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Several hypotheses for how Arctic warming may be influencing mid-latitude weather patterns have been proposed recently. For example, Arctic warming could lead to a weakened jet stream. Or Arctic sea ice loss could lead to an increase of snow on high-latitude land, which in turn would impact the jet stream, resulting in cold Eurasian and North American winters. These and other potential connections are the subject of active research. This publication summarizes a workshop convened in September 2013 by the National Research Council to review our current understanding and to discuss research needed to better understand proposed linkages.
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Workshop
ยท2014
The Arctic has been undergoing significant changes in recent years. Average temperatures are rising twice as fast as they are elsewhere in the world. The extent and thickness of sea ice is rapidly declining. Such changes may have an impact on atmospheric conditions outside the region. Several hypoth...
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Description
Rising global average temperatures, and especially intense warming in the northern polar regions, are leading to a rapid loss of the sea ice cap that covers the Arctic ocean. Emerging research may indicate that large losses of Arctic sea ice cover can have dramatic impacts upon weather patterns across the heavily populated northern mid-latitudes, and that such impacts could increase as ice cover continues to retreat in the coming decades. An ad hoc committee will plan and conduct a public workshop that brings together a diverse array of experts to examine linkages between Arctic sea ice and mid latitude weather patterns. The outcome of this activity will be a report that summarizes the workshop presentations and discussions to address the following questions:
- What do we currently understand about the mechanisms that link declines in Arctic sea ice cover, loss of high-latitude snow cover, changes in arctic-region energy fluxes, atmospheric circulation patterns, and the occurrence of extreme weather events?
- What may be the possible implications of more severe loss (and eventually, total loss) of summer Arctic sea ice upon weather patterns at lower latitudes?
- What are the major gaps in our understanding, and what sort of observational and/or modeling efforts are needed to fill those gaps?
- What are the current opportunities and limitations for using Arctic sea ice predictions to assess the risk of temperature/precipitation anomalies and extreme weather events over northern continents? How might these capabilities improve over time?
Contributors
Sponsors
NASA
National Oceanic and Atmospheric Administration
National Science Foundation
Staff
Katherine C Thomas
Lead