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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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mdEditorWeb application for writing metadata. Built using ember.js.See CONTRIBUTING.md for info on making contributions.Also, see the wiki for more info about the project.Prerequisites (for development)You will need the following things properly installed on your computer. Git Node.js (with NPM) Bower Ember CLI PhantomJSInstallation git clone https://github.com/adiwg/mdEditor.git this repository cd mdEditor change into the new directory npm install bower installRunning / Development ember server Visit your app at http://localhost:4200.Code GeneratorsMake use of the many generators for code, try ember help generate for more detailsRunning Tests ember test ember test --serverBuilding ember build (development) ember...
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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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mdEditorWeb application for writing metadata. Built using ember.js.See CONTRIBUTING.md for info on making contributions.Also, see the wiki for more info about the project.Prerequisites (for development)You will need the following things properly installed on your computer. Git Node.js (with NPM) Bower Ember CLI PhantomJSInstallation git clone https://github.com/adiwg/mdEditor.git this repository cd mdEditor change into the new directory npm install bower installRunning / Development ember server Visit your app at http://localhost:4200.Code GeneratorsMake use of the many generators for code, try ember help generate for more detailsRunning Tests ember test ember test --serverBuilding ember build (development) ember...
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Baseline (1961-1990) average summer total precipitation and projected change in precipitation for the northern portion of Alaska. For the purposes of these maps, ‘summer’ is defined as June - August. The Alaska portion of the Arctic LCC’s terrestrial boundary is depicted by the black line. Baseline results for 1961-1990 are derived from Climate Research Unit (CRU) TS 3.1.01 data and downscaled to 2km grids; results for the other time periods (2010-2039, 2040-2069, 2070-2099) are based on the SNAP 5-GCM composite using the AR5-RCP 8.5, downscaled to 2km grids.
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Baseline (1961-1990) average winter temperature in and projected change in temperature for for the northern portion of Alaska. For the purposes of these maps, ‘winter’ is defined as December - February. The Alaska portion of the Arctic LCC’s terrestrial boundary is depicted by the black line. Baseline results for 1961-1990 are derived from Climate Research Unit (CRU) TS3.1 data and downscaled to 2km grids; results for the other time periods (2010-2039, 2040-2069, 2070-2099) are based on the SNAP 5-GCM composite using the AR5-RCP 8.5, downscaled to 2km grids.
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Average historical total precipitation (mm) 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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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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Final report detailing the results of the climate change vulnerability assessment conducted by the Wildlife Conservation Society.The specific goals of this assessment were to: provide a climate change vulnerability ranking for selected Arctic Alaskan breeding bird species; evaluate the relative contribution of specific sensitivity and exposure factors to individual species rankings; consider how this assessment may be integrated with other approaches; and appraise the effectiveness of the NatureServe Climate Change Vulnerability Index (CCVI) tool.
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Baseline (1961-1990) average summer total precipitation and projected change in precipitation for the northern portion of Alaska. For the purposes of these maps, ‘summer’ is defined as June - August. The Alaska portion of the Arctic LCC’s terrestrial boundary is depicted by the black line. Baseline results for 1961-1990 are derived from Climate Research Unit (CRU) TS 3.1.01 data and downscaled to 2km grids; results for the other time periods (2010-2039, 2040-2069, 2070-2099) are based on the SNAP 5-GCM composite using the AR5-RCP 8.5, downscaled to 2km grids.
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This raster, created in 2010, is output from the Geophysical Institute Permafrost Lab (GIPL) model and represents simulated mean annual ground temperature (MAGT) in Celsius, averaged across a decade, at the base of active layer or at the base of the seasonally frozen soil column. The file name specifies the decade the raster represents. For example, a file named MAGT_1980_1989.tif represents the decade spanning 1980-1989. Cell values represent simulated mean annual ground temperature (degree C) at the base of the active layer (for areas with permafrost) or at the base of the soil column that is seasonally frozen (for areas without permafrost). If the value of the cell is negative,the area has permafrost and the...
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Researchers from the University of Alaska (UAF), The NatureConservancy, and U.S. Fish and Wildlife Service will use‘climate envelope’ models (i.e., models that infer a species’environmental requirements from locations where they arecurrently found) to explore how patterns in temperature,precipitation, and landcover (i.e., climate-biomes) may shift as aresult of changing climate.
