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A Resolution Of The Antarctic Sea Ice Paradox

22.01.2014
22.01.2014 20:18 Age: 3 yrs

A new paper claims to explain the paradox of why sea ice is growing in the Antarctic despite global warming. A combination of observational data and modelling reveals the potential significance of the north and tropical Atlantic Ocean in driving change in Antarctic winds and sea ice on decadal timescales and longer.

Click to enlarge. The gradual warming of the North and Tropical Atlantic Ocean is contributing to climate change in Antarctica, a team of NYU scientists has concluded. The findings, which rely on more than three decades of atmospheric data, show new ways in which distant regional conditions are contributing to Antarctic climate change. Below, several glaciers in the Antarctic Peninsula pass between sharp mountain peaks and converge in a single calving front, as seen by Operation IceBridge while returning from a survey of the Ronne Ice Shelf on Nov. 1, 2012. NASA's Operation IceBridge is an airborne science mission to study Earth's polar ice. For more information about IceBridge, visit: www.nasa.gov/icebridge. Courtesy: Jefferson Beck/NASA IceBridge, National Science Foundation

 

Over the past few decades, Antarctica has experienced dramatic climate change, with its peninsula exhibiting the strongest warming of any region on the planet. During its summer, Antarctic changes have been attributed to greenhouse gas increase and stratospheric ozone loss. However, less clear are the forces behind climate changes that occur during its winter. In addition, the effects of these changes during the cold season are complex, further stifling efforts to find the atmospheric culprit.

 

Different candidate 

 

 

To address this question, the NYU researchers focused on a different candidate: the Atlantic Ocean, which has been overlooked as a force behind Antarctic climate change.

 

 

 

Using a time-series analysis, in which the scientists matched changes in the North and Tropical Atlantic's SST with subsequent changes in Antarctic climate, the researchers found strong correlations. Specifically, they observed that warming Atlantic waters were followed by changes in sea-level pressure in the Antarctic's Amundsen Sea. In addition, these warming patterns also preceded redistribution of sea ice between the Antarctic's Ross and Amundsen-Bellingshausen-Weddell Seas.

 

David Holland, co-author of the study, a professor at NYU's Courant Institute and past director of NYU's Center for Atmospheric Ocean Science, explained that the research consisted of two parts, which incorporated both the use of observational data and computer modeling.

 

Correlation

The first part of the study, using the observational data, found a link, or correlation, between the Atlantic and Antarctic data sets. But a correlation means simply that two things appear to happen in conjunction and does not explain what may be causing a phenomenon.

 

The second used a global atmospheric model, which allowed the researchers to create a simulated warming of the North Atlantic. The model responded, as the researchers had suspected, by "changing" the climate in Antarctica.

 

"While our data analysis showed a correlation, it was the use of a state-of-the-art computer model that allowed us to see that North Atlantic warming was causing Antarctic climate change and not vice versa," he said.

 

The study's findings raise a number of deeper questions, such as, is Antarctic sea-ice change fundamentally different from the well-reported changes in the Arctic? In contrast to the sea-ice decline over the Arctic, Antarctic sea ice has not diminished. Rather, it has redistributed itself in ways that have perplexed scientists, with declines in some areas and increases in others.

 

Holland observes: "From this study, we are learning just how Antarctic sea-ice redistributes itself, and also finding that the underlying mechanisms controlling Antarctic sea ice are completely distinct from those in the Arctic."

 

 

Text of Nature press release:

 

 

 

 

The authors propose that the tropical and north Atlantic have the potential to affect ocean circulation and sea-level change.


Abstract


Citation

 

Read the abstract and get the paper here

 

Source

News release from New York University issued via the EurekAlert! service of the AAAS here.