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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>M. Torre Jorgenson</dc:contributor>
  <dc:contributor>Bruce K. Wylie</dc:contributor>
  <dc:contributor>Shawn J. Nield</dc:contributor>
  <dc:contributor>Kristofer D. Johnson</dc:contributor>
  <dc:contributor>Andrew O. Finley</dc:contributor>
  <dc:creator>Neal J. Pastick</dc:creator>
  <dc:date>2015</dc:date>
  <dc:description>&lt;p&gt;High-latitude regions are experiencing rapid and extensive changes in ecosystem composition and function as&amp;nbsp;the result of increases in average air temperature. Increasing air temperatures have led to widespread thawing&amp;nbsp;and degradation of permafrost, which in turn has affected ecosystems, socioeconomics, and the carbon cycle of&amp;nbsp;high latitudes. Here we overcome complex interactions among surface and subsurface conditions to map nearsurface&amp;nbsp;permafrost through decision and regression tree approaches that statistically and spatially extend field&amp;nbsp;observations using remotely sensed imagery, climatic data, and thematic maps of a wide range of surface and&amp;nbsp;subsurface biophysical characteristics. The data fusion approach generated medium-resolution (30-m pixels)&amp;nbsp;maps of near-surface (within 1 m) permafrost, active-layer thickness, and associated uncertainty estimates&amp;nbsp;throughout mainland Alaska. Our calibrated models (overall test accuracy of ~85%) were used to quantify changes&amp;nbsp;in permafrost distribution under varying future climate scenarios assuming no other changes in biophysical&amp;nbsp;factors. Models indicate that near-surface permafrost underlies 38% of mainland Alaska and that near-surface&amp;nbsp;permafrost will disappear on 16 to 24% of the landscape by the end of the 21st Century. Simulations suggest&amp;nbsp;that near-surface permafrost degradation is more probable in central regions of Alaska than more northerly regions.&amp;nbsp;Taken together, these results have obvious implications for potential remobilization of frozen soil carbon&amp;nbsp;pools under warmer temperatures. Additionally, warmer and drier conditions may increase fire activity and&amp;nbsp;severity, which may exacerbate rates of permafrost thaw and carbon remobilization relative to climate alone.&amp;nbsp;The mapping of permafrost distribution across Alaska is important for land-use planning, environmental assessments,&amp;nbsp;and a wide-array of geophysical studies.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.rse.2015.07.019</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Distribution of near-surface permafrost in Alaska: estimates of present and future conditions</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>