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The purpose of this Traditional Knowledge (TK) research is to document important habitat characteristics of the selected focal fish and wildlife species based on the observations of traditional land users. The information may be used to develop habitat models to show where these specific fish and wildlife habitats occur across the Yukon North Slope. The Traditional Knowledge may also be used to validate other types of habitat mapping or to identify specialized habitats such as movement corridors, denning areas, wintering areas.
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These maps show baseline (1961-1990) average total precipitation and projected change in precipitation for the decades spanning 2010-2039, 2040-2069, and 2070-2099. Precipitation is expressed in both millimeters (mm) and inches (in); projected change in precipitation is expressed as percent of baseline. Baseline results for 1961-1990 are derived from Climate Research Unit (CRU) TS 3.1.01 data and maps for future time periods are based on a composite of projections from five GCMs (CCSM4, GFDL-CM3, GISS-E2-R, IPSL-CM5A-LR, and MRI-CGCM3) under the AR5-RCP 6.0. Data courtesy of Scenarios Network for Alaska and Arctic Planning.
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Average historical total precipitation (inches) in winter (December - February) and projected relative change in total precipitation (% change from baseline) for Northern Alaska. 30-year averages. Handout format. Maps created using the SNAP 5-GCM composite (AR5-RCP 6.0) and CRU TS3.1.01 datasets.
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More than 35,000 lakes larger than 0.01 sq. km. were extracted from an airborne interferometric synthetic aperture radar (IfSAR) derived digital surface model acquired between 2002 and 2006 for the Western Arctic Coastal Plain of northern Alaska. The IfSAR derived lake data layer provides an improvement over previously available datasets for the study area since it is more comprehensive and contemporary. Attributes assigned to the IfSAR-derived lake dataset include: area, lake elevation, elevation in 10, 25, 50, and 100 m buffers around a lake perimeter, the difference in elevation between the lake and these various buffers, whether a particular lake had a detectable drainage gradient exceeding 1.2 m, whether a...
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GIS data are provided for download in geodatabase and shapefile format and contain the following layers: permafrost extent, thermokarst landforms, maximum settlement potential, massive ice, segregated ice, biome, ecoregion, ecological subsection, ecological section, ecological landscape, soil landscape, physiography, lithology, general geology, average elevation (m), and mean annual air temperature (c). ArcGIS layer files are also included in this download.
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These raster datasets are output from the Geophysical Institute Permafrost Lab (GIPL) model and represent simulated active layer thickness (ALT) in meters averaged across a decade. These data were generated by driving the GIPL model with a composite of five GCM model outputs for the A1B emissions scenario. The file name specifies the decade the raster represents. For example, a file named ALT_1980_1989.tif represents the decade spanning 1980-1989. Cell values represent simulated maximum depth (in meters) of thaw penetration (for areas with permafrost) or frost penetration (for areas without permafrost). If the value of the cell is positive, the area is underlain by permafrost and the cell value specifies the depth...
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Potential Evapotranspiration (PET): These data represent decadal mean totals of potential evapotranspiration estimates (mm). The file name specifies the decade the raster represents. For example, a file named pet_mean_mm_decadal_MPI_ECHAM5_A1B_annual_2000-2009.tif represents the decade spanning 2000-2009. The data were generated by using the Hamon equation and output from ECHAM5, a fifth generation general circulation model created by the Max Planck Institute for Meteorology in Hamburg Germany. Data are at 2km x 2km resolution, and all data are stored in geotiffs. Calculations were performed using R 2.12.1 and 2.12.2 for Mac OS Leopard, and data were formatted into geotiffs using the raster and rgdal packages. Users...
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This raster, created in 2010, is output from the Geophysical Institute Permafrost Lab (GIPL) model and represents simulated active layer thickness (ALT) in meters averaged across a decade. The file name specifies the decade the raster represents. For example, a file named ALT_1980_1989.tif represents the decade spanning 1980-1989. Cell values represent simulated maximum depth (in meters) of thaw penetration (for areas with permafrost) or frost penetration (for areas without permafrost). If the value of the cell is positive, the area is underlain by permafrost and the cell value specifies the depth of the seasonally thawing layer above permafrost. If the value of the cell is negative, the ground is only seasonally...
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These raster datasets represent historical stand age. The last four digits of the file name specifies the year represented by the raster. For example a file named Age_years_historical_1990.tif represents the year 1990. Cell values represent the age of vegetation in years since last fire, with zero (0) indicating burned area in that year. Files from years 1860-2006 use a variety of historical datasets for Boreal ALFRESCO model spin up and calibration to most closely match historical wildfire dynamics.
