Contrasting changes in surface waters and barrens over the past 60 years for a subarctic forest–tundra site in northern Manitoba based on remote sensing imagery

• Published in: Canadian Journal of Earth Sciences
• Main Authors: Umbanhowar, Charles, Camill, Philip, Edlund, Mark, Geiss, Christoph, Durham, Wesley, Kreger, Dahna, Molano, William, Raskob, Charlie, Stocker, Mary, Tvera, Andrea, Williams, Jordan
• Other Authors: Brodaric, Boyan
• Format: Article in Journal/Newspaper
• Language: English
• Published: Canadian Science Publishing 2013
• Subjects: Arctic; Nejanilini Lake; Arctic Greening; Climate change; Ice; permafrost; Subarctic; Tundra
• Online Access: http://dx.doi.org/10.1139/cjes-2012-0162; http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2012-0162; http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2012-0162

Intensified warming in the Arctic and Subarctic is resulting in a wide range of changes in the extent, productivity, and composition of aquatic and terrestrial ecosystems. Analysis of remote sensing imagery has documented regional changes in the number and area of ponds and lakes as well as expanding cover of shrubs and small trees in uplands. To better understand long-term changes across the edaphic gradient, we compared the number and area of water bodies and dry barrens (>100 m 2 ) between 1956 (aerial photographs) and 2008–2011 (high-resolution satellite images) for eight ∼25 km 2 sites near Nejanilini Lake, Manitoba (59.559°N, 97.715°W). In the modern landscape, the number of water bodies and barrens were similar (1162 versus 1297, respectively), but water bodies were larger (mean 3.1 × 10 4 versus 681 m 2 , respectively) and represented 17% of surface area compared with 0.4% for barrens. Over the past 60 years, total surface area of water did not change significantly (16.7%–17.1%) despite a ∼30% decrease in numbers of small (<1000 m 2 ) water bodies. However, the number and area of barrens decreased (55% and 67%, respectively) across all size classes. These changes are consistent with Arctic greening in response to increasing temperature and precipitation. Loss of small water bodies suggests that wet tundra areas may be drying, which, if true, may have important implications for carbon balance. Our observations may be the result of changes in winter conditions in combination with low permafrost ice content in the region, in part explaining regional variations in responses to climate change.