Results 1 to 10 of about 100,265 (236)

Future sea ice weakening amplifies wind-driven trends in surface stress and Arctic Ocean spin-up [PDF]

open access: yesNature Communications
Arctic sea ice mediates atmosphere-ocean momentum transfer, which drives upper ocean circulation. How Arctic Ocean surface stress and velocity respond to sea ice decline and changing winds under global warming is unclear.
Morven Muilwijk   +3 more
doaj   +5 more sources

Low Density of Top Predators (Seabirds and Marine Mammals) in the High Arctic Pack Ice [PDF]

open access: goldScientifica, 2016
The at-sea distribution of top predators, seabirds and marine mammals, was determined in the high Arctic pack ice on board the icebreaker RV Polarstern in July to September 2014. In total, 1,620 transect counts were realised, lasting 30 min each.
Claude R. Joiris   +3 more
doaj   +7 more sources

Platelet Ice Under Arctic Pack Ice in Winter [PDF]

open access: hybridGeophysical Research Letters, 2020
The formation of platelet ice is well known to occur under Antarctic sea ice, where subice platelet layers form from supercooled ice shelf water. In the Arctic, however, platelet ice formation has not been extensively observed, and its formation and ...
Christian Katlein   +23 more
core   +12 more sources

Sympagic Fauna in and Under Arctic Pack Ice in the Annual Sea-Ice System of the New Arctic [PDF]

open access: goldFrontiers in Marine Science, 2020
A strong decline and thinning of the Arctic sea-ice cover over the past five decades has been documented. The former multiyear sea-ice system has largely changed to an annual system and with it the dynamics of sea-ice transport across the Arctic Ocean ...
Julia Ehrlich   +8 more
doaj   +3 more sources

Multiscale mushy layer model for Arctic marginal ice zone dynamics [PDF]

open access: yesScientific Reports
Perhaps the most dynamic component of the Arctic sea ice cover is the marginal ice zone (MIZ), the transitional region between dense pack ice to the north and open ocean to the south.
Courtenay Strong   +2 more
doaj   +3 more sources

Status and trends in the structure of Arctic benthic food webs [PDF]

open access: yesPolar Research, 2015
Ongoing climate warming is causing a dramatic loss of sea ice in the Arctic Ocean, and it is projected that the Arctic Ocean will become seasonally ice-free by 2040.
Monika Kędra   +13 more
doaj   +7 more sources

Potential source regions and processes of aerosol in the summer Arctic [PDF]

open access: yesAtmospheric Chemistry and Physics, 2015
Sub-micrometer particle size distributions measured during four summer cruises of the Swedish icebreaker Oden 1991, 1996, 2001, and 2008 were combined with dimethyl sulfide gas data, back trajectories, and daily maps of pack ice cover in order to ...
J. Heintzenberg, C. Leck, P. Tunved
doaj   +4 more sources

Culturable diversity of Arctic phytoplankton during pack ice melting [PDF]

open access: goldElementa: Science of the Anthropocene, 2020
Massive phytoplankton blooms develop at the Arctic ice edge, sometimes extending far under the pack ice. An extensive culturing effort was conducted before and during a phytoplankton bloom in Baffin Bay between April and July 2016.
Catherine Gérikas Ribeiro   +7 more
doaj   +2 more sources

Winter sea ice export from the Laptev Sea preconditions the local summer sea ice cover and fast ice decay [PDF]

open access: yesThe Cryosphere, 2017
Ice retreat in the eastern Eurasian Arctic is a consequence of atmospheric and oceanic processes and regional feedback mechanisms acting on the ice cover, both in winter and summer.
P. Itkin, P. Itkin, T. Krumpen
doaj   +3 more sources

The summer aerosol in the central Arctic 1991–2008: did it change or not? [PDF]

open access: yesAtmospheric Chemistry and Physics, 2012
In the course of global warming dramatic changes are taking place in the Arctic and boreal environments. However, physical aerosol data in from the central summer Arctic taken over the course of 18 yr from 1991 to 2008 do not show systematic year-to-year
J. Heintzenberg, C. Leck
doaj   +5 more sources

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