The crop water need ET crop is defined as the depth or amount of water needed to meet the water loss through evapotranspiration. In other words, it is the amount of water needed by the various crops to grow optimally. The crop water need always refers to a crop grown under optimal conditions, i. The crop thus reaches its full production potential under the given environment. Section 3. The major climatic factors see Fig.
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Skip to search form Skip to main content You are currently offline. Some features of the site may not work correctly. The Blaney-Criddle B-C method is the simplest approach for estimating PE as it requires only temperature data for input.
It has been found that the B-C method can provide accurate estimates for moderate climates. Under extreme climatic conditions the B-C method is inaccurate. Save to Library. Create Alert. Launch Research Feed.
Share This Paper. Citations Publications citing this paper. Final results of the cover system test panel trials at the Pierina mine Michael A. Milczarek , Robert C. Rice , Ma Williamson Environmental Science References Publications referenced by this paper.
Elisavet Papadopoulou Geography Estimating crop evapotranspiration James L. Wright Geography A simple method for determining the evaporation from shallow lakes and ponds Robert Bruce Stewart , Wayne Rouse Geology Natural evaporation from open water, bare soil and grass H. Series A.
Water Management in Horticultural Crops (1+1)
The Blaney—Criddle equation named after H. Blaney and W. Criddle is a method for estimating reference crop evapotranspiration. The Blaney—Criddle equation is a relatively simplistic method for calculating evapotranspiration.
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