Not exact matches
The relevant papers are [Velicogna and Wahr 2006 Measurements
of time - variable gravity show mass
loss in Antarctica Science 311, 1754 - 1756 and Rignot and Thomas «Mass balance
of polar ice sheets» Science 297, 1502 - 1506]
The lower trend found by our study is consistent with the median projected sums
of thermal expansion and glacier mass
loss, implying that no net contribution from
polar ice sheets is needed over 1901 - 1990.
The relevant papers are [Velicogna and Wahr 2006 Measurements
of time - variable gravity show mass
loss in Antarctica Science 311, 1754 - 1756 and Rignot and Thomas «Mass balance
of polar ice sheets» Science 297, 1502 - 1506]
The findings reinforce suggestions that strong positive
ice — temperature feedbacks have emerged in the Arctic15, increasing the chances
of further rapid warming and sea
ice loss, and will probably affect
polar ecosystems,
ice -
sheet mass balance and human activities in the Arctic...» *** This is the heart
of polar amplification and has very little to do with your stated defintion
of amplifying the effects
of warming going on at lower latitudes.
The survey shows that there was a net
loss of ice from the combined
polar ice sheets between 1992 and 2002 and a corresponding rise in sea level.
A major limitation is the fact that the calibration phase for these semi-empirical models does not cover the range
of climate - system behaviour that might be expected for the 21st century, i.e., significant
loss of ice from the large
polar ice sheets.
«Significant
loss of ice from polar ice sheets» Of course, this does not apply to floating ice (with the exception of small changes due to higher temperature and water expansion that might happen incidentally
of ice from
polar ice sheets»
Of course, this does not apply to floating ice (with the exception of small changes due to higher temperature and water expansion that might happen incidentally
Of course, this does not apply to floating
ice (with the exception
of small changes due to higher temperature and water expansion that might happen incidentally
of small changes due to higher temperature and water expansion that might happen incidentally).
Melting Arctic
ice -
sheets will reduce ocean salinities (IPCC, 2001), causing species - specific shifts in the distribution and biomass
of major constituents
of Arctic food webs, including poleward shifts in communities and the potential
loss of some
polar species (such as the narwhal, Monodon monoceros).