Snow Cover Phenology in Xinjiang Based on a Novel Method and MOD10A1 Data

被引:6
作者
Wang, Qingxue [1 ,2 ]
Ma, Yonggang [2 ,3 ,4 ,5 ]
Li, Junli [6 ,7 ,8 ]
机构
[1] Xinjiang Univ, Coll Geog & Remote Sensing Sci, Urumqi 830046, Peoples R China
[2] Xinjiang Univ, Xinjiang Key Lab Oasis Ecol, Urumqi 830046, Peoples R China
[3] Xinjiang Univ, Coll Ecol & Environm, Urumqi 830046, Peoples R China
[4] Minist Educ, Xinjiang Jinghe Observat & Res Stn Temperate Deser, Urumqi 830046, Peoples R China
[5] Educ Minist, Key Lab Oasis Ecol, Urumqi 830046, Peoples R China
[6] Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, Urumqi 830011, Peoples R China
[7] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[8] Xinjiang Uygur Autonomous Reg, Key Lab GIS & RS Applicat, Urumqi 830011, Peoples R China
基金
中国国家自然科学基金;
关键词
snow phenology; Xinjiang; MODIS; snow cover; MK-Test; CENTRAL-ASIA; MODIS DATA; VARIABILITY; CLIMATE; TRENDS; DURATION; PRODUCT; CANADA;
D O I
10.3390/rs15061474
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Using Earth observation to accurately extract snow phenology changes is of great significance for deepening the understanding of the ecological environment and hydrological process, agricultural and animal husbandry production, and high-quality development of the social economy in Xinjiang. Considering snow cover phenology based on MODIS product MOD10A1 data, this paper constructed a method for automatically extracting key phenological parameters in Xinjiang and calculated three key phenological parameters in Xinjiang from 2001 to 2020, including SCD (snow cover duration), SOD (snow onset date), and SED (snow end date). The daily data of four field camera observation points during an overlapping period from 2017 to 2019 were used to evaluate the snow cover phenological parameters extracted by MOD10A1, and the mean absolute error (MAE) and root mean square error (RMSE) values were 0.65 and 1.07, respectively. The results showed the following: 1. The spatiotemporal variation in snow phenology was highly altitude dependent. The mean gradients of SCD in the Altai Mountains, Tienshan Mountains, and Kunlun Mountains is 2.6, 2.1, and 1.2 d/100 m, respectively. The variation trend of snow phenology with latitude and longitude was mainly related to the topography of Xinjiang. Snow phenological parameters of different land-use types were different. The SCD values in wasteland were the lowest and the SED was the earliest, while forest land was the first to enter SOD accumulation. According to the study, the mean annual values of SCD, SOD, and SED were 25, 342 (8 December), and 51 (8 February) as day of year (DOY), respectively. The snow cover area was mainly distributed in the Altai Mountains, Junggar Basin, Tianshan Mountains, and Kunlun Mountains. 2. The variation trend and significance of snow cover phenological parameters in different regions are different, and the variation trend of snow cover phenological parameters in most regions of Xinjiang is non-significant.
引用
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页数:19
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