{"refrec":{"BRefID":247001,"RR":"<b>Tabari, H.; Talaee, H; Some'e, S; Willems, P.</b> (2014). Possible influences of North Atlantic Oscillation on winter reference evapotranspiration in Iran. <i>Global Planet. Change 117</i>: 28-39. <a href=\"http://dx.doi.org/10.1016/j.gloplacha.2014.03.006\" target=\"_blank\">dx.doi.org/10.1016/j.gloplacha.2014.03.006</a>","BEntID":238701,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Global Planet. Change 117</i>: 28-39. <a href=\"https://dx.doi.org/10.1016/j.gloplacha.2014.03.006\" target=\"_blank\">https://dx.doi.org/10.1016/j.gloplacha.2014.03.006</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Tabari, H.; Talaee, H; Some'e, S; Willems, P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Tabari, H. <i>et al.</i>","Englishabstract":"The North Atlantic Oscillation (NAO) is known to be responsible for most of inter-annual atmospheric variability over the Northern Hemisphere, particularly in Europe and the Mediterranean basin. Owing to the importance of reference evapotranspiration (ET<sub>o</sub>) in irrigation planning, water resource monitoring and management, we assessed the impact of the NAO on the ET<sub>o</sub> variability during the winter months from December to March in Iran. The Penman–Monteith FAO 56 method was applied to estimate ET<sub>o</sub> based on meteorological data from 41 synoptic stations during a period of 40 years (1966–2005). The correlation between the monthly NAO index and the ET<sub>o</sub> time series was computed using the Spearman's rho test for time lags from 0 to 6 months. The simultaneous and lag correlation analyses demonstrated that the winter ET<sub>o</sub> series over Iran had negative correlations with the NAO index at almost all the stations. The highest negative correlation of 0.53 was observed between the January ET<sub>o</sub> series and the August NAO at Tabriz station located in the northwest of Iran, whereas the highest positive correlation of 0.55 was found between the January ET<sub>o</sub> series and the simultaneous NAO at Bandar-Lengeh station which is situated on the northern coast of the Persian Gulf. Averaged over the 41 stations, the winter ET<sub>o</sub> values during the negative phase of the NAO were about 3% higher than those during the positive phase.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Possible influences of North Atlantic Oscillation on winter reference evapotranspiration in Iran","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"reference evapotranspiration variability; NAO index; Spearman's rhotest; correlation; time lag; Iran","OtherDescriptors":null,"Notes":null,"AnaPub":2014,"MonPub":null,"DateUpdate":"2015-08-07","DateCreate":"2015-05-21","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000336709400003","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.gloplacha.2014.03.006"},"refs":null,"anarec":{"AnaID":247001,"PubliDate":2014,"Pagination":"28-39","XtraPublOfAnaID":null,"ISBN":null,"Volume":"117","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42934,"SerRR":"Global and Planetary Change. Elsevier: Amsterdam; New York; Oxford; Tokyo.  ISSN 0921-8181; e-ISSN 1872-6364","StandardTitleSer":"Global and Planetary Change","ISSN":"0921-8181","AbbrevSer":"Global Planet. 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