WFS service for befolkning på grunnkretsnivå 2016

WMS

WFS service for befolkningrutenett2016

Cette carte illustre le ratio du prélèvement d’eau douce de surface à l’apport en eau pour le mois d’août 2013, sauf dans les régions de drainage 7, 8, 16, 17 et 18, pour lesquelles on utilise le ratio du prélèvement d’eau du mois d’août à l’apport en eau mensuel minimum à long terme. En ce qui concerne les prélèvements d’eau douce de surface, les données de l’Enquête sur les usines de traitement de l’eau potable de 2013 et de l’Enquête sur l’utilisation industrielle de l’eau de 2013 sont agrégées avec les estimations de l’utilisation de l’eau à des fins agricoles pour 2013, qui sont fondées sur les données de l’Enquête sur l’utilisation de l’eau à des fins agricoles et du rapport intitulé Alberta Irrigation Information. Les données sur l’eau utilisée par l’industrie pétrolière et gazière et les ménages ne provenant pas d’un fournisseur d’eau public sont également exclues.

This service shows the predominant mother tongue in each census division based on English, French or non-official language. The data is from the data table Mother Tongue (10), Age (27) and Sex (3) for the Population of Canada, Provinces and Territories, Census Divisions and Census Subdivisions, 2016 Census - 100% Data, Statistics Canada Catalogue no. 98-400-X2016046. Mother tongue refers to the first language learned at home in childhood and still understood by the person at the time the data was collected. If the person no longer understands the first language learned, the mother tongue is the second language learned. For a person who learned two languages at the same time in early childhood, the mother tongue is the language this person spoke most often at home before starting school. The person has two mother tongues only if the two languages were used equally often and are still understood by the person. For a child who has not yet learned to speak, the mother tongue is the language spoken most often to this child at home. The child has two mother tongues only if both languages are spoken equally often so that the child learns both languages at the same time.

The national agricultural ecumene includes all dissemination areas with 'significant' agricultural activity. Agricultural indicators, such as the ratio of agricultural land on census farms relative to total land area, and total economic value of agricultural production, are used. Regional variations are also taken into account. The ecumene is generalized for small-scale mapping. A new version of the agricultural ecumene was generated every census years (2001, 2006). Previous versions are no longer available.

Aktsomhetsområder for snøskred er en nasjonalt dekkende kartserie som viser potensielt snøskredutsatte områder på oversiktsnivå. Kartene viser potensielle løsneområder og utløpsområder for snøskred.

Data was created or derived from unmanned aerial vehicle (UAV) imagery acquired from a single day survey, July 28th 2016, in Cambridge Bay, Nunavut. Five control points taken from a Global Differential Positioning System were positioned in the corners and the center of the vegetation survey. The following datasets covers 525m2 and was produced by Canada Centre for Remote Sensing /Canada Centre for Mapping and Earth Observation: - UAV Digital Surface Model (DSM) in Cambridge Bay, Nunavut -Vegetation Plot - UAV Orthomosaic of Cambridge Bay, Nunavut - Vegetation Plot - UAV Vegetation Height Model, Cambridge Bay, Nunavut The UAV survey was completed in collaboration with the Canadian High Arctic Research Station (CHARS) for northern vegetation monitoring research. For more information, refer to our current Arctic vegetation research: Fraser et al; ""UAV photogrammetry for mapping vegetation in the low-Arctic"" Arctic Science, 2016, 2(3): 79-102, 10.1139/as-2016-0008 http://www.nrcresearchpress.com/doi/abs/10.1139/AS-2016-0008

Fire weather refers to weather conditions that are conducive to fire. These conditions determine the fire season, which is the period(s) of the year during which fires are likely to start, spread and do sufficient damage to warrant organized fire suppression. The length of fire season is the difference between the start- and end-of-fire-season dates. These are defined by the Canadian Forest Fire Weather Index (FWI; http://cwfis.cfs.nrcan.gc.ca/) start-up and end dates. Start-up occurs when the station has been snow-free for 3 consecutive days, with noon temperatures of at least 12°C. For stations that do not report significant snow cover during the winter (i.e., less than 10 cm or snow-free for 75% of the days in January and February), start-up occurs when the mean daily temperature has been 6°C or higher for 3 consecutive days. The fire season ends with the onset of winter, generally following 7 consecutive days of snow cover. If there are no snow data, shutdown occurs following 7 consecutive days with noon temperatures lower than or equal to 5°C. Historical climate conditions were derived from the 1981–2010 Canadian Climate Normals. Future projections were computed using two different Representative Concentration Pathways (RCP). RCPs are different greenhouse gas concentration trajectories adopted by the Intergovernmental Panel on Climate Change (IPCC) for its fifth Assessment Report. RCP 2.6 (referred to as rapid emissions reductions) assumes that greenhouse gas concentrations peak between 2010-2020, with emissions declining thereafter. In the RCP 8.5 scenario (referred to as continued emissions increases) greenhouse gas concentrations continue to rise throughout the 21st century. Multiple layers are provided. First, the fire season length is shown across Canada for a reference period (1981-2010). Projected fire season length layers are available for the short- (2011-2040), medium- (2041-2070), and long-term (2071-2100) under the RCP 8.5 (continued emissions increases) and, for the long-term (2071-2100), under RCP 2.6 (rapid emissions reductions).

Cette carte montre l'indice de variabilité pour certaines régions de drainage au Canada. La variabilité est mesurée au moyen d’un coefficient de variation (c.v.) qui permet de comparer tous les mois sur une période de 42 ans, et qui permet de mesurer la dispersion ou la variation des valeurs mensuelles d’apport en eau au cours de la période de 1971 à 2013 (et de 1971 à 2012 pour la région de drainage 1). Il s’agit du ratio de l’écart-type à la moyenne ou de l’écart-type divisé par la moyenne avec un c.v. élevé signifiant que les données mensuelles affichent une plus grande variabilité. La variabilité mensuelle n’a pas été calculée pour les régions de drainage 5, 7, 8, 16, 17 et 18 et pour la partie de la région de drainage 25 située au Labrador.