Open Government Portal

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.

The purpose of the field survey of commercial premises is to develop a portrait of street commerce on the territory of the Montréal agglomeration in order to identify the premises intended for the practice of an economic activity (excluding industrial and institutional activities). This dataset makes it possible in particular to measure the occupancy status of commercial premises, to follow the evolution of street commerce as well as to produce various analyses and thematic maps.**This third party metadata element was translated using an automated translation tool (Amazon Translate).**

The Natural Environment Management Plan (MMP) identifies the space for which the City of Lévis has conservation goals.**This third party metadata element was translated using an automated translation tool (Amazon Translate).**

Administrative boundaries of the sectors of the city of Lévis. The sectors correspond to the boundaries of the former municipalities before the merger in 2001.**This third party metadata element was translated using an automated translation tool (Amazon Translate).**

Geographic database containing the result of Statistics Canada's __2021 Census Geography Harmonization Process__. Harmonization is a process of editing geographic boundaries with the aim of spatially adjusting them to the official geographic base. This work was carried out in 2022 by the Institut de la Statistique du Québec (ISQ) according to the official provincial geographical base. A metadata sheet presents the process of harmonizing this geography. __The contents of the resulting database are detailed (page 2), as well as the description of the attributes in the appendix (pages 7 to 11) __.**This third party metadata element was translated using an automated translation tool (Amazon Translate).**

Territorial representation of day and night surface temperatures for planning, consultation and management purposes.**This third party metadata element was translated using an automated translation tool (Amazon Translate).**

Permafrost loss is pervasive across northern circumpolar regions. The loss of frozen ground has profound impacts on water resources at varying spatial and temporal scales via changes to predominant hydrological processes, runoff pathways and entrainment rates of solutes and sediments. Consensus exists that permafrost loss will continue, and rates will vary spatially, but how hydrology and biogeochemistry will respond across large swaths of land remains largely unknown. Previous research elucidated small-scale processes or described circumpolar trends, with minimal cross-scale research.