They have
several ice thickness measurements varying from just 6 points (1990) to more than dozen.
Not exact matches
Ambient geothermal heat emanating up from the seafloor melts the underside of the
ice sheet at a rate of
several penny
thicknesses per year.
The lakes are fed by geothermal heat that seeps up from the Earth's interior, melting away the bottom of the
ice sheet at a rate of
several dime -
thicknesses per year and liberating water from the
ice.
I know that, such as East Antarctica, which
ice sheet's
thickness could reach
several kilometers therefore huge pressure and geothermal flux results in melting, then the subglacial lakes and water channels.
Almost all state - of - the - art AOGCMs now include more elaborate sea
ice dynamics and some now include
several sea
ice thickness categories and relatively advanced thermodynamics.
Several researchers have looked at the «open water formation efficiency» during the melt season, and have found a relationship with the mean March
ice thickness.
The complete absence of multiyear sea
ice in the region, confirmed by
thickness surveys and local observations, is a first for the region in the past
several decades.
The
thickness of Arctic sea
ice has also been on a steady decline over the last
several decades.
While the
ice thickness is generally thinner in May 2016 compared to previous years, the air temperature has been
several degrees above the last 10 year mean in the northern North Atlantic and the Beaufort Sea, but colder in the Eastern Siberian Sea and Laptev Sea causing the described melt pond pattern.
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.
For the Arctic, there are
several techniques available for estimating the
thickness distribution of sea
ice.
6) There are still insufficient observations of
ice thickness to quantify the basin - wide and long - term rate of
ice - volume change over the past
several decades.
This year,
several airborne campaigns, including the German - Canadian - US collaborative effort PAMARCMIP (see Figure 4), the NASA IceBridge flights, and others have collected
ice thickness or surface topography data in the North American Arctic.
This year,
several airborne campaigns have collected
ice thickness or surface topography data in the North American Arctic.