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First- and second-generation agrometeorological models for the prairies and simulated water-demand for potatoes
On the Canadian prairies, moisture is usually the limiting factor in crop production. Occasionally, the thermal regime limits yields. At the Winnipeg Climate Centre, Environment Canada, a root-zone water-balance model simulates crop development, water-demand and water-use with daily climatological o...
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Published in: | Canadian journal of soil science 1996-08, Vol.76 (3), p.297-305 |
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container_title | Canadian journal of soil science |
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creator | Raddatz, R.L Ash, G.H.B Shaykewich, C.F Roberge, K.A Graham, J.L |
description | On the Canadian prairies, moisture is usually the limiting factor in crop production. Occasionally, the thermal regime limits yields. At the Winnipeg Climate Centre, Environment Canada, a root-zone water-balance model simulates crop development, water-demand and water-use with daily climatological observations from across the agricultural portion of the Canadian Prairie Provinces. Simulations are used for regional-scale monitoring of the prairie’s major crops (spring wheat, barley and canola) and they have been used to quantify climatological risks. This agrometeorological model is termed a first-generation model as potential evapotranspiration is estimated empirically from Baier and Robertson’s simplest regression equation.A coupled atmosphere-crop-soil agrometeorological model has also been developed for crop monitoring on the prairies. This model generates atmospheric boundary layer profiles at climatological-sites using upper-air analyses and surface characteristics. The crop-soil boundary layer consists of the growing crop, and the top, root and sub-zones of the soil. Evapotranspiration is calculated deterministically from the air’s water vapour density deficit. The calculation is modulated by aerodynamic, canopy and soil resistances. The coupled approach is termed a second-generation model.The re-formulation of the coupled model to simulate the phenology and water-demand of a newly significant crop, potatoes, is described. Comparison with 1994 and 1995 test-plot observations of fractional leaf area and rooting depth suggests that the potato phenology simulation requires further development. Estimates of daily crop water-demand are similar but show greater day-today variation than values generated by a first-generation Baier and Robertson procedure. Key words: Regional modelling, soil moisture, phenology, crop water-demand, potatoes |
doi_str_mv | 10.4141/cjss96-036 |
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Occasionally, the thermal regime limits yields. At the Winnipeg Climate Centre, Environment Canada, a root-zone water-balance model simulates crop development, water-demand and water-use with daily climatological observations from across the agricultural portion of the Canadian Prairie Provinces. Simulations are used for regional-scale monitoring of the prairie’s major crops (spring wheat, barley and canola) and they have been used to quantify climatological risks. This agrometeorological model is termed a first-generation model as potential evapotranspiration is estimated empirically from Baier and Robertson’s simplest regression equation.A coupled atmosphere-crop-soil agrometeorological model has also been developed for crop monitoring on the prairies. This model generates atmospheric boundary layer profiles at climatological-sites using upper-air analyses and surface characteristics. The crop-soil boundary layer consists of the growing crop, and the top, root and sub-zones of the soil. Evapotranspiration is calculated deterministically from the air’s water vapour density deficit. The calculation is modulated by aerodynamic, canopy and soil resistances. The coupled approach is termed a second-generation model.The re-formulation of the coupled model to simulate the phenology and water-demand of a newly significant crop, potatoes, is described. Comparison with 1994 and 1995 test-plot observations of fractional leaf area and rooting depth suggests that the potato phenology simulation requires further development. Estimates of daily crop water-demand are similar but show greater day-today variation than values generated by a first-generation Baier and Robertson procedure. 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Occasionally, the thermal regime limits yields. At the Winnipeg Climate Centre, Environment Canada, a root-zone water-balance model simulates crop development, water-demand and water-use with daily climatological observations from across the agricultural portion of the Canadian Prairie Provinces. Simulations are used for regional-scale monitoring of the prairie’s major crops (spring wheat, barley and canola) and they have been used to quantify climatological risks. This agrometeorological model is termed a first-generation model as potential evapotranspiration is estimated empirically from Baier and Robertson’s simplest regression equation.A coupled atmosphere-crop-soil agrometeorological model has also been developed for crop monitoring on the prairies. This model generates atmospheric boundary layer profiles at climatological-sites using upper-air analyses and surface characteristics. The crop-soil boundary layer consists of the growing crop, and the top, root and sub-zones of the soil. Evapotranspiration is calculated deterministically from the air’s water vapour density deficit. The calculation is modulated by aerodynamic, canopy and soil resistances. The coupled approach is termed a second-generation model.The re-formulation of the coupled model to simulate the phenology and water-demand of a newly significant crop, potatoes, is described. Comparison with 1994 and 1995 test-plot observations of fractional leaf area and rooting depth suggests that the potato phenology simulation requires further development. Estimates of daily crop water-demand are similar but show greater day-today variation than values generated by a first-generation Baier and Robertson procedure. 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Occasionally, the thermal regime limits yields. At the Winnipeg Climate Centre, Environment Canada, a root-zone water-balance model simulates crop development, water-demand and water-use with daily climatological observations from across the agricultural portion of the Canadian Prairie Provinces. Simulations are used for regional-scale monitoring of the prairie’s major crops (spring wheat, barley and canola) and they have been used to quantify climatological risks. This agrometeorological model is termed a first-generation model as potential evapotranspiration is estimated empirically from Baier and Robertson’s simplest regression equation.A coupled atmosphere-crop-soil agrometeorological model has also been developed for crop monitoring on the prairies. This model generates atmospheric boundary layer profiles at climatological-sites using upper-air analyses and surface characteristics. The crop-soil boundary layer consists of the growing crop, and the top, root and sub-zones of the soil. Evapotranspiration is calculated deterministically from the air’s water vapour density deficit. The calculation is modulated by aerodynamic, canopy and soil resistances. The coupled approach is termed a second-generation model.The re-formulation of the coupled model to simulate the phenology and water-demand of a newly significant crop, potatoes, is described. Comparison with 1994 and 1995 test-plot observations of fractional leaf area and rooting depth suggests that the potato phenology simulation requires further development. Estimates of daily crop water-demand are similar but show greater day-today variation than values generated by a first-generation Baier and Robertson procedure. Key words: Regional modelling, soil moisture, phenology, crop water-demand, potatoes</abstract><doi>10.4141/cjss96-036</doi><tpages>9</tpages><oa>free_for_read</oa></addata></record> |
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subjects | agrometeorology phenology plant-water relations prairie soils simulation simulation models soil water balance Solanum tuberosum temporal variation water requirements water use |
title | First- and second-generation agrometeorological models for the prairies and simulated water-demand for potatoes |
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