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On parameterizing soil evaporation in a direct remote sensing model of ET: PT‐JPL
2020
Water Resources Research
Remote sensing models that measure evapotranspiration directly from the Penman-Monteith or Priestley-Taylor equations typically estimate the soil evaporation component over large areas using coarse spatial resolution relative humidity (RH) from geospatial climate datasets. As a result, the models tend to underperform in dry areas at local scales where moisture status is not well represented by surrounding areas. Earth observation sensors that monitor large-scale global dynamics (e.g., MODIS)
doi:10.1029/2019wr026290
fatcat:lwsu4zqqtba77cvk7hpbpzxtle