| Title | Reconstructed changes in Arctic sea ice over the past 1,450 years |
| Author | Kinnard, C; Zdanowicz, C M; Fisher, D A; Isaksson, E; de Vernal, A; Thompson, L G |
| Source | Nature vol. 479, 2011 p. 509-513, https://doi.org/10.1038/nature10581 |
| Year | 2011 |
| Alt Series | Earth Sciences Sector, Contribution Series 20110321 |
| Document | serial |
| Lang. | English |
| Media | paper; on-line; digital |
| File format | pdf |
| Province | Northern offshore region |
| Area | Arctic Ocean; Kara- Barents Sea; Greenland Sea; Baffin Bay; Davis Strait; Canadian Arctic; Hudson Bay |
| Lat/Long WENS | -180.0000 180.0000 90.0000 60.0000 |
| Subjects | surficial geology/geomorphology; environmental geology; sea ice; ice; ice conditions; massive ice; climate, arctic |
| Illustrations | location maps; graphs; plots |
| |
| Program | Paleoenvironmental Perspectives on Climate Change, Climate Change Geoscience |
| Released | 2011 11 24 |
| Abstract | Arctic sea ice extent is nowmore than twomillion square kilometres less than it was in the late twentieth century, with important consequences for the climate, the ocean and traditional lifestyles in
the Arctic1,2. Although observations show a more or less continuous decline for the past four or five decades3,4, there are few long-term records withwhich to assess natural sea ice variability. Until now, the question of whether or not current
trends are potentially anomalous5 has therefore remained unanswerable. Here we use a network of high-resolution terrestrial proxies from the circum-Arctic region to reconstruct past extents of summer sea ice, and show that - although extensive
uncertainties remain, especially before the sixteenth century - both the duration and magnitude of the current decline in sea ice seem to be unprecedented for the past 1,450 years. Enhanced advection of warm Atlantic water to the Arctic6 seems to be
the main factor driving the decline of sea ice extent on Multidecadal timescales, and may result from nonlinear feedbacks between sea ice and the Atlantic meridional overturning circulation. These results reinforce the assertion that sea ice is an
active component of Arctic climate variability and that the recent decrease in summer Arctic sea ice is consistent with anthropogenically forced warming. |
| GEOSCAN ID | 289695 |
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