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This table provides the current expenditure forecast for each statutory authority within a department or agency, for which a financial requirement has been identified.
The Riparian Area Assessment of the North Saskatchewan and Battle River Watersheds project focused on assessing riparian habitat along lake, creek, stream and river shorelines. The majority of the shorelines of interest were located within the NSR or Battle River watersheds. however, an additional shoreline was also assessed within municipalities that partially intersect, but are not completely contained within, either the NSR or Battle River watersheds. In addition to assessing new shorelines, an important component of this project was compiling data for shorelines that had been previously assessed in central Alberta using the same assessment methodology.
This downloadable data product includes the federal boundary files from previous census years. Data included are the historical boundary files of the year indicated and should not be considered the most recent official boundaries. Layers in each geodatabase include Economic Regions, Census Divisions, Census Subdivisions, Census Metropolitan Areas and Census Agglomerations, Census Tracts, and Disseminations. Current years for the historical dataset include 1996, 2001, 2006, 2011, and 2016.
This downloadable data product includes the federal boundary files from the most recent census year. The official boundaries are updated every 5 years with the census and should be considered the most recent official boundaries. Layers in each geodatabase include Economic Regions, Census Divisions, Census Subdivisions, Census Metropolitan Areas and Census Agglomerations, Census Tracts, and Dissemination Areas. The current boundaries are from the 2021 Census of population.
Drought is a deficiency in precipitation over an extended period, usually a season or more, resulting in a water shortage that has adverse impacts on vegetation, animals and/or people. The Climate Moisture Index (CMI) was calculated as the difference between annual precipitation and potential evapotranspiration (PET) – the potential loss of water vapour from a landscape covered by vegetation. Positive CMI values indicate wet or moist conditions and show that precipitation is sufficient to sustain a closed-canopy forest. Negative CMI values indicate dry conditions that, at best, can support discontinuous parkland-type forests.