Gross Evaporation Calculations and Database Presentation at PPWB Prairie Hydrology Workshop January 29, 2013.

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Presentation transcript:

Gross Evaporation Calculations and Database Presentation at PPWB Prairie Hydrology Workshop January 29, 2013

Overview Why is gross evaporation data required by the PPWB? How is Gross Evaporation Calculated? The Meyer Formula The Future?

Why is gross evaporation data required by the PPWB? Net evaporative losses from reservoirs are considered a consumptive use in calculating net depletion to natural flow for apportionment monitoring purposes Various methods are currently used: Meyer Formula – Lake Diefenbaker, Reid Lake, Tobin Lake, St. Mary Reservoir, Waterton Reservoir, Moosomin Reservoir, Pipestone Lake Morton’s Model – Glennifer Lake Penman’s (recently replaced Evaporation Pan station) – Lodge, Middle and Battle Creek basins Various attempts over the years to assess the most appropriate methodology for computing gross evaporation for operational needs Discussion in PPWB Report No. 162 (Hopkinson, 2003)

How is Gross Evaporation Calculated? Mass Transfer Energy Budget Water Budget Empirical Formulae (Meyer, Penman, etc.) Direct Measurement (pan)

Use of the Meyer Formula on the Canadian Prairies 1962 study by McKay and Stichling on Weyburn Reservoir compared seven methods for evaporation determination including water budget, energy budget, pan and empirical formulae Recommended the Meyer Formula for operational purposes because of data availability and simplicity PPWB used the Meyer Formula to estimate gross evaporation for the period 1921 to 1950 at 15 locations (PPWB Report No. 5, 1952) SNBB used the Meyer Formula to calculate gross evaporation for the period 1912 to 1967 at 17 locations PFRA refined the Meyer Formula for Prairie conditions and published updated data (Hydrology Reports #113, 121, 133 and 143) Data and maps are widely distributed and are used by federal and provincial governments, consultants and academia in the Canadian Prairies

Meyer Formula Requires only monthly: Air Temperature Wind Speed Dew Point Temperature or Relative Humidity Water temperature data is estimated from air temperature as: TW = 0.60TA + B where:TW=monthly mean surface water temperature, in oC, TA=monthly mean air temperature, in oC, and B=intercept value corresponding to the month under consideration and location

Meyer Formula

What Does the Future Hold? Report with monthly gross evaporation data updated to 2010 and new 30-year average maps (1980 to 2010) for gross evaporation and precipitation will be completed soon. ??????? – PFRA no longer exists, and there is no mandate in the current organization to continue gross evaporation updates.