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Detecting climatic change signals: Are there any fingerprints'

Journal Article · · Science (Washington, D.C.); (United States)
 [1]
  1. Stanford Univ., CA (United States)
Projected changes in the Earth's climate can be driven from a combined set of forcing factors consisting of regionally heterogeneous anthropogenic and natural aerosols and land use changes, as well as global-scale influences from solar variability and transient increases in human-produced greenhouse gases. Thus, validation of climate model projections that are driven only by increases in greenhouse gases can be inconsistent when one attempts the validation by looking for a regional or time-evolving fingerprint' of such projected changes in real climatic data. Until climate models are driven by time-evolving, combined, multiple, and heterogeneous forcing factors, the best global climatic change fingerprint' will probably remain a many-decades average of hemispheric- to global-scale trends in surface air temperatures. Century-long global warming (or cooling) trends of 0.5[degrees]C appear to have occurred infrequently over the past several thousand years - perhaps only once or twice a millennium, as proxy records suggest. This implies an 80 to 90 percent heuristic likelihood that the 20th-century 0.5 [+-] 0.2[degrees]C warming trend is not a wholly natural climatic fluctuation.
OSTI ID:
7239911
Journal Information:
Science (Washington, D.C.); (United States), Journal Name: Science (Washington, D.C.); (United States) Vol. 263:5145; ISSN SCIEAS; ISSN 0036-8075
Country of Publication:
United States
Language:
English