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These raster datasets represent historical stand age. The last four digits of the file name specifies the year represented by the raster. For example a file named Age_years_historical_1990.tif represents the year 1990. Cell values represent the age of vegetation in years since last fire, with zero (0) indicating burned area in that year. Files from years 1860-2006 use a variety of historical datasets for Boreal ALFRESCO model spin up and calibration to most closely match historical wildfire dynamics.
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Webinar 2015: Alaska’s National Hydrography Dataset (NHD), the digital data layer that depicts the location of lakes and streams, was originally created from the 1950’s topographic maps. With funding support from the LCC Network, this project focused on establishing a statewide framework to improve the hydrography mapping and stewardship in Alaska. This will be achieved through the creation of a statewide system to make digital mapping data updates accessible and affordable, and through the creation of a statewide hydrography mapping coordinator position to synchronize updates and guide hydrography mapping development. This framework will allow agencies and organizations to greatly improve their hydrography mapping...
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Beaded streams are widespread in permafrost regionsand are considered a common thermokarst landform.However, little is known about their distribution, how andunder what conditions they form, and how their intriguingmorphology translates to ecosystem functions and habitat.Here we report on a circum-Arctic survey of beaded streamsand a watershed-scale analysis in northern Alaska using remotesensing and field studies.We mapped over 400 channelnetworks with beaded morphology throughout the continuouspermafrost zone of northern Alaska, Canada, and Russiaand found the highest abundance associated with mediumto high ground-ice content permafrost in moderately slopingterrain. In one Arctic coastal plain watershed, beaded...
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These rasters represent output from the Boreal ALFRESCO (Alaska Frame Based Ecosystem Code) model. Boreal ALFRESCO operates on an annual time step, in a landscape composed of 1 x 1 km pixels, a scale appropriate for interfacing with mesoscale climate and carbon models. The last four digits of the file name specifies the year represented by the raster. For example a file named Age_years_historical_1990.tif represents the year 1990. Cell values represent the age of vegetation in years since last fire, with zero (0) indicating burned area in that year. Coverage of this dataset includes much of the state of Alaska (but does exclude Southeastern AK, Kodiak Island, portions of the Alaska Peninsula, and the Aleutian Islands)....
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Average historical total precipitation (inches) in summer (June - August) and projected relative change in total precipitation (% change from baseline) for Northern Alaska. 30-year averages. Handout format. Maps created using the SNAP 5-GCM composite (AR5-RCP 6.0) and CRU TS3.1.01 datasets.
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Permafrost is a unique characteristic of polar regions and high mountains and is fundamentalto geomorphic processes and ecological development in permafrost-affected environments.Because permafrost impedes drainage and ice-rich permafrost settles upon thawing, degradationof permafrost in response to climate change will have large consequences for tundra and borealecosystems (Osterkamp 2005, Jorgenson and Osterkamp 2005, Shur and Osterkamp 2007,Jorgenson et al. 2010, 2013). Thawing permafrost affects surface hydrology by impoundingwater in subsiding areas and enhances drainage of upland areas. Changes in soil drainage altersoil carbon dynamics, habitats for vegetation and wildlife, and emissions of greenhouse gases(Ping...
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Information on the nature and distribution of permafrost is critical to assessing the response of Arctic ecosystems to climate change, because thawing permafrost under a warming climate will cause thaw settlement and affect micro-topography, surface water redistribution and groundwater movement, soil carbon balance, trace gas emissions, vegetation changes, and habitat use. While a small-scale regional permafrost map is available, as well as information from numerous site-specific large-scale mapping projects, landscape-level mapping of permafrost characteristics is needed for regional modeling and climate impact assessments. The project addresses this need by: (1) compiling existing soil/permafrost data from available...
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Understanding snow conditions is key to developing a better understanding of hydrologic, biological, and ecosystem processes at work in northern Alaska. The required snow datasets currently do not exist at spatial or temporal scales needed by end users such as scientists, land managers, and policy makers. There are a wide variety of snow datasets that may be generated by this project. The list of desired datasets will be refined based on input from potential end users. However, outputs could include daily spatial distributions spanning the spatial and temporal domains of interest of the following variables: air temperature, wind speed and direction, relative humidity, surface (skin) temperature, incoming solar radiation,...
Categories: Data, Project; Types: Map Service, OGC WFS Layer, OGC WMS Layer, OGC WMS Service; Tags: AIR TEMPERATURE, AIR TEMPERATURE, ALBEDO, ALBEDO, Academics & scientific researchers, All tags...
