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Climate science from climate scientists...
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RealClimate is a commentary site on climate science by working climate scientists for the interested public and journalists and has been operating since Dec 2004. We aim to provide the context sometimes missing in mainstream commentary on climate science. The discussion here is mostly restricted to scientific topics though we maintain open threads for the political or economic implications of the science and for discussions of possible solutions. All posts are signed by the author(s), except ‘group’ posts which are collective efforts from the whole team. Please note this is a moderated forum.
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In addition to the category indexing on the side bar, we have set out a more thematic index here to help you find your way through the content on the site. [Note: this was kept up-to-date through about 2008. For more recent articles, please use the search function.]
Themes: Aerosols, Arctic and Antarctic climate, Atmospheric Science, Climate modelling, Climate sensitivity, Extreme events, Global warming, Greenhouse gases, Mitigation of Climate Change, Present-day observations, Oceans, Paleo-climate, Responses to common contrarian arguments, The Practice of Science, Solar forcing, Projections of future climate, Climate in the media, Meeting Reports, Miscellaneous.
If you are looking for introductions to the whole topic, start here.
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Measure of the pressure gradient between the polar and subpolar regions of the Southern Hemisphere. Term was introduced by Thompson and Wallace (2000). More information on the AAO can be found here. See also Arctic Oscillation (“AO”).
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Forcing due to human, rather than natural, factors. Such factors include increased greenhouse gas concentrations associated with fossil fuel burning, sulphate aerosols produced as an industrial by-product, human-induced changes in land surface properties among other things.
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Measure of the pressure gradient between the polar and subpolar regions of the Northern Hemisphere. The term was introduced by Thompson and Wallace (2000). More information on the AO can be found here. See also North Atlantic Oscillation”(NAO”).
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A multidecadal (50-80 year timescale) pattern of North Atlantic ocean-atmosphere variability whose existence has been argued for based on statistical analyses of observational and proxy climate data, and coupled Atmosphere-Ocean General Circulation Model (“AOGCM”) simulations. This pattern is believed to describe some of the observed early 20th century (1920s-1930s) high-latitude Northern Hemisphere warming and some, but not all, of the high-latitude warming observed in the late 20th century. The term was introduced in a summary by Kerr (2000) of a study by Delworth and Mann (2000).
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Fully coupled atmosphere-ocean model of the three-dimensional global climate. See also ‘General Circulation Model (GCM)’.
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Approach to reconstructing a target large-scale climate field from predictors employing multivariate regression methods. CFR methods have been applied both to filling spatial gaps in early instrumental climate data sets, and to the problem of reconstructing past climate patterns from ‘climate proxy’ data.
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