A new ensemble prediction from an ice - ocean model was submitted by Zhang for the July outlook and the new sea
ice thickness map for September 2010 still shows ice remaining in Lancaster Sound.
If we compare
the ice thickness map of the previous winter with that of 2012, we can see that the current ice conditions are similar to those of the spring of 2012 — in some places, the ice is even thinner,» Dr Marcel Nicolaus, sea ice physicist at AWI, said today at a press conference during the EGU General Assembly in Vienna.
Examining the CyroSat - 2 sea
ice thickness map for this spring, Stefan Hendricks further explained: «The Transpolar Drift Stream, a well - known current in the Arctic Ocean, will be carrying the majority of the thick, perennial ice currently located off the northern coasts of Greenland and Canada through the Fram Strait to the North Atlantic.
However, as you'll see by the sea
ice thickness maps below, there may be good reason for the lack of ringed seal lairs, and a general lack of seals except at the nearshore lead that forms because of tidal action: the ice just a bit further offshore ice looks too thick for a good crop of ringed seals in all three years of the study.
Not exact matches
Developing an understanding of how
ice sheets are changing over time requires precise measurements of the
thickness of the
ice sheets and accurate
mapping of the bedrock below.
The study uses data from two NASA missions — Operation IceBridge, which measures
ice thickness and gravity from aircraft, and Oceans Melting Greenland, or OMG, which uses sonar and gravity instruments to
map the shape and depth of the seafloor close to the
ice front.
The results, in the October 15 Science, agree with theoretical predictions, suggesting that superconducting gravimeters can help satellites chart the earth's gravity to
map changes in polar
ice cap
thickness, seawater levels, atmospheric density and planetary geology.
After compiling 10 floe - scale
maps of the
ice from the Weddell, Bellingshausen, and the Wilkes Land regions of the continent, the researchers found that the sea
ice thickness tended to be highly variable, with many ridges and valleys, they report online today in Nature Geoscience.
For six weeks the researchers collected radar data to
map changes in
ice shelf
thickness to understand the processes that contribute to melting at its base.
It will use
ice - penetrating radar to measure the
thickness of the moon's
ice shell,
map its internal rifts and faults (clues to the tempo of its geologic activity) and locate pockets of water near the surface.
«At Kima'Kho, we were able to
map a passage zone in pyroclastic deposits left by the earliest explosive phase of eruption, allowing for more accurate forensic recovery of paleo - lake levels through time and better estimates of paleo -
ice thicknesses,» says UBC volcanologist James K Russell, lead author on the paper published this week in Nature Communications.
So what we need is detailed topo
maps of the bed and
thickness of the GIS, and to work out a
map of the «net buoyancy», or some such (i.e. total
ice area density subtracted from the area density of a hypothetical column of water resting on the bed and extending up to sea level).
Just thinking out loud (and I only know enough to be dangerous;), but with IR radiation
mapping during winter, one might be able to infer a sub-surface temperature profile and compare that with mass loss and
ice sheet
thickness.
Kids can even create their own data visualization by coloring in a
map showing
ice thickness on Greenland.
A goal for accurate summer forecasts should be an accurate
map of
ice type, age,
thickness distribution, and ridging at the end of winter.
Buoys provide key observations for
mapping and attributing summer
ice loss: drift, bottom vs. top melt, amount of snow accumulation, nature of ponds (even if anecdotal from web cams), and
thickness of level
ice.
To determine how much
ice and snowfall enters a specific
ice shelf and how much makes it to an iceberg, where it may split off, the research team used a regional climate model for snow accumulation and combined the results with
ice velocity data from satellites,
ice shelf
thickness measurements from NASA's Operation IceBridge — a continuing aerial survey of Earth's poles — and a new
map of Antarctica's bedrock.
Now, the complete 2010 — 11 winter season data have been processed to produce a seasonal variation
map of sea -
ice thickness.
In June 2011, the first
map of Arctic sea -
ice thickness was unveiled, using CryoSat data acquired between January and February of that year.
After nearly a year and a half of operations, CryoSat has yielded its first seasonal variation
map of Arctic sea -
ice thickness.
«Initially the idea was just to
map what the
ice thickness distribution was,» Wadhams said.
As surface temperture is altitude dependent one might have thought the first thing to check would be a
map, as the arctic
ice lies at sea level + 9 % of its
thickness, while the antarctic
ice sits several kilometers high in the sky, and the surrounding apron of the stuff is immune to windage because of the circumpolar continent in its midst.
This SMOS
thickness map reveals how thin the recently refrozen sea
ice on the Atlantic side still is: