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首页> 外文期刊>Journal of Applied Remote Sensing >Lake surface temperature retrieval from Landsat-8 and retrospective analysis in Karaoun Reservoir, Lebanon
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Lake surface temperature retrieval from Landsat-8 and retrospective analysis in Karaoun Reservoir, Lebanon

机译:Laksat-8湖表面温度检索和黎巴嫩卡拉尼库尔水库回顾性分析

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The importance of lake water surface temperature has long been highlighted for ecological and hydrological studies as well as for water quality management. In the absence of regular field observations, satellite remote sensing has been recognized as a cost-effective way to monitor water surface temperature on large spatial and temporal scales. The thermal infrared sensors (TIRS) onboard of Landsat satellites (since 1984) are adequate tools for monitoring surface temperature of small to medium sized lakes with a biweekly frequency, as well as for performing retrospective analysis. Nonetheless, the satellite data have to deal with effects due to the atmosphere so that several approaches to correct for atmospheric contributions have been proposed. Among these are: (i) the radiative transfer equation (RTE); (ii) a single-channel algorithm that depends on water vapor content and emissivity (SC1); (iii) its improved version including air temperature (SC2); and (iv) a monowindow (MW) algorithm that requires emissivity, atmospheric transmissivity, and effective mean atmospheric temperature. We aim to evaluate these four approaches in a river dammed reservoir with a size of 12 km(2) using data gathered from the band 10 of the TIRS onboard of Landsat 8. Satellite-derived temperatures were then compared to in situ data acquired from thermistors at the time of Landsat 8 overpasses. All approaches showed a good performance, with the SC1 algorithm yielding the lowest root mean square error (0.73 K), followed by the SC2 method (0.89 K), the RTE (0.94 K), and then the MW algorithm (1.23 K). Based on the validation results, we then applied the SC1 algorithm to Landsat 4, 5, and 8 thermal data (1984 to 2018) to extend data series to past years. These data do not reveal any warming trend of the reservoir surface temperature. The results of this study also confirm how the 100-m spatial resolution of TIRS is valuable as an additional source of data to field-based monitoring. (C) 2019 Society of Photo-Optical Instrumentation Engineers (SPIE)
机译:湖水表面温度的重要性长期以来,为生态和水文研究以及水质管理突出了。在没有常规现场观察的情况下,卫星遥感被认为是一种经济高效的方法来监测大量空间和时间尺度的水面温度。 Landsat卫星(自1984年以来)的热红外传感器(TIRS)是用于监测小于中等湖泊的表面温度的适当工具,以及双周频率,以及进行回顾性分析。尽管如此,卫星数据必须根据大气处理效果,从而提出了若干纠正大气贡献的方法。其中:(i)辐射转移方程(RTE); (ii)一种依赖于水蒸气含量和发射率(SC1)的单通道算法; (iii)其改进的版本,包括气温(SC2); (iv)一种单向管道(MW)算法,需要发射率,大气透射率和有效的平均大气温度。我们的目标是使用从Landsat板上的TIR的频段10收集的数据来评估河流型储层中的这四种方法,其中尺寸为12km(2)。然后将卫星衍生的温度与热敏电阻获取的原位数据进行比较在Landsat 8立交桥的时候。所有方法都显示出良好的性能,SC1算法产生最低的根均方误差(0.73 k),然后是SC2方法(0.89 k),RTE(0.94 k),然后是MW算法(1.23 k)。基于验证结果,我们将SC1算法应用于Landsat 4,5和8个热数据(1984年至2018)以将数据序列扩展到过去几年。这些数据没有透露储层表面温度的任何变暖趋势。本研究的结果还证实了100米的TIR的空间分辨率如何有价值作为基于现场的监测的额外数据来源。 (c)2019年光学仪表工程师协会(SPIE)

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