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Causes of Climate Change Over the Past 1000 Years

Bibliographic Data

ID23362512
AuthorsTony Crowley (0000-0002-5951-6111, Texas A&M University, corresponding author), Thomas J Crowley (Texas A&M University)
Year2000
Volume289
Issue5477
Pages270-277
Publication date2000-07-14
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueScience (JOURNAL)
Journal identifiersISSN: 0036-8075 • E-ISSN: 0193-4511
PublisherAmerican Association for the Advancement of Science (AAAS) (PUBLISHER)
DOI10.1126/science.289.5477.270
PMID10894770
OpenAlexW2130256070
LanguageEN
Citations received173
References cited77

Recent reconstructions of Northern Hemisphere temperatures and climate forcing over the past 1000 years allow the warming of the 20th century to be placed within a historical context and various mechanisms of climate change to be tested. Comparisons of observations with simulations from an energy balance climate model indicate that as much as 41 to 64% of preanthropogenic (pre-1850) decadal-scale temperature variations was due to changes in solar irradiance and volcanism. Removal of the forced response from reconstructed temperature time series yields residuals that show similar variability to those of control runs of coupled models, thereby lending support to the models' value as estimates of low-frequency variability in the climate system. Removal of all forcing except greenhouse gases from the ∼1000-year time series results in a residual with a very large late-20th-century warming that closely agrees with the response predicted from greenhouse gas forcing. The combination of a unique level of temperature increase in the late 20th century and improved constraints on the role of natural variability provides further evidence that the greenhouse effect has already established itself above the level of natural variability in the climate system. A 21st-century global warming projection far exceeds the natural variability of the past 1000 years and is greater than the best estimate of global temperature change for the last interglacial.

Atmospheric sciences · Climate change · Climate model · Climatology · Context (archaeology) · Forcing (mathematics) · Glacial period · Global warming · Greenhouse gas · Interglacial · Northern Hemisphere · Radiative forcing · Solar irradiance · Solar variation · Environmental Science · Geology · Geology and Paleoclimatology Research · Plant Water Relations and Carbon Dynamics · Tree-ring climate responses

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Unique citing works173
Citations per year6,92
Citation span2001 - 2026 (26)
Citation velocitycurrent
Highly citedYes
Citation typesNeutral: 147
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