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Why Ice Minima Occurred in 2007, '08 and '09

Why Ice Minima Occurred in 2007, '08 and '09
Abstract Category: 
1.1. Advances in Understanding Arctic System Components
Type: 
Poster
Jia Wang1
1NOAA Great Lakes Environmental Research Laboratory, 4840 S. State Road, Ann Arbor, MI, 48108, USA, Phone 734-741-2281, Fax 734-741-2055, jia [dot] wang [at] noaa [dot] gov

The record low arctic sea ice occurred in September 2007, followed by the second lowest in 2008 and the third lowest in 2009. Although the Dipole Anomaly (DA) has been identified as the major driver, what are the mechanisms for arctic sea ice to gradually recover? This study examines these three cases in a great detail to search for dynamic and thermodynamic sound mechanisms, along with historical observations. It comes to the conclusion that under the thin-ice preconditioning (warming) during winter season by a strong positive Arctic Oscillation (AO) in the 2009 winter, local meridional wind anomaly associated DA during winter to summer is a major forcing for sea ice recovery. Other mechanisms will be discussed.

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National Science Foundation | Division of Arctic Sciences
National Science Foundation
National Oceanic and Atmospheric Administration
National Oceanic and Atmospheric Administration
International Arctic Systems for Observing the Atmosphere
International Arctic Systems for Observing the Atmosphere
Study of Environmental Arctic Change
Study of Environmental Arctic Change
Arctic System Science Program
Arctic System Science Program
US Arctic Research Commission
US Arctic Research Commission
North Slope Science Initiative
North Slope Science Initiative
International Arctic Science Committee
International Arctic Science Committee
Arctic Ocean Sciences Board
Arctic Ocean Sciences Board
Alaska Ocean Observing System
Alaska Ocean Observing System
Department of Energy
Department of Energy
National Aeronautics and Space Administration
National Aeronautics and Space Administration
World Wildlife Fund
WWF
Association of Polar Early Career Scientists
Association of Polar Early Career Scientists
Bureau of Land Management
Bureau of Land Management
International Study of Arctic Change
International Study of Arctic Change
ArcticNet
ArcticNet
DAMOCLES
Developing Arctic Modeling and Observing Capabilities for Long-term Environmental Studies

This work is supported by the National Science Foundation (NSF) under the ARCUS Cooperative Agreement ARC-0618885. Any opinions, findings, and conclusions or recommendations expressed do not necessarily reflect the views of the NSF.