One of the most objective, and reasoned discussions on this topic, in my humble opinion is the research published by the British Antarctic Society:
www.antarctica.ac.uk...
First, they explain why the Antarctic is important:
Climate change - causes and effects
December 2007
Why should we study Antarctic climate?
The Antarctic region is an important regulator of global climate. The Southern Ocean is a significant sink for both heat and carbon dioxide, acting as
a buffer against human-induced climate change. The sea ice that forms around the continent each winter controls the exchange of energy between the Sun
and the Earth, and its partition between atmosphere and ocean. As sea ice forms, brine rejected from the ice increases the density of the upper ocean.
These waters then sink and form the deep ocean currents that carry heat around the globe.
Changes in global climate can have impacts on the Antarctic environment. The Southern Ocean supports a unique ecosystem that is well adapted to
present climate conditions. Changes in ocean temperatures, currents and sea ice will impact on this ecosystem, possibly changing the ocean's capacity
to absorb carbon dioxide. Warming of the atmosphere and ocean around Antarctica may lead to increased loss of mass from the Antarctic ice sheets and
hence a rise in global sea level. In order to make soundly-based predictions of how the global environment may change over the coming decades and
centuries, we need to understand the role played by the Antarctic in the Earth system.
Next, they take a reasoned look at the last 50 years:
How has Antarctic climate varied over the past 50 years?
Few continuous observations of Antarctic climate are available before the International Geophysical Year of 1957-58. Since this time, surface
temperatures have remained fairly stable over much of Antarctica, although individual station records show a high level of year-to-year variability,
which could mask any underlying long term-trend. The majority of stations in East Antarctica, including the two long-term records from the high
plateau of East Antarctica (South Pole and Vostok) show no statistically-significant warming or cooling trends1. By contrast, large and
statistically-significant warming trends are seen at stations in the Antarctic Peninsula. Over the past 50 years, the west coast of the Peninsula has
been one of the most rapidly-warming parts of the planet. Here, annual mean temperatures have risen by nearly 3°C, with the largest warming occurring
in the winter season1,2,3. This is approximately 10 times the mean rate of global warming, as reported by the Intergovernmental Panel on Climate
Change (IPCC). The east coast of the Peninsula has warmed more slowly and here the largest warming has taken place in summer and autumn3.
Significant warming has also been observed in the Southern Ocean. Upper ocean temperatures to the west of the Antarctic Peninsula have increased by
over 1°C since 19554. Within the circumpolar Southern Ocean, it is now well-established that the waters of the Antarctic Circumpolar Current (ACC)
are warming more rapidly than the global ocean as a whole. A comparison of temperature measurements from the 1990s with data from earlier decades
shows a large-scale warming of around 0.2°C in the ACC waters at around 700-1100 m depth21.
Analysis of weather balloon data collected over the past 30 years has shown that the Antarctic atmosphere has warmed below 8 km and cooled above this
height. This pattern of warming in the troposphere and cooling in the stratosphere is seen globally and is the expected signature of increases in
greenhouse gases, such as carbon dioxide. However, the 30-year warming at 5 km over the Antarctic during winter (0.75°C) is over three times the
average rate of warming at this level for the globe as a whole5.
Reliable year-round measurements of Antarctic sea ice extent are only available from the 1970s, when satellite observations first became available.
Unlike in the Arctic, where there has been a significant decline in observed sea ice extent over this period, there has been a small but
statistically-significant increase in the overall extent of Antarctic sea ice. However, there are strong geographical variations at a regional scale.
Sea ice cover has declined substantially in the seas to the west of the Antarctic Peninsula while it has increased in other parts of the
Antarctic6.
Subtle but important changes have occurred in the atmospheric circulation around Antarctica. Since the early 1960s, atmospheric pressure has dropped
over Antarctica and risen in the mid-latitudes of the Southern Hemisphere, a pattern of variability known as the Southern Hemisphere Annular Mode
(SAM)7. These changes have resulted in a strengthening of the westerly winds that blow over the Southern Ocean around Antarctica. Stronger westerlies
will impact on ocean currents, upwelling and mixing, but the consequences of such changes have yet to be fully understood.
They then discuss how recent environmental changes have affected the Antarctic:
How has recent climate change impacted on the Antarctic environment?
Recent climate change has driven significant changes in the physical and living environment of the Antarctic. Environmental change is most apparent in
the Antarctic Peninsula, where climate change has been largest. Adélie penguins, a species well adapted to sea ice conditions, have declined in
numbers and been replaced by open-water species such as chinstrap penguins8. Melting of perennial snow and ice covers has resulted in increased
colonisation by plants9. A long-term decline in the abundance of Antarctic krill in the SW Atlantic sector of the southern ocean may be associated
with reduced sea ice cover10.
Large changes have occurred in the ice cover of the Peninsula. Many glaciers have retreated11 and around 10 ice shelves that formerly fringed the
Peninsula have been observed to retreat in recent years12 and some have collapsed completely. Furthermore, 87% of glaciers along the west coast of the
AP have retreated in the last 50 years, and in the last 12 years most have accelerated. The Antarctic Peninsula is contributing to sea-level rise, at
about the same rate as Alaska Glaciers.
Analysis of global measurements of atmospheric CO2 indicates that the Southern Ocean carbon sink has weakened significantly since 1981. This reduction
in the capacity of the ocean to absorb CO2 has been attributed to increased upwelling of carbon-rich waters associated with strengthening of the
westerly winds19. Although future changes in the ability of the Southern Ocean to sequester CO2 are not completely known, this will be a key factor
that helps shape global climate.
Continued on my next post.