| Title | [The Arctic:] terrestrial permafrost |
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| Author | Romanovsky, V E; Smith, S L ; Isaksen, K; Shiklomanov, N I; Streletskiy, D A; Kholodov, A L; Christiansen, H H; Drozdov, D S; Malkova, G V; Marchenko, S S |
| Source | State of the climate in 2018; by Blunden, J (ed.); Arndt, D S (ed.); Bulletin of the American Meteorological Society vol. 100, no. 9, 2019 p. S153-S156, https://doi.org/10.1175/2019BAMSStateoftheClimate.1  Open Access |
| Links | Online - En ligne
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| Image |  |
| Year | 2019 |
| Alt Series | Natural Resources Canada, Contribution Series 20190050 |
| Publisher | American Meteorological Society |
| Document | serial |
| Lang. | English |
| Media | paper; on-line; digital |
| Province | Northwest Territories; Nunavut; Yukon |
| NTS | 15; 16; 25; 26; 27; 28; 29; 35; 36; 37; 38; 39; 45; 46; 47; 48; 49; 55; 56; 57; 58; 59; 65; 66; 67; 68; 69; 75; 76; 77; 78; 79; 85; 86; 87; 88; 89; 95; 96; 97; 98; 99; 105; 106; 107; 115; 116; 117; 120; 340;
560 |
| Area | Arctic; Canada; United States of America; Russian Federation; Svalbard and Jan Mayen; Norway; Finland; Sweden; Greenland; Denmark |
| Lat/Long WENS | -180.0000 180.0000 90.0000 60.0000 |
| Subjects | surficial geology/geomorphology; environmental geology; Nature and Environment; permafrost; ground ice; climate, arctic; climate effects; ground temperatures; planning; Global Terrestrial Network for
Permafrost; Climate change; Northern development; Decision making; Climate change adaptation; International cooperation |
| Illustrations | geoscientific sketch maps; tables; time series |
| Program | Climate Change
Geoscience Permafrost |
| Released | 2019 08 01 |
| Summary | (Plain Language Summary, not published)
This article is the permafrost contribution to the 'State of the Climate (2018)', an annual peer-reviewed report providing clear, reliable information on
the current state of the Arctic environmental system relative to historical records. Information acquired from the Global Terrestrial Network for Permafrost (to which Canada contributes) indicates that permafrost continues to warm across the
circumpolar region and in some regions such as the Canadian High Arctic the permafrost temperatures are the highest they have been in the past 3-4 decades. Since permafrost is an important component of the northern landscape, knowledge of how
conditions are changing is essential for planning adaptation to a changing climate and to support decisions regarding northern development. |
| GEOSCAN ID | 314658 |
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