Mapping reference evapotranspiration from meteorological satellite data and applications

  • Author(s): Ming-Hwi Yao, Ming-Hsu Li, Jehn-Yih Juan, Yue-Joe Hsia, Ping-Ho Lee, and Yuan Shen
  • DOI: 10.3319/TAO.2016.11.15.01
  • Keywords: Remote sensing, Flux tower, Evapotranspiration, Crop coefficient, Landscape coefficient
  • Citation: Yao, M.-H., M.-H. Li, J.-Y. Juan, Y.-J. Hsia, P.-H. Lee, and Y. Shen, 2017: Mapping reference evapotranspiration from meteorological satellite data and applications. Terr. Atmos. Ocean. Sci., 28, 501-515, doi: 10.3319/TAO.2016.11.15.01
  • Deriving ETo without LST and auxiliary weather data
  • Derived ETo is comparable with the FAO PM method
  • Land coefficients for four landscapes were determined

Reference evapotranspiration (ETo) is an agrometeorological variable widely used in hydrology and agriculture. The FAO-56 Penman-Monteith combination method (PM method) is a standard for computing ETo for water management. However, this scheme is limited to areas where climatic data with good quality are available. Maps of 10-day averaged ETo at 5 km × 5 km grid spacing for the Taiwan region were produced by multiplying pan evaporation (Epan), derived from ground solar radiation (GSR) retrieved from satellite images using the Heliosat-3 method, by a fixed pan coefficient (Kp). Validation results indicated that the overall mean absolute percentage error (MAPE) and normalized root-mean-square deviation (NRMSD) were 6.2 and 7.7%, respectively, when compared with ETo computed by the PM method using spatially interpolated 10-day averaged daily maximum and minimum temperature datasets and GSR derived from satellite inputs. Land coefficient (KL) values based on the derived ETo estimates and long term latent heat flux measurements, were determined for the following landscapes: Paddy rice (Oryza sativa), subtropical cypress forest (Chamaecyparis obtusa var. formosana and Chamaecyparis formosensis), warm-to-temperate mixed rainforest (Cryptocarya chinensis, Engelhardtia roxburghiana, Tutcheria shinkoensis, and Helicia formosana), and grass marsh (Brachiaria mutica and Phragmites australis). The determined land coefficients are indispensable to scale ETo in estimating regional evapotranspiration.

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