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首页> 外文期刊>International journal of remote sensing >An integrated algorithm for estimating regional latent heat flux and daily evapotranspiration
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An integrated algorithm for estimating regional latent heat flux and daily evapotranspiration

机译:估计区域潜热通量和日蒸散量的集成算法

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Using remote-sensing data and ground-based data, we constructed an integrated algorithm for estimating regional surface latent heat flux (LE) and daily evapotranspiration (ET_d). In the algorithm, we first used trapezoidal diagrams relating the surface temperature and fractional vegetation cover (f_c) to calculate the surface temperature-vegetation cover index, a land surface moisture index with a range from 0.0 to 1.0. We then revised a sine function to assess ET_d from LE estimated for the satellite's overpass time. The algorithm was applied to farmland in the North China Plain using Landsat Thematic Mapper (TM)/Enhanced Thematic Mapper Plus (ETM~+) data and synchronous surface-observed data as inputs. The estimated LE and ET_d were tested against measured data from a Bowen Ratio Energy Balance (BREB) system and a large-scale weighing lysimeter, respectively. The algorithm estimated LE with a root mean square error (RMSE) of 50.1 W m~(-2) as compared to measurements with the BREB System, and ET_d with an RMSE of 0.93 mm d~(-1) as compared with the measurement by the lysimeter. Sensitivity analysis showed that changing meteorological variables have some influence on LE, while variation of f_c has little effect on LE. The test of the model in the study indicated that the improved algorithm provides an accurate and easy-to-handle approach for assessing regional surface LE and ET_d. Further improvement can be achieved in the assessments if we increase the accuracy of some key parameters on a large regional scale, such as the minimum stomatal conductance and the atmospheric vapour pressure deficit.
机译:利用遥感数据和地面数据,我们构建了一个综合算法来估算区域表面潜热通量(LE)和日蒸散量(ET_d)。在该算法中,我们首先使用与地表温度和植被分数覆盖率(f_c)相关的梯形图来计算地表温度-植被覆盖指数,即地表水分指数范围为0.0到1.0。然后,我们修改了一个正弦函数,以根据LE估算的卫星过桥时间来评估ET_d。该算法以Landsat Thematic Mapper(TM)/ Enhanced Thematic Mapper Plus(ETM〜+)数据和地面同步观测数据为输入,应用于华北平原农田。分别针对来自鲍文比能量平衡(BREB)系统和大规模称量溶渗仪的测量数据对估计的LE和ET_d进行了测试。该算法估计的LE与BREB系统的测量相比的均方根误差(RMSE)为50.1 W m〜(-2),而ET_d与测量的RMSE的均方根误差为0.93 mm d〜(-1)通过溶渗仪。敏感性分析表明,变化的气象变量对LE有一定影响,而f_c的变化对LE影响不大。在研究中对模型的测试表明,改进的算法为评估区域表面LE和ET_d提供了一种准确且易于操作的方法。如果我们在较大的区域范围内提高某些关键参数的准确性,例如最小的气孔导度和大气蒸气压亏缺,则可以在评估中实现进一步的改进。

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