temporal phase bias on multiyear glacier changes

WANG Hui1(), LIU Ruoxi1, XU Weixin1,2(), ZHENG Zhaojun3, XIAO Ruixiang4, LI Huijun1, WU Chengna1   

  1. 1. College of Resources and Environment Science, Chengdu University of Information Technology, Chengdu 610225, Sichuan, China
    2. Chengdu Plain Urban Meteorology and Environment Observation and Research Station of Sichuan Province, Chengdu 610225, Sichuan, China
    3. National Satellite Meteorological Center, Beijing 100081, China
    4. Qinghai Institute of Meteorological Science, Xining 810001, Qinghai, China
  • Received:2025-05-12 Revised:2025-10-08 Online:2025-11-15 Published:2025-12-13
  • Contact: XU Weixin E-mail:13980867805@163.com;weixin.xu@cuit.edu.cn

Abstract:

The seasonal difference in satellite time phase directly affects the accuracy of studies of multiyear changes in glaciers. In this study, we used the daily MODIS images for the warm season (June-September) from 2000 to 2023 to establish a unified comparison standard for the daily snow-area sequence and the annual minimum snow area in glacier areas, evaluate the impact of time-phase deviation on determinations of the temporal variations in glaciers, and analyze the multi-year dynamic-variation characteristics of the snow area in the glacier areas. The results show that: (1) The maximum deviation of glacier-area estimations caused by the time-phase deviation of satellite images is -23.25%, and the deviation is still as much as 7.75% even when the period is in the range from June to September. (2) After eliminating the influence of the time-phase deviation, we found that the existing research results for the changes in the Geladandong and Animachen glacier regions have significantly underestimated the downward trend of glacier changes in the past 20 years. In addition, the rate of reduction in the area of the Animachen glacier is 17.03%, which is greater than the original finding. (3) Based on the time series for the minimum area of snow cover from 2000 to 2023, the annual rate of reduction of the Geladandong glacier over the past 24 years is 0.24%·a-1 (a cumulative reduction of 5.42%), and that of the Animachen glacier is 0.43%·a-1 (a cumulative reduction of 9.82%). The annual minimum snow cover area of the Geladandong glacier exhibits a significant downward trend, while that of the Animachen glacier is not obvious, which is different from the current understanding. (4) Taking these two glacier regions as typical examples, we find that the snow-cover area in the glacier regions in the hinterland of the Qinghai-Xizang Plateau usually reaches its minimum during the first ten days of August. The time-phase deviation is generally less than 0.5% when the satellite images in this period or near 20 days are selected. If instead satellite images in early June or late September are selected, the time-phase deviation may may account for more than 12% of the resulting total deviation, and the time-phase deviation of the images in June is generally less than that in September.

Key words: glacier variations, temporal phase bias, satellite remote sensing, Three-River Source region