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ISSN 2096-7780 CN 10-1665/P

兴安盟区域断裂带与地表温度场变化特征研究

Study on characteristics of regional fault zone and surface temperature change in Xing’an League

  • 摘要: 本文基于Landsat 8 OLI/TIRS遥感影像及最新断裂带矢量数据,分析研究兴安盟区域断裂带与地表温度变化的相关特征。为了提高地表温度反演的准确性,使用最大似然分类算法进行了地表物的分类,然后使用辐射传输方程求解算法分类逆推地表温度。根据研究区域矢量数据绘制的断裂带构造图与遥感影像反演的相同区域的地表温度图,使用Arcmap处理软件,将两幅影像叠加在同一图层上,使用等间距分段均值划分方法,研究分析兴安盟区域断裂带构造地表温度场变化特征,绘制等分断裂带内的平均距离与平均地表温度数据的相关性曲线,进一步确认了断裂带与地表温度场变化的相关性特征。最后,利用同月份不同年份的遥感影像数据进行实验结果的准确性验证。结果表明:兴安盟区域断裂带与地表温度场之间存在一定的相关性,地表温度会随着断裂带等分带距离远近表现出不同程度的变化,越靠近断裂带,地表温度值越高,越远,地表温度值越低。

     

    Abstract: Based on Landsat 8 OLI/TIRS remote sensing images and the latest fault zone vector data, this paper analyzes and studies the characteristics of the regional fault zone and land surface temperature changes in the Xing’an League region. For the accuracy of land surface temperature inversion, the maximum likelihood classification algorithm is used to classify the surface objects, and then the radiative transfer equation algorithm is used to classify and retrieve the land surface temperature. The surface temperature inversion image and the fault zone structure image are superimposed on the same layer, and the average surface temperature and the average distance in each isozonal zone are calculated by using the method of equal interval segmented mean division, the change characteristics of surface temperature field in fault structure are shown by graph, and the relationship between fault zone and surface temperature field is further described by correlation curve. Finally, the remote sensing image data of the same month and different years are used to verify the results. The results show that the farther away the fault zone is from the Xing’an zone, the lower the surface temperature is, on the contrary, the closer the fault zone is, the higher the temperature.

     

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