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干旱区地理 ›› 2019, Vol. 42 ›› Issue (4): 782-789.doi: 10.12118/j.issn.1000-6060.2019.04.09

• 气候与水文 • 上一篇    下一篇

基于MODIS数据的蒙古高原积雪时空变化研究

姜康,包刚,乌兰图雅,姜莉,王牧兰   

  1. 1内蒙古师范大学地理科学学院,内蒙古呼和浩特010022; 2内蒙古师范大学内蒙古自治区遥感与地理信息系统重点实验室,内蒙古呼和浩特010022
  • 收稿日期:2019-01-24 修回日期:2019-04-01 出版日期:2019-07-25 发布日期:2019-07-24
  • 通讯作者: 包刚(1978-),男,内蒙古库伦旗人,副研究员,主要从事遥感与地理信息系统应用研究. E-mail:baogang@imnu.edu.cn
  • 作者简介:姜康(1994-),男,山东青岛人,硕士研究生,研究方向为遥感应用研究. E-mail:jiangkangyjs@163.com
  • 基金资助:
    内蒙古自治区自然科学基金项目(2017MS0402,2016MS0409);内蒙古自治区高等学校“青年科技英才”支持计划项目(NJYT-18-A11)的资助

Spatiotemporal changes of snow cover in Mongolian Plateau based on MODIS data

JIANG Kang1,BAO Gang1,2,WULANTUYA1,JIANG Li1,WANG Mulan1   

  1. 1 College of Geographical Science,Inner Mongolia Normal University,Hohhot 010022,Inner Mongolia,China; 2 Inner Mongolia Key Laboratory of Remote Sensing and Geographic Information Systems,Inner Mongolia Normal University,Hohhot 010022,Inner Mongolia,China
  • Received:2019-01-24 Revised:2019-04-01 Online:2019-07-25 Published:2019-07-24

摘要: 利用Terra卫星和Aqua卫星提供的2002年9月1日~2017年5月31日每日积雪覆盖产品MOD10C1和MYD10C1,提取蒙古高原积雪日数、积雪面积、积雪初日及积雪终日信息,得到蒙古高原积雪特征分布和变化趋势,同时,结合蒙古高原108个地面气象观测站的气温资料,分析研究区积雪变化特征和气温的关系。结果表明:(1)蒙古高原平均积雪日数在60~90 d之间,积雪初日主要分布在315~335 d之间,积雪终日大多集中在31~61 d之间,蒙古高原东部地区积雪初日有明显的提前趋势,西南地区积雪终日有明显的提前趋势。(2)积雪面积在积雪季内呈 “单峰型”,1月份为积雪面积最大月,年均积雪面积呈微弱的下降趋势。(3)最大积雪覆盖面积与温度具有明显的相关性,稳定积雪覆盖区的临界温度大概介于-11~-8 ℃之间。(4)温度是影响积雪特征变化的重要因素。

关键词: 蒙古高原, 积雪, MODIS, 气候变化, 温度

Abstract: The paper extracted the snow cover days (SCD),snow cover area (SCA),snow cover onset dates (SCOD) and snow cover melting dates (SCMD) in the Mongolian Plateau using the daily snow cover products MOD10C1 and MYD10C1 derived from the Terra and Aqua satellite from September 1,2002 to May 31,2017.At the same time,the temperature from the 108 weather stations across the plateau was used to analyze the relationship between snow cover characteristics and temperature.The paper used the pixel discrimination method to identify snowcovered pixels,and used the method of pixel accumulation to obtain the annual snow cover days of the plateau.The results show as follows: (1) The average SCD in the Mongolian Plateau ranged between 60 and 90 days,and it was correlated well with latitude.The SCD in the eastern region showed a slight upward trend and the southwestern region showed a significant downward trend.The SCOD in the plateau was mainly distributed between 315 and 335 days,and SCMD was mostly concentrated between 31 and 61 days.The SCOD in the east of the plateau showed a clear trend of moving early.(2) SCA presented “singlepeak” during the snow season.The SCA reached its maximum value in January,and the average SCA was 101.6×104 km2.The average annual SCA fluctuated greatly and there was a weak downward trend overall.(3) The maximum coverage area of snow has a significant correlation with temperature.From September to December,the average temperature was dropped by around 10 ℃ per month,and the temperature was relatively stable from December to February.From February to May,the average temperature was risen by around 10 ℃ per month.(4) There is a significant negative correlation between SCD,SCMD and temperature.SCOD has a significant positive correlation with temperature.A higher correlation can indicate that temperature is a key factor affecting snow cover.The paper used MODIS data to analyze the spatial and temporal distribution and changes of snow cover in the Mongolian Plateau,and could provide reference for the subsequent changes in water resources and vegetation growth in the Mongolian Plateau.At the same time,this paper also shows the dynamic changes of snow in the Mongolian Plateau during the years and the relationship with temperature,which provides a basis for disaster prevention and animal husbandry in the Mongolian Plateau.

Key words: Mongolian Plateau, snow cover, MODIS, climate change, temperature