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基于2001-2015年遥感数据的天山山区雪线监测及分析

李帅 侯小刚 郑照军 张连成 木扎帕尔·木合塔尔 胥志德

水科学进展2017,Vol.28Issue(3):364-372,9.
水科学进展2017,Vol.28Issue(3):364-372,9.DOI:10.14042/j.cnki.32.1309.2017.03.006

基于2001-2015年遥感数据的天山山区雪线监测及分析

Monitoring and analysis of snowline on Tianshan Mountains basedon remotely sensed data from 2001 to 2015

李帅 1侯小刚 2郑照军 3张连成 2木扎帕尔·木合塔尔 4胥志德5

作者信息

  • 1. 中国气象局乌鲁木齐沙漠气象研究所,新疆乌鲁木齐 830002
  • 2. 新疆维吾尔自治区气候中心,新疆乌鲁木齐 830002
  • 3. 国家卫星气象中心,北京 100081
  • 4. 乌鲁木齐气象卫星地面站,新疆乌鲁木齐 830011
  • 5. 民航新疆管理局,新疆乌鲁木齐 830016
  • 折叠

摘要

Abstract

We monitored the seasonal snowline elevation on Tianshan Mountains and analyzed its changing characteristics and impact factors by adopting the snow cover duration ratio method, based on MOD10A1/MYD10A1, MOD13Q1 and related meteorological data from 2001 to 2015.The results show that: ① The overall snowline on Tianshan Mountains have been on the rise significantly in the recent 15 years, with average elevation of about 3680 meters, wherein the stability of the snow lines on the northern slope of Tianshan Mountains, Yili River Valley and the southern slope of Tianshan Mountains has weakened successively, the average elevations of which are 3620, 3390 and 3820 meters respectively;the snowline elevation in space shows the latitudinal zonality distribution characteristics of being high in the south and low in the north and high in the east and low in the west.② On the interannual scale, temperature is the main controlling factor which influences the snowline elevation of Tianshan Mountains, with significant positive correlation, so are the case on the south and north slopes of the Tianshan Mountains, while in Yili River Valley, precipitation is the main controlling factor that influences its change, with significant negative correlation;on the seasonal scale, the temperature in summer and the precipitation in winter are the main controlling factors which influence the snowline elevation, precipitation assumes negative correlation with it, while in areas with higher temperature, the precipitation in summer and autumn can facilitate snow melting, which makes the snowline elevation rise;on the monthly scale, the temperature in July and the precipitation in January are most obvious in affecting it, and there exists a certain lag in response.③ The snowline elevation of Tianshan Mountains is about 800 meters lower than the zero degree layer, the two have a good positive correlation;snowline elevation shows negative correlation with NDVI, in areas with good vegetation cover, NDVI and snowline elevation in the same year have a good correlation, while in areas with poor vegetation cover, NDVI in the previous year has a good correlation with it.

关键词

雪线高程/遥感/天山山区/影响因子

Key words

snowline/remote sense/Tianshan Mountains/impact factor

分类

天文与地球科学

引用本文复制引用

李帅,侯小刚,郑照军,张连成,木扎帕尔·木合塔尔,胥志德..基于2001-2015年遥感数据的天山山区雪线监测及分析[J].水科学进展,2017,28(3):364-372,9.

基金项目

国家自然科学基金资助项目(41505077 ()

41471358)The study is financially supported by the National Natural Science Foundation of China (No.41505077 ()

No.41471358). ()

水科学进展

OA北大核心CSCDCSTPCD

1001-6791

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