Tiempo Climate PortalNorth Atlantic Oscillation |
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Featured sitesThe Global Coral Reef Monitoring Network works to improve management and conservation of coral reefs by providing manuals, equipment, databases, training, problem solving, and helps with finding funds for reef monitoring. The Cities for Climate Protection Campaign assists cities to adopt policies and implement quantifiable measures to reduce local greenhouse gas emissions, improve air quality, and enhance urban livebility and sustainability. zerocarbonbritain details how Britain can eliminate emissions from fossil fuels in 20 years and break dependence on imported energy. Plan B, from the Earth Policy Institute, details how to rescue a planet under stress by cutting carbon emissions 80 per cent by 2020. And finally,Lorraine Berry was commissioned by the Environmental Change Network to produce a web-based creative work, as Seasons Change, drawing on data and knowledge concerning climate change. About the PortalThe Tiempo Climate Portal provides access to carefully selected documents, websites and other resources concerned with climate and sustainable development. It is edited by Mick Kelly and Sarah Granich and maintained by Mick Kelly and Mike Salmon. Part of the Tiempo Climate Cyberlibrary, Tiempo Climate Newswatch is hosted by the Climatic Research Unit, School of Environmental Sciences, University of East Anglia. The Tiempo Climate Cyberlibrary is a co-production of the Stockholm Environment Institute and the International Institute for Environment and Development, sponsored by the Swedish International Development Cooperation Agency. While every effort is made to ensure that information on this site, and on other sites that are referenced here, is accurate, no liability for loss or damage resulting from use of this information can be accepted. |
The North Atlantic Oscillation is a major disturbance of the atmospheric circulation and climate of the North Atlantic-European region, linked to a waxing and waning of the dominant middle-latitude westerly wind flow during winter. The North Atlantic Oscillation Index is based on the pressure difference between various stations to the north (Iceland) and south (Azores) of the middle latitude westerly flow. It is, therefore, a measure of the strength of these winds. Strictly, it should only be used for the winter period. Discussion When the North Atlantic Oscillation Index is positive, the westerly flow across the North Atlantic and western Europe is enhanced, along with the Iceland Low and the Azores High. During the winter half-year, the strengthened westerly winds bring warmer, maritime air over northwest Europe causing a rise in temperature. At the same time, enhanced northerly flow over the northeast Atlantic results in a drop in temperatures over the area. When the Index is low, the opposite occurs with temperatures falling over northwest Europe and rising over northwest Atlantic. The net result is a "sea-saw" in temperatures across the North Atlantic-European sector, as well as changes in other climate variables such as precipitation and sea-ice extent. The North Atlantic Oscillation exerts a strong influence on year-to-year climate variability and there is evidence of longer-term trends in this phenomenon. It is related to the shorter-term shift between zonal and meridional circulation types that occurs on the day-to-day timescale and is known as the "index cycle". Data availability The North Atlantic Oscillation Index can be downloaded for the period since 1821 and a regular monthly update is available. On the Web An information sheet on the North Atlantic Oscillation is available. Acknowledgements The North Atlantic Oscillation Index is maintained by Phil Jones, Climatic Research Unit, University of East Anglia. |
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