In the end,
total sea ice volume grew by 373 km3 during April, which is the largest increase in the 2007 - 2018 period, almost 200 km3 above average.
At close to 8,000 cubic kilometres (cubic km),
total sea ice volume in November stood at just 48 % of the long - term average and the smallest of any November in the satellite record stretching back to 1979.
Not exact matches
According to the latest Piomas data, a combination of the smallest
sea ice extent and the second - thinnest
ice cover on record puts
total volume of
sea ice in November 2016 at a record low for this time of year.
Is the
total volume of Arctic
sea ice also declining?
The typical estimate of the
sea - level change is five metres, a value arrived at by taking the
total volume of the West Antarctic
Ice Sheet, converting it to water and spreading it evenly across the oceans.
PIOMAS has been used in a wide range of applications but arguably the most popular product has been the time series of
total Arctic
sea ice volume which we have been putting out since March 2010 (see also Fig 1).
The sampling issues arise from the fact that
sea ice is highly dynamic with lots of spatial and seasonal variability so that measurements from individual moorings, submarine sonar tracks, and aircraft flights can only construct an incomplete picture of the evolution of the
total Arctic
sea ice volume.
Ice volume, the product of sea ice area and thickness, is a measure for the total loss in sea ice and the total amount of energy involved in melting the i
Ice volume, the product of
sea ice area and thickness, is a measure for the total loss in sea ice and the total amount of energy involved in melting the i
ice area and thickness, is a measure for the
total loss in
sea ice and the total amount of energy involved in melting the i
ice and the
total amount of energy involved in melting the
iceice.
I sent some questions to some of the authors of the new study showing how much the thickness and
total volume of Arctic
sea ice have declined since 2003.
This work concerns only
sea ice extent without considerations of the age, thickness, and
total volume of
sea ice.
(d, e)
Total area of Arctic
sea ice and AMOC
volume transport as a function of time in the CTL, LW, and SW experiments.
Given the close correlation between latent heat of fusion and net energy in the Arctic, this excellent animation of
sea ice volume gives one of the indications of the
total energy in the Arctic.
All of these characteristics (except for the ocean temperature) have been used in SAR and TAR IPCC (Houghton et al. 1996; 2001) reports for model - data inter-comparison: we considered as tolerable the following intervals for the annual means of the following climate characteristics which encompass corresponding empirical estimates: global SAT 13.1 — 14.1 °C (Jones et al. 1999); area of
sea ice in the Northern Hemisphere 6 — 14 mil km2 and in the Southern Hemisphere 6 — 18 mil km2 (Cavalieri et al. 2003);
total precipitation rate 2.45 — 3.05 mm / day (Legates 1995); maximum Atlantic northward heat transport 0.5 — 1.5 PW (Ganachaud and Wunsch 2003); maximum of North Atlantic meridional overturning stream function 15 — 25 Sv (Talley et al. 2003),
volume averaged ocean temperature 3 — 5 °C (Levitus 1982).
Because of the dramatic thinning, the
total volume of
sea ice is shrinking even faster than its area.
The PIOMAS
sea ice volume estimates, based on a model constrained by satellite extent observations, indicate a
total volume through May in line with recent years, though not at a record low (Figure 7).
That's the case in Antarctica, which is geographically very different to the Arctic, where an increase in surface
sea ice area, but not
total volume, is currently being observed due to increased precipitation and increased surface water run off.