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A Method for Calculating Reference Evapotranspiration on Daily Time Scales

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dc.contributor.author Farmer, William
dc.contributor.author Strzepek, Ken
dc.contributor.author Schlosser, C. Adam
dc.contributor.author Droogers, Peter
dc.contributor.author Gao, Xiang
dc.date.accessioned 2011-03-23T19:01:15Z
dc.date.available 2011-03-23T19:01:15Z
dc.date.issued 2011-02
dc.identifier.uri http://globalchange.mit.edu/pubs/abstract.php?publication_id=2141
dc.identifier.uri http://hdl.handle.net/1721.1/61773
dc.description Abstract and PDF report are also available on the MIT Joint Program on the Science and Policy of Global Change website (http://globalchange.mit.edu/) en_US
dc.description.abstract Measures of reference evapotranspiration are essential for applications of agricultural management and water resources engineering. Using numerous esoteric variables, one can calculate daily reference evapotranspiration using the Modified Penman-Monteith methods. In 1985, Hargreaves developed a simplified method for estimating reference evapotranspiration. Similarly, Droogers and Allen improved upon Hargreaves’ method in 2002. Both methods provide excellent estimates of average daily rates for a given month, based on monthly climatology. The Hargraeves method also estimates daily rates based on daily data, though the Modified Hargreaves approach developed by Droogers and Allen is largely accepted as a stronger metric. Here efforts are made to improve the functionality of Droogers and Allen’s approach and to adapt it to provide daily estimates of reference evapotranspiration based on daily weather. The Hargreaves and Modified Hargeaves are used to calculate daily reference evapotranspiration based on daily data. The coefficients in these equations are then optimized to reduce the root mean squared difference between each estimate and the baseline value calculated by the Modified Penman-Monteith approach. The adapted method for daily reference evapotranspiration proves promising; estimating rates near a root mean squared difference of 1.07 mm/day. These results are validated with data from 1976-1980; here the root mean squared difference is 1.06 mm/day. Results are evaluated spatially and temporally. Weaknesses are seen in the estimates around clearly-defined summers. Further weaknesses are seen in pole-ward regions. Still, at the 1% significance level, the daily optimization of the Modified Hargreaves equation is found to be the best replica of the Modified Penman-Monteith method, globally. Finally, specific caveats and further avenues of research are noted. Overall, the daily Modified-Hargreaves method is advocated for general use in global studies where daily data and variation is of the utmost concern. en_US
dc.description.sponsorship This study received support from the MIT Joint Program on the Science and Policy of Global Change, which is funded by a consortium of government, industry and foundation sponsors. en_US
dc.language.iso en_US en_US
dc.publisher MIT Joint Program on the Science and Policy of Global Change en_US
dc.relation.ispartofseries ;Report no. 195
dc.rights An error occurred on the license name. en
dc.rights.uri An error occurred getting the license - uri. en
dc.title A Method for Calculating Reference Evapotranspiration on Daily Time Scales en_US
dc.type Technical Report en_US
dc.identifier.citation Report no. 195 en_US


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