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A newly released study finds that ice sheets in Greenland and Antarctica are disappearing three times faster than they were two decades ago, the latest evidence supporting the existence of global warming.
The study was published in the journal Science and is considered an extremely accurate portrayal of ice melts in these polar regions. According to the paper’s authors, the rapid polar ice melting has caused an increase in sea level that may become problematic to low coastal regions.
Perhaps the most alarming data found by the researchers was in Greenland where the ice was melting an estimated five times the rate it was in the mid-1990s. Melt from Greenland accounted for a whopping two-thirds of the polar ice melt.
...
Shepherd estimates that the data compiled in the new study is two to three times more reliable than previous studies on melting ice and rising sea-level.
She expects sea level to move up the coast by at least 40 inches in the next 90 years.
Mass Gains of the Antarctic Ice Sheet Exceed Losses
Zwally, H. Jay; Li, Jun; Robbins, John; Saba, Jack L.; Yi, Donghui; Brenner, Anita; Bromwich, David Abstract: During 2003 to 2008, the mass gain of the Antarctic ice sheet from snow accumulation exceeded the mass loss from ice discharge by 49 Gt/yr (2.5% of input), as derived from ICESat laser measurements of elevation change. The net gain (86 Gt/yr) over the West Antarctic (WA) and East Antarctic ice sheets (WA and EA) is essentially unchanged from revised results for 1992 to 2001 from ERS radar altimetry. Imbalances in individual drainage systems (DS) are large (-68% to +103% of input), as are temporal changes (-39% to +44%). The recent 90 Gt/yr loss from three DS (Pine Island, Thwaites-Smith, and Marie-Bryd Coast) of WA exceeds the earlier 61 Gt/yr loss, consistent with reports of accelerating ice flow and dynamic thinning. Similarly, the recent 24 Gt/yr loss from three DS in the Antarctic Peninsula (AP) is consistent with glacier accelerations following breakup of the Larsen B and other ice shelves. In contrast, net increases in the five other DS of WA and AP and three of the 16 DS in East Antarctica (EA) exceed the increased losses. Alternate interpretations of the mass changes driven by accumulation variations are given using results from atmospheric-model re-analysis and a parameterization based on 5% change in accumulation per degree of observed surface temperature change. A slow increase in snowfall with climate warming, consistent with model predictions, may be offsetting increased dynamic losses.
Shepherd estimates that the data compiled in the new study is two to three times more reliable than previous studies on melting ice and rising sea-level. The current go-to report on this subject, which is used by the Intergovernmental Panel on Climate Change, or IPCC, was created in 2007.
The study used by the IPCC covers the increasing ice melt in Greenland and Antarctica and even reports a sheet loss within the range of the new study. However, the IPCC report did not consider a crucial question answered by Shepherd and Ivans’ team: could Antarctica be growing instead of shrinking?
Originally posted by poet1b
And if you look at the Antarctic Penninsula, there is no doubt the glaciers are retreating.
www.usgs.gov...
And what is ignored more than anything is that GW continues to accelerate.
First of all the data you are claiming to post is about ten years out of date, while I provide a link to the latest reports.
During 2003 to 2008, the mass gain of the Antarctic ice sheet from snow accumulation exceeded the mass loss from ice discharge by 49 Gt/yr (2.5% of input), as derived from ICESat laser measurements of elevation change...
However, the IPCC report did not consider a crucial question answered by Shepherd and Ivans’ team: could Antarctica be growing instead of shrinking? Shephard thinks that without answer this question and others like it, scientists would not be able to announce, with confidence, how the ice sheets have changed for certain.
Originally posted by poet1b
reply to post by totallackey
Data from 2003 is almost 10 years old, it will be 2013 in less than a month.
And you still have yet to provide an actual link to the source of the study. Your quote talks abut snow and elevation measurements, that prove nothing about ice. It reads like some cherry picked info that almost says something.
Originally posted by poet1b
reply to post by totallackey
Data from 2003 is almost 10 years old, it will be 2013 in less than a month.
And you still have yet to provide an actual link to the source of the study. Your quote talks abut snow and elevation measurements, that prove nothing about ice. It reads like some cherry picked info that almost says something.
Our modification of the
outflow changes the balance estimate by ?282 Gt/year (15% of the annual output) and
modification of the IOM input value changes the balance estimate by -159 Gt/year (8% of
Surv Geophys
123
the annual input), which together bring the net balance for overall AIS to a loss of 13 Gt/
year.
