This type of analysis may be useful for future applications of using seismic records to track the strength of sea
ice over large regions, which has been difficult to determine from satellite observations.»
Scientists say there was no new record set this year because summer temperatures were cooler than in the past two summers and because winds tended to disperse
ice over a larger region.
Not exact matches
For their work Maksym and co-investigators Guy Williams from the University of Hobart, Tasmania and Jeremy Wilkinson of the British Antarctic Survey in Cambridge, UK, used a robot known as an autonomous underwater vehicle (AUV) to cruise under
ice in three
regions near the coast and measure the thickness directly
over a much
larger area.
The Arctic has transformed
over the last five years into a
region that's warmer and greener, with
larger patches of open water as sea
ice recedes.
«As a result of the acceleration of outlet glaciers
over large regions, the
ice sheets in Greenland and Antarctica are already contributing more and faster to sea level rise than anticipated,» he observed.
«As the Arctic sea -
ice cover continues to disappear and the snow cover melts ever earlier
over vast
regions of Eurasia and North America, it is expected that
large - scale circulation patterns throughout the northern hemisphere will become increasingly influenced by Arctic Amplification.»
It is a model of the ocean and
ice over a specific domain covering a
large part of the Arctic
region.
Summer of 2008 shows a
large region of less sea
ice than normal
over the Beaufort Sea compared to 2005 which had less
ice cover than normal in the Eastern Siberian Sea and Laptev Sea.
The ongoing loss of
ice in a
region that is on average not wamer in the latter part of 60 years (1941 - 2000) seems like a good reminder that it does not take a constant yeaer on year increase to cause pronounced natural response
over large areas.
If the «boxes» are so
large that every land area is considered equal — how are coastal
regions and
ice - covered areas modelled as they change
over the year?
Two main geomorphological forms are commonly found in continuous permafrost
regions of Eastern Canada: (i) small, shallow, narrow runnel ponds formed
over melting
ice wedges where peat slumping occurs, and (ii) more stable, slightly
larger and deeper, polygonal ponds, which are naturally linked to the active layer freeze - thaw cycles, and can be colonized by aquatic plants and microbial mats (Fig. 1).
In contrast, SLP has been higher
over the Kara sector, which may have contributed to the
large current negative anomalies in sea
ice concentration in that
region of the Arctic.
To a
large extent the probability forecasts in Figure 11 resemble the surface air temperature anomaly of the last two months in Figure 7 in the high latitudes, illustrating the persistence of weak climate anomalies
over the sea
ice and ocean covered
regions throughout the summer months.
Behavior of the sea
ice over the past winter and the spring and the
large positive temperature anomalies in the Arctic (as high as 20 degrees C
over large regions in the past winter) suggest that an extent near that of the 2012 minimum may occur again if there is
large export of sea
ice out to the Atlantic Ocean via the Fram Strait.
The issue, beyond the core data representing but a single geospacial location and thus by itself not representative of the whole (and much
larger)
region in which it resides, is that the core is near the Greenland summit (in order to get the deepest profile of the
ice possible) and therefore at an elevation of
over 2 miles above sea level.
Polar Stratospheric Clouds
Large, diffuse,
ice - particle clouds that form in the stratosphere usually
over polar
regions.