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内蒙古积雪面积时空变化及其对气候响应
引用本文:萨楚拉,刘桂香,包刚,包玉海,王牧兰. 内蒙古积雪面积时空变化及其对气候响应[J]. 干旱区资源与环境, 2013, 0(2): 137-142
作者姓名:萨楚拉  刘桂香  包刚  包玉海  王牧兰
作者单位:中国农业科学院草原研究所;内蒙古师范大学地理科学学院;内蒙古自治区遥感与地理信息系统重点实验室
基金项目:农业部公益性行业项目"草原火灾应急管理技术(200903041)";内蒙古科技计划项目"内蒙古数字农牧业GIS集成开发与应用示范";内蒙古自然基金项目(2012MS0620)资助
摘    要:区域尺度积雪信息的时空监测,对确定雪灾的影响范围及灾情等级划分具有重要意义。利用2002-2012年10个积雪季节的Terra Aqua/MODIS积雪产品(MOD10A2),按月最大面积合成,分析了内蒙古积雪覆盖面积的时空变化特征及气候响应。结果表明:时间上,近10年内蒙古积雪面积年内变化整体上呈现双峰和单峰的波动特点,最大积雪面积发生在12月和1月份,最小积雪面积发生在10月份。近10年内蒙古积雪面积年际变化呈现波动的特点,整体上积雪面积有减少的趋势。空间上大兴安岭西麓、呼伦贝尔高原以及乌珠穆沁盆地是积雪长时间覆盖区,锡林郭勒草原和乌兰察布草原的积雪面积变化主导着内蒙古的总体积雪面积波动,1月份之前是积雪面积增加的阶段,之后是积雪消融阶段。内蒙古的积雪面积变化与当地的气候条件变化趋势相关,气温的明显上升引起暖冬化,可能导致积雪面积的减少,说明内蒙古积雪面积的变化主要受气温的影响。

关 键 词:内蒙古  MOD10A2  积雪面积  气候响应

The spatial and temporal changes of snow cover in Inner Mongolia and their responses to climate
SA Chula,LIU Guixiang,BAO Gang,BAO Yuhai,WANG Mulan. The spatial and temporal changes of snow cover in Inner Mongolia and their responses to climate[J]. Journal of Arid Land Resources and Environment, 2013, 0(2): 137-142
Authors:SA Chula  LIU Guixiang  BAO Gang  BAO Yuhai  WANG Mulan
Affiliation:1.Grassland Research Institute of Chinese Academy of Agricultural Sciences,Hohhot 010010,P.R.China;2.College of Geographical Science Inner Mongolia Normal University,Hohhot 010022,P.R.China;3.Inner Mongolia Key Laboratory of Remote Sensing and Geographic Information System,Inner Mongolia Normal University,Hohhot 010022,P.R.China)
Abstract:The spatial and temporal change patterns of snow cover of the Inner Mongolia were analyzed by 10 seasonal Terra Aqua/MODIS snow products(MOD10A2) collected during 2002-2010 which were composed according to maximum area rule.The results indicate that snow cover change presented fluctuation patterns of 2 peaks and 1 peak in recent 10 years.The maximum snow cover appeared in December and January and the minimum was in October.The snow cover fluctuated and had a decreasing trend.The Hulunbeier grassland and ujimqin Basin were the long-term snow coverage area.The snow cover changes of Xilin Gol and Wulanchabu Grassland were dominant in general snow cover change fluctuation.The snow in the Inner Mongolia accumulated before January and thawed after January.The changes of snow cover were consistent well with regional climate change.Temperature increasing and decrease of the precipitation were the major reason for decreases of snow cover.This indicates the climate condition has an important consequence for snow cover changes.
Keywords:Inner Mongolia  MOD10A2  snow cover  climate responses
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