新疆准东露天煤矿区地表温度反演及时空变化特征

    Spatio-temporal variation of land surface temperature in the coalmine area of Zhundong in Xinjiang

    • 摘要: 使用Landsat7/ETM+于2005年7月22日和2013年6月10日过境的新疆准东煤田矿区的影像数据,运用单窗算法以及Weng算法反演准东煤矿开采前后的地表温度。通过反演结果与热红外辐射计实测数据对比证明在本研究区运用单窗算法反演地表温度较Weng算法精度更高。在此基础上,分析了不同时期准东矿区地表温度分布格局得出:①时间尺度上,由开采前的最高温42.7℃上升至49.2℃,最低温保持在11~12℃。2013年地表温度平均值为35.1℃高于2005年的30.8℃;②空间尺度上,矿区地形独特,北方为喀拉麦里山,南方为天山绿洲带,两山包裹呈现典型的"热岛"效应。从2013年温度分布图可以看出明显的温度变化梯度,由外到内依次是荒漠草原、荒漠裸土、岩石裸地以及露天矿坑,地表温度呈现依次升高。总之,单窗算法反演精度高,适合干旱区露天煤矿地表温度反演。

       

      Abstract: This article is about retrieving the land surface temperature in Wucaiwan coalfield before-and-after mined in Xinjiang by using the Monowindow algorithm and Weng algorithm with the images of Landsat7/ETM+ taken in July 22th,2005 and June 10th,2013.Compared the inversion results with the measured data by thermal infrared radiometer,it proved that the Monowindow algorithm has higher precision than Weng for retrieving the land surface temperature in this study area.Based on this,it concludes after analyzing different LST distribution patterns that ① on temporal scales,the highest temperature before mining went 42.7℃ to 49.2℃while the lowest was higher 4℃.The LST mean value in 2013 being 35.1℃ was higher than that of 2005 being 30.8℃.② on spatial scales,the coalmine area terrain distinctively present typical heat island effect between the Kalamali mountain in its north and Tianshan mountain oasis band.

       

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