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==Climate Change== | ==Climate Change== | ||
[[File:Sea Ice Chart.png|thumb|right|400px|NASA chart showing sea ice loss]] | |||
Recent changes in wind patterns around Antarctica have advected the sea ice farther north in some areas and not as far north in others. The net change is a slight increase in the area of sea ice in the Antarctic seas (unlike the Arctic Ocean, which is showing a much stronger decrease in the area of sea ice). Increased sea ice extent does not indicate that the Southern Ocean is cooling, since the Southern Ocean is warming. | Recent changes in wind patterns around Antarctica have advected the sea ice farther north in some areas and not as far north in others. The net change is a slight increase in the area of sea ice in the Antarctic seas (unlike the Arctic Ocean, which is showing a much stronger decrease in the area of sea ice). Increased sea ice extent does not indicate that the Southern Ocean is cooling, since the Southern Ocean is warming. | ||
The IPCC AR5 report concluded that "it is very likely" that annual mean Antarctic sea ice extent increased 1.2 to 1.8% per decade, which is 0.13 to 0.20 million km2 per decade, during the period 1979 to 2012. The effect probably has more than one cause. | The IPCC AR5 report concluded that "it is very likely" that annual mean Antarctic sea ice extent increased 1.2 to 1.8% per decade, which is 0.13 to 0.20 million km2 per decade, during the period 1979 to 2012. The effect probably has more than one cause. A separate report concluded that due to the lack of data it is not possible to determine the trend in total volume or mass of the sea ice. | ||
Implications for sub-surface temperatures and coastal currents have been identified, mainly related to changes in the southern hemispheric westerly winds, among possible implications is rapid | Implications for sub-surface temperatures and coastal currents have been identified, mainly related to changes in the southern hemispheric westerly winds, among possible implications is rapid glacier melting, thus affecting calving rates and subsequently sea ice formation. | ||
Temperatures in the atmosphere and Southern Ocean have increased during the period 1979–2004. However, sea ice grows faster than it melts, because of a weakly stratified Ocean. Thus, this mechanism is responsible for an increase in the net ice production, contributing to more sea ice. The sea ice volume increase presents about half the size of the increased freshwater supply from the Antarctic ice sheets. Modelling suggests that observed ice-drift toward the coastal regions are responsible for dynamical thickening during autumn and winter. | Temperatures in the atmosphere and Southern Ocean have increased during the period 1979–2004. However, sea ice grows faster than it melts, because of a weakly stratified Ocean. Thus, this mechanism is responsible for an increase in the net ice production, contributing to more sea ice. The sea ice volume increase presents about half the size of the increased freshwater supply from the Antarctic ice sheets. Modelling suggests that observed ice-drift toward the coastal regions are responsible for dynamical thickening during autumn and winter. | ||
A study published in 2015 found that the subsurface ocean warming of ice-shelves increased freshwater runoff simulated by models, due to basal melt, and was responsible for an increase of sea ice in the winter months. | A study published in 2015 found that the subsurface ocean warming of [[ice shelf|ice-shelves]] increased freshwater runoff simulated by models, due to basal melt, and was responsible for an increase of sea ice in the winter months. | ||
Monitoring these changes is important as this impacts the psychrophiles that live here. | Monitoring these changes is important as this impacts the [[psychrophiles]] that live here. | ||
[[Category:Climate Change]] | [[Category:Climate Change]] | ||
[[Category:Environment of Antarctica]] | |||