Comparison between two ERS-based estimates shows that the difference between the
preferred estimate for overall AIS of -31 ± 12 Gt/year for 1992 to 2001 given in Z05 and
the preferred estimate of ?27 ± 29 Gt/year for 1992 to 2003 given in W06 are mainly due
to different treatments of firn/ice density, corrections for the rate of upper firn compaction,
differences in areal coverage, and IEP. The methodology in Z05 included an important
correction for elevation changes caused by changes in the rate of firn compaction driven by
changes in surface temperature, covered more AIS area with crossover analyses, and
estimated the uncovered areas with optimal interpolation compared to the other analyses.
Nevertheless, the difference between the two ERS estimates is only 3% of the annual mass
input.
For all of the AIS, the IOMMd estimate lies within the range of the two ERS estimates,
which along with the GRACE-based estimate of Raimillen et al. (2006) gives a narrowed
range of ? 29 to -40 Gt/year that is only about 3.5% of the annual mass input. Our
preferred estimate for 1992–2001 is -47 Gt/year for WA, ? 16 Gt/year for EA, and -31
Gt/year overall (?0.1 mm/year SLE), not including part of the AP (1.07% of the AIS area)
as taken from Z05. However, this narrowed range of estimates leaves the more negative
GRACE-based estimates as outliers. Regarding the trend toward an increasing mass loss in
some GRACE estimates, we also find that the evidence presented in R08, supporting an
increase in mass loss from the IOM analyses, is insufficient as published.
A change of approximately 5% of the annual mass input or output to the AIS is
approximately 100 Gt/year, which is 0.3 mm/year SLE and 10% of current sea level rise.
Therefore, for the purpose of closing the sea level change budget to 10% or better,
obtaining estimates of the AIS mass balance to an accuracy of several percent is required.
Considering the state-of-art for determining the input and output fluxes, it is difficult to see
how the IOM can achieve the required accuracy even for a snapshot in time. Furthermore,
the problems with the IOM are even more difficult for determining trends.
Although the published GRACE estimates of mass change have a wide range and
relatively large estimates of error, the methodology for deriving mass changes from
GRACE data and correcting errors is improving significantly with time. The convergence
of results from ICESat and GRACE within estimated errors for the recent mass loss from
Greenland is a significant advance. However, the GIA is significantly larger in the Antarctic
and the uncertainty of the modeled GIA is also larger, mainly because of uncertainty
in the history of the glacial unloading and the sparsity of data for model calibration. The
expansion of Global Positioning System (GPS) measurements of crustal motion in the
Antarctic in recent years is providing new data that are being used for improving the
modeled GIA estimates (e.g. King et al. 2010). Applying these improvements to GRACE
data analyses, the recent improvements applied to the ICES at data analyses for Greenland,
and the joint analyses of GRACE and ICESat data for the same time periods should
significantly improve not only the estimates of the current mass balance of Antarctica, but
also of its changes over time.
Acknowledgments This research was supported by NASA’s ICESat Project Science funding. We thank
Scott Luthcke for providing his insights on GRACE methodology, issues, and developments, and two
anonymous reviewers for helpful suggestions and corrections.
Open Access This article is distributed under the terms of the Creative Commons Attribution Noncommercial
License which permits any noncommercial use, distribution, and reproduction in any medium,
provided the original author(s) and source are credited.
Surv Geophys
123
The international team of 47 experts led by Shepherd analysed data collected by these methods from almost 30 previous ice-sheet studies, including 20 years of data from 10 different satellite missions and 32 years of model data on surface mass balance — the difference in the weight of the ice sheet gained through snowfall and lost through melting of the ice sheets.
The result is an estimate “two to three times more accurate than that in the last IPCC report”, says Shepherd.
The latest study “moves Antarctica from a position of relative uncertainty in terms of its ice loss to one where we are now certain that it is losing ice”, says Andrew Shepherd, first author of the study and professor of Earth observation at the University of Leeds, UK.
Scientists use four techniques to gauge whether the ice caps are gaining or losing mass. Two techniques involve using either lasers or radars on satellites to measure changes in the surface elevation of the ice; another uses a method known as input-output modelling to represent regional changes in snowfall and ice melt; and the fourth measures changes in ice-sheet mass from space using the Gravity Recovery and Climate Experiment (GRACE) mission satellites.