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The Arctic Oscillation: A Key To This Winter's Cold -- And A Warmer Planet

Date:
February 25, 2003
Source:
National Center For Atmospheric Research
Summary:
Why has the Arctic warmed so dramatically in recent years? How does the Arctic's circulation keep frigid air over the poles and sometimes allow it to spill across the United States? And how might global change affect the behavior of this circulation?

BOULDER -- Why has the Arctic warmed so dramatically in recent years? How does the Arctic's circulation keep frigid air over the poles and sometimes allow it to spill across the United States? And how might global change affect the behavior of this circulation?

Clara Deser, from the National Center for Atmospheric Research (NCAR), will address these and other questions in a presentation in Denver on February 17 at the annual meeting of the American Association for the Advancement of Science. Deser will summarize the structure and effects of the Arctic Oscillation (AO) as part of the symposium "El Nino, Monsoon, Arctic Oscillation, and Global Warming."

Although the AO has been recognized by various names for many years, it has become a topic of keen research interest only in the last decade. The AO index describes the relative intensity of a semipermanent low-pressure center over the North Pole. A band of upper-level winds circulates around this center, forming a vortex. When the AO index is positive and the vortex intense, the winds tighten like a noose around the North Pole, locking cold air in place. A negative AO and weak vortex (as has been the case most of this winter) allow intrusions of cold air to plunge southward into North America, Europe, and Asia. Apart from variations like this winter's, the index has been mostly positive in wintertime since the late 1980s.

"The Arctic Oscillation has strengthened in recent decades, contributing to the unusual warmth over the Northern Hemisphere land masses," says Deser. "This has led to the speculation that the AO may be affected by increasing greenhouse gas concentrations and that it may, in turn, enhance global warming." Deser will discuss recent computer-model simulations that support this view. She will also address the relationship between the AO and ozone, which has been measurably depleted across the region in recent years.

About the presenter: Clara Deser has been a scientist in the NCAR Climate and Global Dynamics Division since 1997. Her research focuses on analyzing climate variability, including the interplay among the atmosphere, oceans, and ice. She has also studied upper-ocean dynamics and the El Nino/Southern Oscillation. The author or coauthor of more than 30 scientific papers, Deser received the Meisinger Award from the American Meteorological Society in 1998. She holds a Ph.D. in atmospheric science from the University of Washington.

The University Corporation for Atmospheric Research manages the National Center for Atmospheric Research under primary sponsorship by the National Science Foundation. Opinions, findings, conclusions, or recommendations expressed in this publication are those of the author(s) and do not necessarily reflect the views of the National Science Foundation.


Story Source:

The above story is based on materials provided by National Center For Atmospheric Research. Note: Materials may be edited for content and length.


Cite This Page:

National Center For Atmospheric Research. "The Arctic Oscillation: A Key To This Winter's Cold -- And A Warmer Planet." ScienceDaily. ScienceDaily, 25 February 2003. <www.sciencedaily.com/releases/2003/02/030225071423.htm>.
National Center For Atmospheric Research. (2003, February 25). The Arctic Oscillation: A Key To This Winter's Cold -- And A Warmer Planet. ScienceDaily. Retrieved July 28, 2014 from www.sciencedaily.com/releases/2003/02/030225071423.htm
National Center For Atmospheric Research. "The Arctic Oscillation: A Key To This Winter's Cold -- And A Warmer Planet." ScienceDaily. www.sciencedaily.com/releases/2003/02/030225071423.htm (accessed July 28, 2014).

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