Not exact matches
Computer
model simulations have suggested that
ice - sheet melting through warm water incursions could initiate a collapse of the WAIS
within the next few centuries, raising global
sea - level by up to 3.5 metres.»
We quantify
sea - level commitment in the baseline case by building on Levermann et al. (10), who used physical simulations to
model the SLR
within a 2,000 - y envelope as the sum of the contributions of (i) ocean thermal expansion, based on six coupled climate
models; (ii) mountain glacier and
ice cap melting, based on surface mass balance and simplified
ice dynamic
models; (iii) Greenland
ice sheet decay, based on a coupled regional climate
model and
ice sheet dynamic
model; and (iv) Antarctic
ice sheet decay, based on a continental - scale
model parameterizing grounding line
ice flux in relation to temperature.
This is starting to make the second graph (below) looking reasonable, and those scientists and
models which have been suggesting an
sea -
ice - free summer Arctic
within a decade to be on the money.
The current operational ensemble forecast systems
model sea ice dynamically using the LIM2
model within NEMO ocean
model to represent the dynamic and thermodynamic evolution of
sea ice within the coupled forecast system.
In addition, chosen
models had to simulate (hindcast),
within 20 % accuracy, September
sea ice extent observed from 1980 to 1999.
RCP 2.6 and a realistic
model based on past
sea ice extent and its relationship to AMO are indistinguishable and do not anticipate an Arctic free of
ice within the 21st century if current trends are maintained.
«Using complex new
modeling, the scientists have found that rapidly melting Arctic
sea ice now threatens to diminish precipitation over California by as much as 15 percent
within 20 to 30 years,» the Los Angeles Times writes.
A
sea ice free summer arctic
within 30 years: an update from CMIP5
models.
Within the Outlook project, there may be differences in how each group obtains their area (e.g.,
model grid cells of varying resolution,
sea ice charts, and satellite observations); each of these could produce a different value for
ice extent.
As
sea ice declines, it becomes thinner, with less
ice build - up over multiple years, and therefore more vulnerable to further melting.15
Models that best match historical trends project northern waters that are virtually
ice - free by late summer by the 2030s.25, 26,12
Within the general downward trend in
sea ice, there will be time periods with both rapid
ice loss and temporary recovery, 27 making it challenging to predict short - term changes in
ice conditions.
Wang, M., and J. E. Overland, 2012: A
sea ice free summer Arctic
within 30 years: An update from CMIP5
models.
Given that the IPCC
models significantly underestimate the observed rate of Arctic
sea -
ice decline (17), a summer
ice - loss threshold, if not already passed, may be very close and a transition could occur well
within this century.
They may result from more tuning of
sea ice conditions
within the
models, improved
model parameterizations and processes, or some combination of the two.
Using a
model that tracked a range of habitat conditions, including water temperature and depth from
sea ice, to predict which habitats would be most impacted by climate change, William Cheung, the study's lead author, and his colleagues found that around 50 species of commercial fishes living near or at the poles will go extinct
within the next 4 decades.