1996
DOI: 10.1016/0378-3774(95)01194-3
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A statistical approach for estimating irrigation water usage in western Saudi Arabia

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Cited by 9 publications
(5 citation statements)
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“…Chiew et al (1995) indicated that the BC equation gave similar ET 0 estimates as the FAO-56 PM method at 16 Australian locations with a wide range of climate conditions. Abu Rizaiza and Al-Osaimy (1996) indicated that irrigation water requirements for vegetables and perennial crops are close to the values estimated by the BC equation in the western region of Saudi Arabia. The results of another study showed that the Hargreaves and BC equations were the best ones for Davis in California and Jagdalpur in India with arid and humid climates, respectively (George et al 2002a, b).…”
Section: Introductionmentioning
confidence: 88%
“…Chiew et al (1995) indicated that the BC equation gave similar ET 0 estimates as the FAO-56 PM method at 16 Australian locations with a wide range of climate conditions. Abu Rizaiza and Al-Osaimy (1996) indicated that irrigation water requirements for vegetables and perennial crops are close to the values estimated by the BC equation in the western region of Saudi Arabia. The results of another study showed that the Hargreaves and BC equations were the best ones for Davis in California and Jagdalpur in India with arid and humid climates, respectively (George et al 2002a, b).…”
Section: Introductionmentioning
confidence: 88%
“…As an example, a reduction in the irrigation water of 30-40 % could be attained when sprinkler irrigation is used instead of traditional methods. An additional saving of 10-25 % can be reached with drip irrigation systems (Rizaiza and Al-Osaimy, 1996). Furthermore, implementation of recent innovative precision irrigation technologies, in conjunction with the accurate estimation of crop water requirements through remotely sensed data, could significantly enhance the efficient use of irrigation water in the agricultural sector.…”
Section: Introductionmentioning
confidence: 99%
“…Groundwater recharge and evapotranspiration from the meteorological data were calculated using a simple water balance method (Bonell et al , 1993) and a modified Penman method (Ayob et al , 2007) was assigned to the top layer. The modified Penman method has been successfully applied in evapotranspiration estimation in worldwide application (Lee et al , 2004; Abu Rizaiza and Al‐Osaimy, 1996). Recharge and evapotranspiration were found to vary with time and these were generally the larger factors influencing the transient behavior of the groundwater system.…”
Section: Methodsmentioning
confidence: 99%