Not exact matches
GOING, GOING... Warmer
conditions in the Arctic are melting
sea ice (as seen here
near Barrow, Alaska).
The islands bordering the Scotia
Sea are rocky and partly covered in
ice and snow year round; despite these harsh
conditions, however, the islands do support vegetation and have been described as the Scotia
Sea Islands tundra ecoregion, which includes South Georgia, the volcanic South Sandwich Islands, and the South Orkneys in the Scotia
Sea, as well as the remote South Shetland Islands
near the Antarctic Peninsula and the small isolated volcano called Bouvet Island.
But before you read on, have a quick look at this short time - lapse video of
sea ice and weather
conditions in the central Arctic Ocean from early July through August 8, recorded by one of the two autonomous cameras set on the
sea ice near the North Pole each spring by a research team from the University of Washington (the same folks I accompanied in 2003).
The following video gives you a fascinating view of one patch of
sea ice through 90 days, provided by a webcam left behind by researchers who annually set up camp
near the North Pole to check ocean and
ice conditions up close.
Having stood on the shifting
sea ice near the North Pole once, I do feel the desire to be bipolar and go to Antarctic waters someday, despite
conditions that will always make trips there adventure travel in the purest sense of that word.
For several years, Rhett Herman, a physics professor at Radford University, has been leading students on an expedition each spring break to study the
condition of the
sea ice off the coast
near Barrow, Alaska.
The animated
sea -
ice imagery above — from one of two autonomous cameras set on
ice near the North Pole each spring — gives a close - focus view of the slushy
conditions that develop on the shifting
ice when the summer sun is at its peak.
Simultaneously, the same measurements were taken colleagues
near Barrow, Alaska, where the
conditions are first - year
sea ice with thin snow cover.
«
Near - bottom water warming in the Laptev
Sea in response to atmospheric and sea - ice conditions in 2007&raq
Sea in response to atmospheric and
sea - ice conditions in 2007&raq
sea -
ice conditions in 2007»
Sea ice, and the cold
conditions it sustains, serves to stabilize methane deposits on and
near the shoreline, [40] preventing the clathrate breaking down and outgassing methane into the atmosphere, causing further warming.
If they do so by simulating
near - average
conditions most of the time, they are getting the right answer for the wrong reason, and their predictions of future
sea ice decline should be discounted.
The
near absence of planktic foraminifers in the MIS 6 sediments of these cores (Supplementary Figs. 2 and 3) 56 also supports the interpretation of virtually no surface water productivity due to closed
sea ice conditions.
Is 2009 simply part of such an extended pause, as it will take another
near - perfect synchrony of summer weather
conditions to provide another major drop in
sea ice extent (Overland)?
While the value for 2009 is
near the trend line (see Stern), arctic
sea ice internal
conditions are considerably different from 2005.
Then things took a turn for the worse, and
sea ice was at record or
near - record low
conditions for most of the summer.
Using a model that tracked a range of habitat
conditions, including water temperature and depth from
sea ice, to predict which habitats would be most impacted by climate change, William Cheung, the study's lead author, and his colleagues found that around 50 species of commercial fishes living
near or at the poles will go extinct within the next 4 decades.
Near - real - time data do not receive the rigorous quality control that final
sea ice products enjoy, but it allows us to monitor
ice conditions as they develop.
Current
sea ice extent and meteorological
conditions suggest a record low is unlikely, as surface temperature over the central Arctic has been
near normal in the last two months and forecasts of atmospheric temperatures for the next few weeks indicate average surface temperatures.