Showing 1 - 4 results of 4 for search '"Torngat Mountains"', query time: 0.16s Refine Results
  1. 1

    Recent changes in area and thickness of Torngat Mountain glaciers (northern Labrador, Canada) by N. E. Barrand, R. G. Way, T. Bell, M. J. Sharp

    Published 2017-01-01
    “…The Torngat Mountains National Park, northern Labrador, Canada, contains more than 120 small glaciers: the only remaining glaciers in continental northeast North America. …”
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  2. 2

    Rapid Ecosystem Change at the Southern Limit of the Canadian Arctic, Torngat Mountains National Park by Emma L. Davis, Andrew J. Trant, Robert G. Way, Luise Hermanutz, Darroch Whitaker

    Published 2021-05-01
    “…In the low Arctic, Torngat Mountains National Park (TMNP) of Canada, widespread greening has recently occurred alongside warming temperatures and regional declines in caribou. …”
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  3. 3

    Shallow subtidal marine benthic communities of Nachvak Fjord, Nunatsiavut, Labrador: A glimpse into species composition and drivers of their distribution. by Alan M Friedlander, Enric Ballesteros, Alyssa M Adler, Whitney Goodell, Ryan Jenkinson, Jennie A Knopp, Christopher D H Thompson, Molly Timmers, Cameron A J Walsh, Enric Sala

    Published 2023-01-01
    “…Here we conducted the first quantitative underwater scuba surveys, down to 12 m, of the nearshore marine ecology of Nachvak Fjord, which is surrounded by Torngat Mountains National Park located in Nunatsiavut, the Indigenous lands claim region of northeastern Canada. …”
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  4. 4

    Elevation-Dependent Changes to Plant Phenology in Canada’s Arctic Detected Using Long-Term Satellite Observations by Wenjun Chen, Lori White, Sylvain G. Leblanc, Rasim Latifovic, Ian Olthof

    Published 2021-09-01
    “…We found that the start of the growing season (SOS) became earlier faster with an increasing elevation over mountainous study areas (i.e., Sirmilik, the Torngat Mountains, and Ivvavik National Parks). Similarly, the changes rates in the end of growing season (EOS) and the growing season length (GSL) were also higher at high elevations. …”
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