BOND EVENTS

John A. Matthews

doi:10.4135/9781446247501

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BOND EVENTS

Edited by:
John A. Matthews
In:Encyclopedia of Environmental Change
Chapter DOI:https://doi.org/10.4135/9781446247501.n466
Subject:Environmental Sciences (general), Environmental Technology, Policy & Management

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Inferred climatic events approxi-mately 1,500 years apart during the holocene, as iden-tified by Gerard Bond from ice-rafted debris in the North Atlantic, and claimed by Bond et al. (1997) to be of the same pacing as dansgaard-oeschger (D-O)events. Bond events should not be confused with Late Pleistocene bond cycles. Similar events have been recognised in other proxy records, such as glacier variations and lake-level variations.

Frank M.ChambersUniversity of Gloucestershire

http://dx.doi.org/10.4135/9781446247501.n466

10.4135/9781446247501.n466

BondG, KromerB, BeerJ et al. (2001) Persistent solar influence on North Atlantic climate during the Holocene. Science294: 2130–2136.

BondG, ShowersW, ChesebyM et al. (1997) A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science278: 1257–1266.

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