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USGS · 70243873

Sensitivity of the Penman-Monteith reference evapotranspiration equation to meteorological variables for Puerto Rico

Abstract

Spatiotemporal variations in reference evapotranspiration ( ET o ) are sensitive to the meteorological data used in its estimation. The sensitivity of the ASCE standardized ET o equation to meteorological variables from GOES-PRWEB dataset was evaluated for the island of Puerto Rico. Island wide, ET o is most sensitive to daily mean relative humidity ( RH mean ), followed by solar radiation, daily maximum ( T max ) and minimum ( T min ) air temperatures, and wind speed with average absolute relative sensitivity coefficients (SCs) of 0.98, 0.57, 0.50, 0.27, and 0.12, respectively. The derived SCs guided the prioritization of bias correction of meteorological data for ET o estimation from two downscaled climate models (CNRM and CESM). The SCs were applied to evaluate how meteorological variables contribute to model errors and projected future changes in ET o from 1985–2005 to 2040–2060 at irrigated farms in the south. Both models project a 5.6% average increase in annual ET o due to projected increases in T max and T min and a decrease in RH mean . Despite ET o being most sensitive to relative changes in RH mean , the contributions from RH mean , T max , and T min to future changes in ET o are similar. CESM projects increases in ET o in March, November, and December, increasing the potential for crop water stress. Study limitations are discussed.

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90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 17.926875° to 18.515757° latitude; -67.940799° to -65.221568° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeXRIS

Michelle M. Irizarry-Ortiz, Eric Harmsen. 2023-04-25. Sensitivity of the Penman-Monteith reference evapotranspiration equation to meteorological variables for Puerto Rico. https://doi.org/10.3390/hydrology10050101

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