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Use of Alternative Temperature Expressions with Blaney-Criddle
Journal of Irrigation and Drainage Engineering - ASCE, 2011The widely used Penman-Monteith equation to estimate crop evapotranspiration (ET) has limited utility in many areas of the world because of its requirement for full meteorological data. Legal and engineering water agencies commonly use the original Blaney-Criddle method in their efforts to manage competing water demands in mountain basins, both for its
Joe E Brummer
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Blaney-Criddle Coefficients for Western Turf Grasses
Journal of the Irrigation and Drainage Division, ASCE, 105 (IR4), Proc Paper, 1981Evapotranspiration rates were measured for several turf grasses in Arizona, California, Colorado, and Wyoming. These data were used to calibrate the Blaney-Criddle method for estimating evapotranspiration rates. Warm-season grasses used less water than did cool-season grasses when grown in warm climates.
William E Hart
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Rational Use of The FAO Blaney‐Criddle Formula
Journal of Irrigation and Drainage Engineering - ASCE, 1986The FAO Blaney-Criddle (FAO-BC) evapotranspiration equation was calibrated and tested against a Penman combination equation with local wind function and daily lysimeter measurements of alfalfa evapotranspiration. Agreement between the calibrated FAO-BC method and lysimeters was excellent for daily, weekly and monthly estimates when measured values for ...
Richard G Allen
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Spatio-temporal Calibration of Blaney–Criddle Equation in Arid and Semiarid Environment
Water Resources Management, 2009Estimates of reference evapotranspiration (ETo) are widely used in irrigation engineering to define crop water requirements. A major drawback to application of the FAO Penman-Monteith is the relatively high data demand which unfortunately, for many locations; such meteorological variables are often incomplete and/or not available.
Osama Mohawesh
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Water Resources Management, 2014
Reference evapotranspiration (ET0) data are desirable for assessing crop water requirements and irrigation needs. A large number of methods have been developed for assessing ET0 from meteorological data. In several places of the world, the existing network of weather stations is insufficient to capture the spatial heterogeneity of this variable The ...
Ali Rahimikhoob
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Reference evapotranspiration (ET0) data are desirable for assessing crop water requirements and irrigation needs. A large number of methods have been developed for assessing ET0 from meteorological data. In several places of the world, the existing network of weather stations is insufficient to capture the spatial heterogeneity of this variable The ...
Ali Rahimikhoob
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Hydrological Sciences Journal, 2013
Abstract The Blaney-Criddle (BC) temperature-based equation is used in areas where the complete weather data to estimate reference evapotranspiration (ET0) by the Penman-Monteith FAO-56 (PMF-56) standard model is complex. In this study, the BC equation was first tested and calibrated against the ET0 values computed by the PMF-56 method using data from ...
Hossein Tabari +2 more
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Abstract The Blaney-Criddle (BC) temperature-based equation is used in areas where the complete weather data to estimate reference evapotranspiration (ET0) by the Penman-Monteith FAO-56 (PMF-56) standard model is complex. In this study, the BC equation was first tested and calibrated against the ET0 values computed by the PMF-56 method using data from ...
Hossein Tabari +2 more
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Discussion of “Blaney-Criddle Coefficients for Western Turf Grasses”
Journal of the Irrigation and Drainage Division, ASCE, 105 (IR4), Proc Paper, 1982George H Hargreaves
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Closure to “Blaney-Criddle Coefficients for Western Turf Grasses”
Journal of the Irrigation and Drainage Division, ASCE, 105 (IR4), Proc Paper, 1982William E Hart
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