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The Arctic, including Alaska, has warmed significantly over the last five decades, withwidespread changes in every region, particularly in Alaska’s Arctic slope, north of the BrooksRange. Prominent changes include changes of ocean temperature, increase in permafrosttemperature in many regions, warmer winter seasons, with longer and warmer snow-freeseasons, warmer freshwater temperatures, movement of plant and wildlife species previouslyfound in more southern regions of Alaska into the Arctic slope region, changes in summer andwinter ranges of terrestrial mammal species, and the extension of more southern host specieswith their zoonotic pathogens into more northern regions of Alaska and Canada. These changeshave...
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ire-induced permafrost degradation is well documented in boreal forests, but the role of fires in initiating thermokarst development in Arctic tundra is less well understood. Here we show that Arctic tundra fires may induce widespread thaw subsidence of permafrost terrain in the first seven years following the disturbance. Quantitative analysis of airborne LiDAR data acquired two and seven years post-fire, detected permafrost thaw subsidence across 34% of the burned tundra area studied, compared to less than 1% in similar undisturbed, ice-rich tundra terrain units. The variability in thermokarst development appears to be influenced by the interaction of tundra fire burn severity and near-surface, ground-ice content....
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The Yukon North Slope (YNS) has been and remains a core hunting territory of the Inuvialuit of the Canadian Western Arctic. From their communities in Aklavik and Inuvik in the Northwest Territories, the Inuvialuit rely on the Yukon North Slope for their subsistence livelihood. They travel by boat, foot, allterrain vehicle or skidoo to hunt, trap and fish along the coast, foothills and mountains of the Yukon North Slope (YNS). The Inuvialuit Final Agreement (IFA) was legislated in 1984 and confirms the management priority for the YNS is the conservation of the land, waters, wildlife and Inuvialuit traditional use. To assist in delivering on this management priority, the IFA established the Wildlife Management Advisory...


map background search result map search result map SNOWDATA: Snow Datasets for Arctic Terrestrial Applications (Alaska Arctic LCC Distributed Snow Property Datasets) Winter Precipitation Maps - RCP 6.0, Inches Summer Precipitation Maps - RCP 6.0, Inches Northern Alaska Landscape/Permafrost GIS files Research Description and Data Collection Manual for the Collection of Traditional Knowledge of the Yukon North Slope Traditional Land Users Distribution and biophysical processes of beaded streams in Arctic permafrost landscapes Inuvialuit Traditional Knowledge of Wildlife Habitat on the Yukon North Slope 2015 Webinar: Bringing Alaska's Freshwater Hydrography into the 21st Century Simulated Active Layer Thickness Stand Age Projections 2020-2029 Potential Evapotranspiration 2070-2079: ECHAM5 - A1B Scenario Western Arctic Coastal Plain, IfSAR DSM Mosaic RAMP Final Report Recent Arctic tundra fire initiates widespread thermokarst development Precipitation Projection Maps - RCP 6.0 Historical Stand Age 2000-2006 Active Layer Thickness 1980-1989 Historical Stand Age 1890-1899 Permafrost Database Development, Characterization, and Mapping for Northern Alaska Permafrost Characterization and Mapping for Northern Alaska Final Report Distribution and biophysical processes of beaded streams in Arctic permafrost landscapes Western Arctic Coastal Plain, IfSAR DSM Mosaic Recent Arctic tundra fire initiates widespread thermokarst development Northern Alaska Landscape/Permafrost GIS files Permafrost Database Development, Characterization, and Mapping for Northern Alaska Permafrost Characterization and Mapping for Northern Alaska Final Report Research Description and Data Collection Manual for the Collection of Traditional Knowledge of the Yukon North Slope Traditional Land Users Inuvialuit Traditional Knowledge of Wildlife Habitat on the Yukon North Slope SNOWDATA: Snow Datasets for Arctic Terrestrial Applications (Alaska Arctic LCC Distributed Snow Property Datasets) RAMP Final Report Simulated Active Layer Thickness Stand Age Projections 2020-2029 Potential Evapotranspiration 2070-2079: ECHAM5 - A1B Scenario Historical Stand Age 2000-2006 Active Layer Thickness 1980-1989 Historical Stand Age 1890-1899 2015 Webinar: Bringing Alaska's Freshwater Hydrography into the 21st Century Winter Precipitation Maps - RCP 6.0, Inches Summer Precipitation Maps - RCP 6.0, Inches Precipitation Projection Maps - RCP 6.0