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This data set represents an updated Ecological Subsection Map for Northern Alaska. This 2012 revision focused on completing the incompletely mapped portion of the southern NPRA, improving mapping of glacial and outwash deposits within the Brooks Foothills, and improving consistency with existing surficial and bedrock geology maps in northern Alaska. The revisions resulted in 525 ecological subsections, nested within 55 ecosections and 12 ecoregions covering 411,781 km2. Attributes for the polygons include information on physiography, generalized geology, lithology, and referenced information sources. Description of attributes is provided in the map documentation report. The dataset can be downloaded from catalog.northslope.org
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Baseline (1961-1990) average winter temperature in and projected change in temperature for for the northern portion of Alaska. For the purposes of these maps, ‘winter’ is defined as December - February. The Alaska portion of the Arctic LCC’s terrestrial boundary is depicted by the black line. Baseline results for 1961-1990 are derived from Climate Research Unit (CRU) TS3.1 data and downscaled to 2km grids; results for the other time periods (2010-2039, 2040-2069, 2070-2099) are based on the SNAP 5-GCM composite using the AR5-RCP 8.5, downscaled to 2km grids.
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Baseline (1961-1990) average winter temperature in and projected change in temperature for for the northern portion of Alaska. For the purposes of these maps, ‘winter’ is defined as December - February. The Alaska portion of the Arctic LCC’s terrestrial boundary is depicted by the black line. Baseline results for 1961-1990 are derived from Climate Research Unit (CRU) TS3.1 data and downscaled to 2km grids; results for the other time periods (2010-2039, 2040-2069, 2070-2099) are based on the SNAP 5-GCM composite using the AR5-RCP 8.5, downscaled to 2km grids.
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Rural Arctic communities are vulnerable to climate change and residents seek adaptive strategies that will protect public health. In the Inupiat community of Selawik, climate change is impacting the weather, land, river, wildlife, plants, and the lives of the people who live there. This report identifies health concerns related to food and water security and community infrastructure. This report documents these issues as described by the local people and interpreted through the lens of public health. It is the fifth report in a series describing climate change in Northwest Alaska.
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The USGS St. Petersburg Coastal and Marine Science Center (USGS St. Pete) processed lidar topographic data in Alaska. Raw lidar data are not in a format that is generally usable by resource managers and scientists for scientific analysis. Converting dense lidar elevation data into a readily usable format without loss of essential information requires specialized processing. Project included processing of lidar data acquired in Summer 2010 along the North Slope of Alaska between Colville River and Hulahula River.
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These data are the result of a geospatial analysis involving multi-year SAR-based lake ice regime classification using sigma-naught backscatter intensity from calibrated space-borne C-band SAR for thousands of lakes in 7 lake districts in Alaska, USA, detailed in Engram et al., (in review). Historically, radar backscatter from space-borne and airborne platforms shows a lower backscatter return from bedfast lake ice and a higher backscatter return from floating ice (where liquid phase water exists under the ice) (Jeffries, Morris, Weeks, & Wakabayashi, 1994; Weeks, 1977). We used a threshold method where the threshold to differentiate floating and bedfast ice regimes was determined for each year from the frequency...


map background search result map search result map Map Edited Imported from SB Arctic LCC Alaskan Boundary Map, Satellite Summer Precipitation Maps - RCP 6.0, Millimeters Changing Climate-Biomes Model factsheet Mean Annual Ground Temperature 2010-2019 Summer Temperature Maps - RCP 6.0, Celsius Barrow/Meade River Watershed map Ecological Subsections for Northern Alaska 2012, shapefile and report Winter Temperature Maps - RCP 6.0, Celsius Annual Temperature Maps - RCP 8.5, Celsius Assessing Climate Change Vulnerability of Breeding Birds in Arctic Alaska Climate Change in Selawik, Alaska.  Strategies for Community Health Summer Precipitation Maps - RCP 8.5, Millimeters Historical Stand Age 1990-1999 Summer Precipitation Maps - RCP 8.5, Inches Lake Ice Regime Classification Alaska LiDAR Data Processing - Colville to Staines River Permafrost Characterization and Mapping for Northern Alaska Final Report Permafrost Characterization and Mapping for Northern Alaska Final Report Alaska LiDAR Data Processing - Colville to Staines River Imported from SB Barrow/Meade River Watershed map Map Edited Lake Ice Regime Classification Arctic LCC Alaskan Boundary Map, Satellite Ecological Subsections for Northern Alaska 2012, shapefile and report Assessing Climate Change Vulnerability of Breeding Birds in Arctic Alaska Permafrost Characterization and Mapping for Northern Alaska Final Report Permafrost Characterization and Mapping for Northern Alaska Final Report Changing Climate-Biomes Model factsheet Climate Change in Selawik, Alaska.  Strategies for Community Health Mean Annual Ground Temperature 2010-2019 Historical Stand Age 1990-1999 Summer Precipitation Maps - RCP 6.0, Millimeters Summer Temperature Maps - RCP 6.0, Celsius Winter Temperature Maps - RCP 6.0, Celsius Annual Temperature Maps - RCP 8.5, Celsius Summer Precipitation Maps - RCP 8.5, Millimeters Summer Precipitation Maps - RCP 8.5, Inches