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Northern Hemisphere Climate Variability

Character, Forcing Mechanisms, and Significance of the North Atlantic/Arctic Oscillation

Bibliographic Data

ID7784889
AuthorsDagmar Budikova (0000-0001-6661-7685, corresponding author)
Year2012
Volume6
Issue7
Pages401-422
Publication date2012-07-01
Open AccessYes
TypeARTICLE
VenueGeography Compass (JOURNAL)
Journal identifiersISSN: 1749-8198 • E-ISSN: 1749-8198
PublisherWiley (PUBLISHER • GB)
DOI10.1111/j.1749-8198.2012.00498.x
OpenAlexW1686785051
LanguageEN
References cited78

The North Atlantic Oscillation (NAO) has long been recognized as an important source of climate variability over the north Atlantic region. The NAO is often referred to as the regional expression of the Arctic Oscillation that reflects a redistribution of atmospheric mass between the Arctic and the middle latitudes of the Northern Hemisphere (NH). This review highlights our current understanding of these prominent teleconnection patterns and discusses outstanding questions and challenges that scientists face as they continue to build our knowledge of climate variability and change across the NH. The work discusses the strengths and limitations of the multitude of methods by which these phenomena have been defined, while highlighting recent changes in their character. Addressed also are the various internal and external forcing mechanisms that shape these phenomena and ultimately help define their predictive nature

Arctic · Arctic oscillation · Atlantic multidecadal oscillation · Circumpolar star · Climatology · El Niño Southern Oscillation · Geography · North Atlantic oscillation · Northern Hemisphere · Teleconnection · The arctic · Arctic and Antarctic ice dynamics · Climate variability and models · Meteorological Phenomena and Simulations · Geology · Oceanography

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Highly citedNo

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