New paper finds Arctic sea ice extent has increased over the last few centuries
A new paper published in Quaternary Science Reviews finds that reconstructed Arctic sea ice extent has increased over the last few centuries. According to the authors, the only sea ice proxy "records having a resolution suitable to document sea ice cover variations over the last centuries" find that "all records show an increase of the sea ice cover over the last centuries" and "a distinct trend for an increased sea ice cover towards modern values over the last centuries."
Excerpt:
"Records having a resolution suitable to document sea ice cover variations over the last centuries have been obtained from the Mackenzie slope, the Beaufort Sea (Richerol et al., 2008; Bringué and Rochon, 2012; Durantou et al., 2012), and the Chukchi Shelf (core B5; de Vernal et al., 2008; Kinnard et al., 2011). At the Beaufort Sea sites, the variations are of limited amplitude and the estimates are close to “modern” observations, but all records show an increase of the sea ice cover over the last centuries. At the Chukchi site, the record shows large amplitude variations with a distinct trend for an increased sea ice cover towards modern values over the last centuries."
Dinocyst-based reconstructions of sea ice cover concentration during the Holocene in the Arctic Ocean, the northern North Atlantic Ocean and its adjacent seas
Anne de Vernal et al
Sea ice cover extent expressed in terms of mean annual concentration was reconstructed from the application of the modern analogue technique to dinocyst assemblages. The use of an updated database, which includes 1492 sites and 66 taxa, yields sea ice concentration estimates with an accuracy of 1.1/10. Holocene reconstructions of sea ice cover were made from dinocyst counts in 35 cores of the northern North Atlantic and Arctic seas. In the Canadian Arctic, the results show high sea ice concentration (>7/10) with little variations throughout the interval. In contrast, in Arctic areas such as the Chukchi Sea and the Barents Sea, the reconstructions show large amplitude variations of sea ice cover suggesting millennial type oscillations with a pacing almost opposite in western vs. eastern Arctic. Other records show tenuous changes with some regionalism either in trends or sea ice cover variability. During the mid-Holocene, and notably at 6 0.5 ka, minimum sea ice concentration is recorded in the eastern Fram Strait, northern Baffin Bay and Labrador Sea. However, this minimum cannot be extrapolated at the scale of the Arctic and circum-Arctic. The comparison of recent observations and reconstructions suggests larger variations in the Arctic sea ice cover during the last decades than throughout the Holocene.
2 comments:
Another excerpt from the paper:
Finally, it should be stressed that the sea ice reconstructions
presented in this paper suggest that some areas were marked
by larger differences between the late Holocene as a whole and
the second half of the 20th Century, than at the scale the Holocene.
Thus, the Holocene data further support the studies of
Fauria et al. (2010) and Kinnard et al. (2011) which both led to
conclude that the recent trends in sea ice cover are unprecedented
at the scales of the last millennium.
Bottom line... the Arctic is becoming colder and ice is returning from a previous low point...
Post a Comment
Enter your comment(s) here...