基于MODIS数据的拉萨市地表温度变化研究

Changes of Spatial Distribution of Land Surface Temperature in Lhasa

  • 摘要: 采用2000~2011年6月MODIS地表温度产品和拉萨市4个气象站6月平均地表温度对拉萨市地表温度的时空变化进行了分析。结果表明:拉萨市在近12年内地表温度呈明显上升趋势,2009年地表温度达到最高为28.49℃,最小值出现在2003年为14.12℃。在空间分布上高温区主要集中在城市中心和城市周边区域,并随着时间推移不断向外扩张,在2007年6月拉萨市地表温度高温区分布范围最大,其中纳木错东部和林周县的高温区增加最显著;在利用实测的地表温度与MODIS反演的地表温度做相关分析发现,两者的相关系数为0.64通过了0.001的显著性检验,两种地表温度的时间变化趋势也较为一致,因此MODIS地表温度反演产品适用于大范围地表温度和城市热环境监测是可行的。

     

    Abstract: in this study,the spatial and temporal variations of the MODIS Land Surface Temperature (LST) product (MOD11) and average surface temperature in-situ observation data which belongs to 4 weather station was analysed for the whole of LHASA city during the sixth month of 2000-2011.Resultsshowed that LST increases obviously in nearly 12 years,espacially 2009 and 2010,the spatial distribution of high surface temperature concentrated in the center city and the surrounding area,it is going to expand outward as time elapses.the largest high temperature extend presented to june,2007,espacially west area of Namtso and Linzhou district of Lhasa city;in addition,the correlation coefficient are almost accordance between in-situ LST data and LST MODIS inversion data,thus,the MODIS land surface temperature product (MOD11) are suited to monitor large extend surface temperature and Urban Heat Island.

     

/

返回文章
返回