The study found that, based on
recent ice loss rates and the movement of the Thwaites Glacier in West Antarctica, as well as computer model projections, «early - stage collapse has begun.»
Not exact matches
From
recent instrumental observations alone we are therefore unable to predict whether mass
loss from these
ice sheets will vary linearly with changes in the
rate of sea - level rise, or if a non-linear response is more likely.
The reasonable agreement in
recent years between the observed
rate of sea level rise and the sum of thermal expansion and
loss of land
ice suggests an upper limit for the magnitude of change in land - based water storage, which is relatively poorly known.
We are seeing an increase in the
recent speed of
ice loss, when compared to the long - term
ice -
loss rate,» says lead researcher Whyjay Zheng, a doctoral student in geophysics at Cornell University.
This has likely delayed further
ice loss in these areas, which together with the low SLP over the central Arctic Ocean, accounts in part for the
recent decrease in the
rate of
ice loss seen in Figure 2.
Interestingly this year, while July
ice loss rates were rapid in the central Arctic, melt out of the seasonal
ice in Hudson and Baffin bays was slow with the
ice cover persisting longer than in
recent years.
Mass gains of the Antarctic
ice sheet exceed
losses Mass changes of the Antarctic
ice sheet impact sea - level rise as climate changes, but
recent rates have been uncertain.
«Second, in contrast to the previously reported slowing in the
rate during the past two decades1, our corrected GMSL data set indicates an acceleration in sea - level rise (independent of the VLM used), which is of opposite sign to previous estimates and comparable to the accelerated
loss of
ice from Greenland and to
recent projections, and larger than the twentieth - century acceleration.
The
loss, in
recent decades, of thousands of square miles of sea
ice has accelerated warming in the Arctic, where temperatures are increasing at two to three times the
rate of the globe as a whole.
Because of that uncertainty, the United Nations Intergovernmental Panel on Climate Change (IPCC)-- the international body that reviews and assesses the most
recent peer - reviewed climate research from around the world — assumed in 2007 that the
rate of
ice loss from the poles wouldn't change much over the next century.
Contrary to the aforementioned report, a
recent study by Gardelle and others (2012) reveals that high
rates of
ice loss can occur on debris - covered glacier tongues (12).
While the
loss of glacier mass has continued for the past few decades with a slight increase in
recent years, the
rate of mass
loss from the Greenland
ice sheet has dramatically increased in the past decade and continues to increase.
In 2002, the Larsen B
ice shelf collapsed; in 2003, the World Glacial Monitoring Service reported that «The
recent increase in the
rates of
ice loss over reduced glacier surface areas as compared with earlier
losses related to larger surface areas (cf. the thorough revision of available data by Dyurgerov, 2002) becomes even more pronounced and leaves no doubt about the accelerating change in climatic conditions.»