That 2005 paper is talking about increases in ice mass
in Greenland interiors - something that isn't necessarily
inconsistent with AGW, which predicts higher water evaporation
and precipitation rates, producing more snow in places like
Greenland. This paper says that it it "possible" that ablation
in coastal areas may be offset by winter accumulation, but is
by no means shown to be the case by the ERS data sets under
consideration in that 2005 paper.
From the conclusions in that paper:
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In conclusion, we have presented new evidence
of (i) decadal increase in surface elevation
(È5 cm/year) within a study area
comprising most of the Greenland Ice Sheet,
1992 to 2003, caused by accumulation over
extensive areas in the interior of Greenland;
(ii) divergence in elevation changes since the
year 2000 for areas above and below 1500 m,
with high-elevation increases and low-elevation
decreases, the former in contrast to previous
research (10, 13); and (iii) negative correlation
between winter elevation changes and the NAO
index, suggesting an underappreciated role of
the winter season and the NAO for elevation
changes—a wild card in Greenland Ice Sheet
mass-balance scenarios under global warming.
There are, however, caveats to consider.
First, we cannot make an integrated assessment
of elevation changes—let alone ice volume
and its equivalent sea-level change—for the
whole Greenland Ice Sheet, including its outlet
glaciers, from these observations alone, because
the marginal areas are not measured
completely using ERS-1/ERS-2 altimetry (see
Fig. 1). It is conceivable that pronounced
ablation (e.g., 10, 11) in low-elevation marginal
areas could offset the elevation increases
that we observed in the interior areas. Second,
there is large interannual to decadal variability
in the high-latitude climate system including
the NAO, such that the 11-year-long data set
developed here remains too brief to establish
long-term trends. Therefore, there is clearly a
need for continued monitoring using new satellite
altimeters—including advanced ones with
improved ice-sheet ranging in steeper coastal
areas—and other remote-sensing and field observations,
together with numerical modeling
to calculate the mass budget through net losses
and net input from snow (33).
----
KMM
Dave Snope said:
That is a 60cm INCREASE in thickness over 11 years. And they point out that the only areas losing ice are coastal areas, and that is due to normal ocean warm oscillation cycles. But since the coastal phenomenon is all you will read about in the major newspapers and hear about on the major networks, most of the world will remain uninformed.
Averaged over the study area, the increase is 5.4 T 0.2 cm/year, or
È60 cm over 11 years, or È54 cm when corrected for isostatic uplift.
http://www.cfa.harvard.edu/~wsoon/MattCronin-Mar21-07-d/Johannessenetal05-GreenlandIceFinal.pdf