1997
DOI: 10.1061/(asce)0733-9437(1997)123:4(253)
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Analytical Estimation of Modified Penman Equation Parameters

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Cited by 19 publications
(8 citation statements)
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“…For northern Greece and according to Flokas (1980) a = 0.19 and b = 0.54. Actual daily sunshine (n) is estimated from daily sunshine data, while the terms N and R 0 are calculated, as a function of latitude and day of the year, with the equations proposed by Kotsopoulos and Babajimopoulos (1997).…”
Section: Mathematical Modelling Energy Budget Methods For Evaporation mentioning
confidence: 99%
“…For northern Greece and according to Flokas (1980) a = 0.19 and b = 0.54. Actual daily sunshine (n) is estimated from daily sunshine data, while the terms N and R 0 are calculated, as a function of latitude and day of the year, with the equations proposed by Kotsopoulos and Babajimopoulos (1997).…”
Section: Mathematical Modelling Energy Budget Methods For Evaporation mentioning
confidence: 99%
“…The intra-annual and spatial variability of the ET for regions of Greece has been investigated using different methods by many authors [4][5][6][7][8][9][10][11][12][13][14][15][16][17][18]. The latest and the most detailed mean monthly ET estimations at country scale based on FAO Penman-Monteith method [1] have been performed by Dalezios et al [5] using 66 meteorological stations covering a period of 15 years.…”
Section: Introductionmentioning
confidence: 99%
“…, μ Kassam, 1979Kassam, , , 1999. μ (Doorenbos and Pruitt, 1977, Jensen et al, 1990, USDA, 1993 ., μ μ 94 1994, Papazafiriou, 1996, Papamichail and Terzidis, 1996, Kotsopoulos and Babajimopoulos, 1997, Allen et al, 1998, μ , 1999, -, 2003. , μ Allen et al, 1998Allen et al, , , 1999.…”
Section: Thomas-fieringmentioning
confidence: 99%