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What were the Primary Forcing Mechanisms of High-Frequency Holocene Climate and Glacier Variations

Bibliographic Data

ID12266108
AuthorsAtle Nesje (0000-0001-8508-5805, University of Bergen, corresponding author), Truls Johannessen (0000-0002-1671-3465, University of Bergen)
Year1992
Volume2
Issue1
Pages79-84
Publication date1992-03-01
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/095968369200200110
OpenAlexW1480291103
LanguageEN
Citations received12
References cited61

A compilation of Holocene glacial advances throughout the world is compared with summer solar insolation integrated over the Northern Hemisphere and the magnitudes of global acid fallout from volcanic eruptions north of 20°S*** estimated from the acidity signal of annual ice layers in the Crëte and Camp Century ice cores in Greenland. Correlation analysis between glacial advances versus volcanic eruptions yielded a correlation coefficient of r = 0.71. A ‘climatic forcing’ curve (solar insolation and volcanic eruptions weighted 1:1) versus glacial advances increased the correlation coefficient to r = 0.90. This suggests that the combined effect of volcanic aerosols and orbital-related Northern Hemisphere summer insolation may have been the primary forcing mechanism of worldwide climate and glacier fluctuations throughout the Holocene

Climate change · Climatology · Forcing (mathematics · Geography · Geomorphology · Glacial period · Glacier · Holocene · Ice core · Ice sheet · Insolation · Northern Hemisphere · Orbital forcing · Paleoclimatology · Physical geography · Radiative forcing · Volcano · Cryospheric studies and observations · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Geology · Oceanography · Paleontology

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Citations per year0.38
Citation span1994 - 2012 (19)
Highly citedNo
Open DOISci-Hub
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