An evaluation of common evapotranspiration equations (Articolo in rivista)

Type
Label
  • An evaluation of common evapotranspiration equations (Articolo in rivista) (literal)
Anno
  • 1999-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1007/s002710050058 (literal)
Alternative label
  • Ventura F., Duce P., Spano D., Snyder R. L. (1999)
    An evaluation of common evapotranspiration equations
    in Irrigation science; Springer New York, New York (Stati Uniti d'America)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Ventura F., Duce P., Spano D., Snyder R. L. (literal)
Pagina inizio
  • 163 (literal)
Pagina fine
  • 170 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 18 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 8 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
  • 4 (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • Ventura F, Spano D: Università di Sassari, Dipartimento di Economia e Sistemi Arborei Duce P: CNR-IBIMET, Sassari Snyder RL: Department of Land, Air and Water Resources,University of California, Davis (literal)
Titolo
  • An evaluation of common evapotranspiration equations (literal)
Abstract
  • A comparison is made between the Pruitt and Doorenbos version of an hourly Penman-type equation, the Food and Agriculture Organization (FAO) hourly Penman-Monteith equation, and an independent measure of reference evapotranspiration (ET0) from lysimeter data. Reducing the canopy resistance improved the hourly FAO Penman-Monteith estimates. Daytime soil heat flux density is estimated as 10% of net radiation in the FAO hourly Penman-Monteith equation; however, the measured soil heat flux density under grass that was never shorter than 0.10 m in this study was between 3% and 5% of net radiation. The daytime totals of hourly ET0 from the hourly Penman-Monteith and Pruitt-Doorenbos equations and ET0 from the 24-h FAO Penman-Monteith equation were computed using data from five Italian and five Californian stations. A comparison showed that all of the equations gave acceptable results. The Pruitt-Doorenbos equation may slightly over-estimate ET0 in conditions of summertime cold air advection. (literal)
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