• From 1976 to 1999
the average thickness of ice in the Arctic Ocean had dropped 43 percent.
Still more striking, and significant, has been a severe decline in
the average thickness of the ice pack, and thus of its volume (graph).
Not exact matches
There also appears to be a strong correlation between the area
of multiyear
ice and the spatially
averaged thickness of the perennial
ice pack, which suggests that the satellite - derived areal decreases represent substantial rather than only peripheral changes.
With a volume
of more than 700,000 cubic miles and an
average thickness of 4,000 feet, the West Antarctic
Ice Sheet (WAIS) holds enough water to raise sea levels by 15 to 20 feet — and it is already sweating off 130 billion tons of ice per ye
Ice Sheet (WAIS) holds enough water to raise sea levels by 15 to 20 feet — and it is already sweating off 130 billion tons
of ice per ye
ice per year.
Ice originating from the Arctic Ocean showed a mean
thickness of more than three metres on
average.
Rising polar temperatures caused the
average thickness of winter Arctic sea
ice to decrease from about 12 feet to 6 feet between 1978 and 2008, and thinner
ice melts more readily.
With an
average thickness of 625 feet, the iceberg will contain 277 cubic miles
of ice.
So unless the perimeter
of the Greenland
ice sheet is the exact same
thickness as the entire
ice sheet (say 3 km on
average), an area loss there,
of 15 %, will produce a much smaller % volume loss, than say if this area loss were smack dab in the middle
of the Greenland
ice sheet.
[Response: The
thickness of the greenland
ice sheet is ~ 2000 m on
average (don't quote me, that's a ballpark estimate).
(And the
average age
of all
ice never got above single digits) Because most
of the
thickness increases come in the first couple
of years, and most old
ice is «old» because it is nearing the end
of its natural cycle (where it thins to zero.)
The
average thickness is usually still falling at this time
of year (presumably because thin
ice is being added) but it has not yet been calculated for this year.
% due to eruption 9.5 % (assuming the
average thickness of melted
ice was 1 meter, and not allowing for any
of the heat being lost to warming the 4 km thick sea water column, or air, or evaporation)
Ice covered by the insulating material melted 60 percent less than exposed portions which lost an
average of 5 feet in
thickness during the test.
Having said that, it is a really small effect — if the entire Arctic summer sea
ice pack melted (
average thickness 2 metres, density ~ 920 kg / m3, area 3 × 10 ^ 6 km ^ 2 (0.8 % total ocean area) = > a 4.5 cm rise instantly which implies a global sea level rise
of 0.36 mm.
(Right) Extents and
thicknesses of the Greenland
Ice Sheet and western Canadian and Iceland glaciers at their minimum extent during the last interglacial, shown as a multi-model average from three ice mode
Ice Sheet and western Canadian and Iceland glaciers at their minimum extent during the last interglacial, shown as a multi-model
average from three
ice mode
ice models.
The scientists have measured
average sea
ice thickness to less than a meter in the area, and observed a late start
of the freeze up period.
Given the minimum
ice extent is about 4 million km2 and 4000 km3 (an
average of 1 meter
thickness) the SMOS data is
of limited value.
The melting is most pronounced for small glaciers at altitudes below 17,000 feet, he said, which have lost an
average of 4.4 feet
of ice thickness per year.
On page 16 here: https://curryja.files.wordpress.com/2014/10/sea-
ice-physical-processes.pdf There is the «Annual cycle
of net surface heat flux for various
ice thicknesses» Roughly interpolating the no sea
ice flux I got an
average of — 310 Wm2 over the course
of a year.
Starting with the April Pan-Arctic
Ice Ocean Modeling and Assimilation System (PIOMAS) volume distribution and the April National Snow and Ice Data Center (NSIDC) average ice extent the estimated extent loss for each 10 cm thickness of ice loss is calculat
Ice Ocean Modeling and Assimilation System (PIOMAS) volume distribution and the April National Snow and
Ice Data Center (NSIDC) average ice extent the estimated extent loss for each 10 cm thickness of ice loss is calculat
Ice Data Center (NSIDC)
average ice extent the estimated extent loss for each 10 cm thickness of ice loss is calculat
ice extent the estimated extent loss for each 10 cm
thickness of ice loss is calculat
ice loss is calculated.
[Gallery: Vanishing Glaciers] «The
average thickness of the Arctic sea
ice cover is declining because it is rapidly losing its thick component, the multi-year
ice.
Rennie (Public), 3.20 (2.50 - 3.80), Heuristic Starting with the April PIOMAS volume distribution and the April NSIDC
average ice extent the estimated extent loss for each 10 cm
thickness of ice loss is calculated.
The time constants
of albedo feedback from melting N America snow cover are shorter than the albedo feedback from melting Arctic sea
ice, and the sea
ice is changing response as its
average thickness decreases, and the ratios
of 1, 2, 3, 4, 5 year
ice area changes.
The research, reported in Geophysical Research Letters, showed that last winter the
average thickness of sea
ice over the whole Arctic fell by 26 cm (10 %) compared with the
average thickness of the previous five winters, but sea
ice in the western Arctic lost around 49 cm
of thickness.
This is on top
of very significant drops in
average ice thickness.
«Since the 1970's, temperatures at the earth's surface have warmed, Arctic sea
ice has decreased in
thickness, and now we know that the
average temperature
of the world's oceans has increased during this same time period.»
Last winter the
average thickness of sea
ice over the whole Arctic fell by 26 cm (10 %) compared with the
average thickness of the previous five winters, but sea
ice in the western Arctic lost around 49 cm
of thickness.