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Science marches on.
The http://www.ipcc.ch/publications_and_data/publications_ipcc_fourth_assessment_report_wg1_report_the_physical_science_basis.htm" for climate change was based on
peer reviewed literature available in 2006. Since that time,
there have been a number of newer studies that have contributed
to a better understanding. These have been put together into a
http://www.ccrc.unsw.edu.au/Copenhagen/Copenhagen_Diagnosis_LOW.pdf" for the meeting in Copenhagen.
In general, uncertainties resolved since 2006 point to a more
rapidly changing and more sensitive climate than previously thought.
There are several interesting sections in the report with lots of vivid
color photos. However, overall it is a sombering report.
CO2 emissions are accelerating while temperatures, sea level and
water cycle increases are all expected to accelerate.
It's very difficult to conceive the climate tracking anything but
the upper end of the projections.
Here are highlights from the new report:
http://www.copenhagendiagnosis.com/default.html
Link directly to pdf file:
http://www.ccrc.unsw.edu.au/Copenhagen/Copenhagen_Diagnosis_LOW.pdf
The http://www.ipcc.ch/publications_and_data/publications_ipcc_fourth_assessment_report_wg1_report_the_physical_science_basis.htm" for climate change was based on
peer reviewed literature available in 2006. Since that time,
there have been a number of newer studies that have contributed
to a better understanding. These have been put together into a
http://www.ccrc.unsw.edu.au/Copenhagen/Copenhagen_Diagnosis_LOW.pdf" for the meeting in Copenhagen.
In general, uncertainties resolved since 2006 point to a more
rapidly changing and more sensitive climate than previously thought.
There are several interesting sections in the report with lots of vivid
color photos. However, overall it is a sombering report.
CO2 emissions are accelerating while temperatures, sea level and
water cycle increases are all expected to accelerate.
It's very difficult to conceive the climate tracking anything but
the upper end of the projections.
Here are highlights from the new report:
The full report is available here:Global carbon dioxide (CO2) emissions from fossil fuel burning in 2008 were 40%
higher than those in 1990, with a three-fold acceleration over the past 18 years.
Global CO2 emissions from fossil fuel burning are tracking near the highest scenarios
considered so far by the IPCC.
The fraction of CO2 emissions absorbed by the land and ocean CO2 reservoirs has likely
decreased by ~5% (from 60 to 55%) in the past 50 years, though interannual variability is
large.
Global air temperature, humidity and rainfall trend patterns exhibit a distinct fingerprint
that cannot be explained by phenomena apart from increased atmospheric greenhouse gas
concentrations.
Every year this century (2001-2008) has been among the top 10 warmest years since
instrumental records began, despite solar irradiance being relatively weak over the past few
years.
Global atmospheric temperatures maintain a strong warming trend since the 1970s
(~0.6°C), consistent with expectations of greenhouse induced warming.
Increases in hot extremes and decreases in cold extremes have continued and are expected
to amplify further.
Ice-shelves connect continental ice-sheets to the ocean. Destabilization of ice-shelves
along the Antarctic Peninsula has been widespread with 7 collapses over the past 20 years.
Signs of ice shelf weakening have been observed elsewhere than in the Antarctic Peninsula,
e.g. in the Bellingshausen and Amundsen seas, indicating a more widespread influence of
atmospheric and oceanic warming than previously thought.
There is a strong influence of ocean warming on ice sheet stability and mass balance via the
melting of ice-shelves. Anthropogenic climate change is expected to lead to further increases
in precipitation extremes, both increases in heavy precipitation and increases in drought.
Although future changes in tropical cyclone activity cannot yet be modeled, new analyses
of observational data confirm that the intensity of tropical cyclones has increased in the
past three decades in line with rising tropical ocean temperatures.
There is widespread evidence of increased melting of glaciers and ice-caps since the mid
1990s.
The contribution of glaciers and ice-caps to global sea-level has increased from 0.8
millimeters per year in the 1990s to be 1.2 millimeters per year today.
The adjustment of glaciers and ice caps to present climate alone is expected to raise sea
level by ~18 centimeters. Under warming conditions they may contribute as much as ~55
centimeters by 2100
The surface area of the Greenland ice sheet which experiences summer melt has increased
by 30% since 1979, consistent with warming air temperatures. Melt covered 50% of the ice
sheet during the record season in 2007.
The net loss of ice from the Greenland ice sheet has accelerated since the mid-1990s and is
now contributing as much as 0.7 millimeters per year to sea level rise due to both increased
melting and accelerated ice flow.
Antarctica is also losing ice mass at an increasing rate, mostly from the West Antarctic ice
sheet due to increased ice flow. Antarctica is currently contributing to sea level rise at a
rate nearly equal to Greenland.
The observed summer-time melting of Arctic sea-ice has far exceeded the worst-case
projections from climate models of IPCC AR4.
The warming commitment associated with existing atmospheric greenhouse gas levels means
it is very likely that in the coming decades the summer Arctic Ocean will become ice-free,
although the precise timing of this remains uncertain.
Satellite observations show a small increase of Antarctic sea-ice extent and changes to
seasonality, although there is considerable regional variability. This is most likely due to
changes in Southern Ocean winds associated with stratospheric ozone-depletion.
Estimates of ocean heat uptake have converged and are found to be 50% higher than
previous calculations.
Global ocean surface temperature reached the warmest ever recorded for each of June, July
and August 2009.
Ocean acidification and ocean de-oxygenation have been identified as potentially
devastating for large parts of the marine ecosystem.
Satellite measurements show sea-level is rising at 3.4 millimeters per year since these
records began in 1993. This is 80% faster than the best estimate of the IPCC Third
Assessment Report for the same time period.
Accounting for ice-sheet mass loss, sea-level rise until 2100 is likely to be at least twice as
large as that presented by IPCC AR4, with an upper limit of ~2m based on new ice-sheet
understanding.
There are several elements in the climate system that could pass a tipping point this century
due to human activities, leading to abrupt and/or irreversible change.
1 °C global warming (above 1980-1999) carries moderately significant risks of passing large
scale tipping points, and 3 °C global warming would give substantial or severe risks.
There are prospects for early warning of approaching tipping points, but if we wait until a
transition begins to be observed, in some cases it would be unstoppable.
http://www.copenhagendiagnosis.com/default.html
Link directly to pdf file:
http://www.ccrc.unsw.edu.au/Copenhagen/Copenhagen_Diagnosis_LOW.pdf
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