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WATER AENV SIRS 15 – 43<br />

Section 12.1<br />

Blaney, H. F. and Criddle, W. D. 1950. Determining Water Requirements in<br />

Irrigated Area from Climatological Irrigation Data, US Department of<br />

Agriculture, Soil Conservation Service, Tech. Pap. No. 96, 48 pp.<br />

Guitjens, J. C. 1982. Models of Alfalfa Yield and Evapotranspiration,. Journal of<br />

the Irrigation and Drainage Division, Proceedings of the American<br />

Society of Civil Engineers. 108(IR3), pp. 212–222.<br />

Harbeck Jr., G. E.1962. A Practical Field Technique for Measuring Reservoir<br />

Evaporation Utilizing Mass-transfer Theory. U.S. Geol. Surv., Paper<br />

272-E, pp. 101–105.<br />

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significance to the science and practice of hydrology. Journal of<br />

Hydrology, 66, 1-76.<br />

Penman, H. L. 1948. Natural Evaporation from Open Water, Bare Soil and Grass.<br />

Proc., Royal Soc., London 193, 120–145.<br />

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Flux and Evaporation using Large-scale Parameters. Monthly Weather<br />

Review 100, 81–92.<br />

Thornthwaite, C.W., 1948, An approach toward a rational classification of<br />

climate: Geographical Review, v. 38, p. 55–94.<br />

Weiß, M. and Menzel, L. A global comparison of four potential<br />

evapotranspiration equations and their relevance to stream flow<br />

modelling in semi-arid environments. Adv. Geosci., 18, 15-23, 2008.<br />

Xu, C.-Y. and Singh, V. P. 2002. Cross Comparison of Empirical Equations for<br />

calculating Potential Evapotranspiration with Data from Switzerland<br />

Water Resources Management 16: 197–219, 2002.<br />

Request 22c Explain why only one estimate or calculation of AET (314 mm) was used to<br />

represent both sides of the Athabasca <strong>River</strong>, given that <strong>Pierre</strong> <strong>River</strong> (with 374<br />

mm precipitation annually) differs appreciably (by 59 mm) from Jackpine (433<br />

mm). Different precipitation regimes can also be manifested in variations among<br />

other climate characteristics including those that may play a role in the<br />

calculation or estimation of AET; such parameters can include differences in<br />

cloud covers and insolation, vapour pressure deficits, and boundary layer<br />

conditions. Provide an explanation that addresses this particular concern<br />

related to AET determination.<br />

April 2010 Shell Canada Limited 12-25<br />

CR029

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