Not exact matches
The findings «lend support to our confidence in recent
estimates of sea level rise and the increasing
ice sheet contribution,» said Michael Oppenheimer, the Albert G. Milbank professor of geosciences and international affairs at Princeton University's department of geosciences, in an email to The Post.
For recent years, better
estimates of the land
ice contribution to sea level are available from various observations of glaciers,
ice caps and
ice sheets.
These values have been
estimated using relatively simple climate models (one low - resolution AOGCM and several EMICs based on the best
estimate of 3 °C climate sensitivity) and do not include
contributions from melting
ice sheets, glaciers and
ice caps.
(A 2014 study by McMillan et al. examining CryoSat - 2 data more than doubled the
estimated rate of Antarctic
ice sheet contribution to sea level.
And more recent
estimates of the Antarctic mass balance
contribution to sea level rise has the East Antarctica
ice sheet gaining mass at a more accelerated pace for 2003 - 2013 than the mere +14 Gt per year identified by Shepherd et al. (2012) for 1992 - 2011.
IMBIE is an international collaboration of polar scientists, providing improved
estimates of the
ice sheet contribution to sea level rise.
As with IMBIE 2012, it will collate, compare, integrate, interpret, and report satellite
estimates of
ice sheet mass balance, with the overall aim of producing a community assessment of Greenland and Antarctica's ongoing
contributions to global sea level rise.
Hay et al. (2015) argue that rates of sea level rise between 1.0 and 1.4 mm yr - 1 close the sea - level budget for 1901 — 1990 as
estimated in AR5, without appealing to an underestimation of individual
contributions from ocean thermal expansion, glacier melting, or
ice sheet mass balance.
We take this as an
estimate of the part of the present
ice sheet mass imbalance that is due to recent
ice flow acceleration (Section 4.6.3.2), and assume that this
contribution will persist unchanged.