Attribution of regional-scale temperature changes to anthropogenic and natural causes

Details Attribution of regional-scale temperature changes to anthropogenic and natural causes Attribution of regional-scale temperature changes to anthropogenic and natural causes

Jul 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30n...2s&link_type=abstract

Geophysical Research Letters, Volume 30, Issue 14, pp. 2-1, CiteID 1728, DOI 10.1029/2003GL017324

Physics

53

Global Change: Atmosphere (0315, 0325), Meteorology And Atmospheric Dynamics: Climatology (1620), Meteorology And Atmospheric Dynamics: Numerical Modeling And Data Assimilation

Scientific paper

The causes of twentieth century temperature change in six separate land areas of the Earth have been determined by carrying out a series of optimal detection analyses. The warming effects of increasing greenhouse gas concentrations have been detected in all the regions examined, including North America and Europe. In most regions, cooling from sulfate aerosols counteracts some of the greenhouse warming, and there is some evidence for reduced net aerosol cooling in Asia, possibly as a result of warming from black carbon.

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