S. Hakkinen, A. Proshutinsky, and I. Ashik, “Sea Ice Drift in the Arctic since the 1950s,” Geophys. Rev. Lett. 35 , L19704 (2008).Hakkinen S, Proshutinsky A, Ashik I. Sea ice drift in the Arctic since the 1950s [ J ]. Geophysical Research Letters, 2008, 35 ( 19 ), ...
The drift pattern of sea ice in the Arctic with particular reference to the Atlantic ap- proach. In: The Arctic Ocean, Rey, L. (ed.), 82-96.VINJE, T.E. (1982): The drift Pattern of sea ice in the Arctic with particular refe- rence to the atlantic approach. IA§The Arctic ...
Ice cover of the Arctic Ocean is a dynamic dissipative system of the geophysical level, in which physicomechanical processes of various scales and intensities occur simultaneously and lead to the formation of a discrete structure of the ice cover. Spatial gradients of the ice drift velocity [1, ...
Sea ice drift in the Arctic since the 1950s Oceanography: Physical: Ice mechanics and air/sea/ice exchange processes (0700075007520754Oceanography: General: Climate and interannual variability (1616... S Hakkinen,A Proshutinsky,I Ashik - 《Geophysical Research Letters》 被引量: 126发表: 2008年 ...
The decline of sea ice in the Arctic region is a critical indicator of rapid global warming and can also influence the feedback processes in the Arctic, so the prediction of sea ice extent and thickness plays an important role in climate modeling and pre
sea ice growth. Here we show that sea ice MP has no uniform polymer composition and that, depending on the growth region and drift paths of the sea ice, unique MP patterns can be observed in different sea ice horizons. Thus even in remote regions such as the Arctic Ocean, certain MP ...
A variety of hypotheses, involving sub-ice-shelf melting, stratospheric ozone depletion and tropical teleconnections, have been proposed to explain the observed Antarctic sea-ice expansion over the period of continuous satellite monitoring and correspond
We demonstrate that the large-scale hydrographic structure of the central Iceland Sea has changed significantly over this period and that the locally transformed water has become less dense, in concert with a retreating sea-ice edge and diminished ocean-to-atmosphere heat fluxes. This has reduced ...
Analysis of Arctic sea ice drift from 1979-1997 using a Lagrangian perspective shows the complexities of ice drift response to variations in atmospheric conditions. Changes in ice dynamics influence the redistribution of ice, and any transported material, from different source areas. Sources of ice ...
Despite global warming and Arctic sea-ice loss, on average the Antarctic sea-ice extent has not declined since 1979 when satellite data became available. In contrast, climate model simulations tend to exhibit strong negative sea-ice trends for the same period. This Antarctic sea-ice paradox leads...