Despite its areas of inaccuracy, near - real - time data are still useful for
assessing changes in sea ice coverage, particularly when averaged over an entire month.
Not exact matches
In turn, sharing scientific and indigenous predictive capabilities is meant to improve coastal ice interpretation and prediction based on satellite imagery, assist communities refining public safety measures, and to add local sea ice to parameters used in assessing global climate change in the Arcti
In turn, sharing scientific and indigenous predictive capabilities is meant to improve coastal
ice interpretation and prediction based on satellite imagery, assist communities refining public safety measures, and to add local
sea ice to parameters used
in assessing global climate change in the Arcti
in assessing global climate
change in the Arcti
in the Arctic.
On average, Antarctic
sea ice may be considerably thicker than once thought, which could significantly
change how scientists
assess sea ice dynamics and their interactions with the ocean
in a warming world.
Sea level rise, ocean acidification and the rapid melting of massive
ice sheets are among the significantly increased effects of human - induced global warming
assessed in the survey, which also examines the emissions of heat - trapping gases that are causing the climate
change.
To
assess these implications, we translate global into local SLR projections using a model of spatial variation
in sea - level contributions caused by isostatic deformation and
changes in gravity as the Greenland and Antarctic
ice sheets lose mass (36 ⇓ — 38), represented as two global 0.5 ° matrices of scalar adjustment factors to the
ice sheets» respective median global contributions to SLR and (squared) to their variances.
Huntington's research activities include reviewing the regulation of subsistence hunting
in northern Alaska, documenting traditional ecological knowledge of beluga whales and bowhead whales, examining Iñupiat Eskimo and Inuit knowledge and use of
sea ice, and
assessing the impacts of climate
change on Arctic communities and Arctic marine mammals.
This report discusses our current understanding of the mechanisms that link declines
in Arctic
sea ice cover, loss of high - latitude snow cover,
changes in Arctic - region energy fluxes, atmospheric circulation patterns, and the occurrence of extreme weather events; possible implications of more severe loss of summer Arctic
sea ice upon weather patterns at lower latitudes; major gaps
in our understanding, and observational and / or modeling efforts that are needed to fill those gaps; and current opportunities and limitations for using Arctic
sea ice predictions to
assess the risk of temperature / precipitation anomalies and extreme weather events over northern continents.
In their paper «Exploring recent trends in Northern Hemisphere blocking,» Barnes and colleagues used various meteorological definitions of «blocking» along with various datasets of atmospheric conditions to assess whether or not there have been any trends in the frequency of blocking events that could be tied to changes in global warming and / or the declines in Arctic sea ic
In their paper «Exploring recent trends
in Northern Hemisphere blocking,» Barnes and colleagues used various meteorological definitions of «blocking» along with various datasets of atmospheric conditions to assess whether or not there have been any trends in the frequency of blocking events that could be tied to changes in global warming and / or the declines in Arctic sea ic
in Northern Hemisphere blocking,» Barnes and colleagues used various meteorological definitions of «blocking» along with various datasets of atmospheric conditions to
assess whether or not there have been any trends
in the frequency of blocking events that could be tied to changes in global warming and / or the declines in Arctic sea ic
in the frequency of blocking events that could be tied to
changes in global warming and / or the declines in Arctic sea ic
in global warming and / or the declines
in Arctic sea ic
in Arctic
sea ice.
Among numerous expeditions by icebreakers and other research vessels to the northern Bering
Sea and Strait, the Chukchi Sea, and other Arctic regions [272] is the Western Arctic Shelf - Basin Interactions Project in 2002 - 2008, which assessed the effects of variability in sea ice cover and hydrography on the marine ecosystem and the impacts of climate chan
Sea and Strait, the Chukchi
Sea, and other Arctic regions [272] is the Western Arctic Shelf - Basin Interactions Project in 2002 - 2008, which assessed the effects of variability in sea ice cover and hydrography on the marine ecosystem and the impacts of climate chan
Sea, and other Arctic regions [272] is the Western Arctic Shelf - Basin Interactions Project
in 2002 - 2008, which
assessed the effects of variability
in sea ice cover and hydrography on the marine ecosystem and the impacts of climate chan
sea ice cover and hydrography on the marine ecosystem and the impacts of climate
change.