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首页> 外文期刊>Geothermics >Monitoring thermal anomaly and radiative heat flux using thermal infrared satellite imagery - A case study at Tuzla geothermal region
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Monitoring thermal anomaly and radiative heat flux using thermal infrared satellite imagery - A case study at Tuzla geothermal region

机译:利用热红外卫星图像监测热异常和辐射热通量-以图兹拉地热区为例

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Geothermal energy, which is renewable, reliable and environmentally friendly, is one of the most important energy resources. Thus, it is crucial to explore geothermal areas in order to reduce the use of other energy sources that are detrimental to the environment and ecology. Thermal Infrared (TIR) remote sensing is an effective way to detect thermal anomalies in geothermal areas and volcanoes, since it is cost and time effective, and offers to work on a large scale compared to geophysical methods. The aim of this study is to investigate thermal anomalies in Tuzla geothermal region using daytime and nighttime TIR data with reference to Land Surface Temperature (LST) and Radiative Heat Flux (RHF). Many geophysical studies have been conducted in this region; however, it can also be studied with TIR remote sensing for further exploration. Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) data, acquired on 15.06.2012 and 15.07.2017 as daytime image and 15.09.2013 and 31.12.2017 as nighttime image, were utilized as satellite imagery. In addition to ASTER data, we proposed a multi-sensor based LST retrieval for nighttime using Landsat 8 data for emissivity acquisition. In order to evaluate the accuracy of LST images, cross-validation method was utilized with reference to Moderate Resolution Imaging Spectroradiometer (MODIS) LST products. The coefficient of determination (r(2)) and Root Mean Square Error (RMSE) were considered as statistical metrics and the lowest result was obtained as 90% and 1.76 K, respectively. As a result of the analyses, it was observed that nighttime LST presented better results for thermal anomalies in that geothermal area than daytime LST. Considering geothermal anomaly, the geothermal area had higher LST values even though it held identical or same NDVI values as compared to non-geothermal surroundings. In addition, the net radiative heat loss values were calculated as 17.83 MW and 121.28 MW for 2013 and 2017, respectively. The obtained results proved that TIR remote sensing could be utilized in the studies of geothermal area exploration.
机译:地热能是可再生的,可靠的和环境友好的,是最重要的能源之一。因此,至关重要的是探索地热区域,以减少对环境和生态有害的其他能源的使用。热红外(TIR)遥感是一种检测地热区域和火山中热异常的有效方法,因为它既节省成本又节省时间,并且与地球物理方法相比具有较大的工作量。这项研究的目的是参考白天和夜间的TIR数据,参考地表温度(LST)和辐射热通量(RHF),调查图兹拉地热地区的热异常。该地区已进行了许多地球物理研究。但是,也可以使用TIR遥感进行研究以进一步探索。于2012年6月15日和2017年7月15日获取的先进星载热发射和反射辐射计(ASTER)数据为白天图像,并于2013年9月15日和2017年12月31日获取为夜间图像,用作卫星图像。除ASTER数据外,我们还提出了一种基于多传感器的LST夜间检索,该检索使用Landsat 8数据进行了发射率采集。为了评估LST图像的准确性,参考了中分辨率成像光谱仪(MODIS)LST产品的交叉验证方法。确定系数(r(2))和均方根误差(RMSE)被视为统计指标,最低结果分别为90%和1.76K。分析的结果是,观察到夜间LST在该地热区域的热异常结果要比白天LST更好。考虑到地热异常,即使与非地热环境相比,地热区域具有相同或相同的NDVI值,其LST值也较高。此外,2013年和2017年的净辐射热损失值分别计算为17.83 MW和121.28 MW。所得结果证明,TIR遥感技术可用于地热区勘探研究。

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