However, July conditions greatly
reduced sea ice drift speed in the Beaufort Sea and produced a counterclockwise drift pattern in the Laptev Sea (Figure 5a, bottom).
Not exact matches
... The dominance of summer anticyclonic circulation over the Arctic and the
reduced SIE over eastern Siberia and the north of Alaska were similar to the results of Ogi et al. (2008), who demonstrated that the dramatic changes in Arctic SIE in 2007 were produced by [wind - driven] Ekman
drift of
sea ice out of the marginal
seas to the central Arctic.»
A combined lack of coherence in
ice drift fields and
reduced ice concentrations in April 2011 relative to April 2007 suggest that springtime
ice dynamical contributions to fall
sea ice extent may be associated with
sea ice deformation and ridging within an increasingly mobile and fractured
ice cover.