4.7 Article

Landsat Snow-Free Surface Albedo Estimation Over Sloping Terrain: Algorithm Development and Evaluation

出版社

IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
DOI: 10.1109/TGRS.2022.3149762

关键词

Surface topography; Estimation; Atmospheric modeling; Remote sensing; Reflectivity; Satellites; Surfaces; Artificial neural network (ANN); direct estimation algorithm; Landsat; discrete anisotropic radiative transfer (DART); sloping terrain; surface albedo

资金

  1. National Key Research and Development Program of China [2020YFA0608704]
  2. National Natural Science Foundation of China [42090012, 41771379]

向作者/读者索取更多资源

Surface albedo estimation is challenging in rugged terrains, but this study successfully retrieved albedo on sloping terrain using satellite data and artificial neural networks. The accuracy of the method was verified and different albedo results were evaluated, advancing our understanding of energy budget in mountains.
Surface albedo plays a key role in global climate modeling as a factor controlling the energy budget. Satellite observations were utilized to estimate surface albedo at global and regional scales with good precision over flat areas. However, because topography greatly complicates radiative transfer (RT) processes, estimating the albedo of rugged terrain with satellite data remains a challenge. In addition, albedo definitions over sloping terrain differ from that for flat areas. They include horizontal/horizontal sloped surface albedo (HHSA) and inclined/inclined sloped surface albedo (IISA). Methods for retrieving HHSA and IISA in mountains have not been well-explored. Here, we retrieved HHSA and IISA on sloping terrain from Landsat 8 using a direct estimation algorithm. We simulated a dataset of Landsat top-of-atmosphere (TOA) reflectance and surface albedo with discrete anisotropic radiative transfer (DART) model, for variable atmospheric, vegetation, soil, and topography properties. Then, we used artificial neural networks (ANNs) to derive an empirical relationship between TOA reflectance and surface albedo. The accuracy of our method was verified with in situ measurements: root mean squared error (RMSE) and bias equal to 0.029 and -0.010 for HHSA, and 0.023 and -0.001 for IISA, respectively. Several albedo results (HHSA, IISA, values without topographic consideration) were evaluated and compared. HHSA was found similar to albedo without topographic consideration, but IISA, considered as the true albedo for sloping terrain, showed large difference from them. This study demonstrated the feasibility of surface albedo estimation from Landsat TOA reflectance directly in rugged terrains and advanced our understanding of energy budget in mountains.

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