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The Influence of Vegetation-Atmosphere-Ocean Interaction on Climate During the Mid-Holocene

Ganopolski, Andrey, Kubatzki, Claudia, Claussen, Martin, Brovkin, Victor, Petoukhov, Vladimir·1998·Science

Abstract

Simulations with a synchronously coupled atmosphere–ocean–vegetation model show that changes in vegetation cover during the mid-Holocene, some 6000 years ago, modify and amplify the climate system response to an enhanced seasonal cycle of solar insolation in the Northern Hemisphere both directly (primarily through the changes in surface albedo) and indirectly (through changes in oceanic temperature, sea-ice cover, and oceanic circulation). The model results indicate strong synergistic effects of changes in vegetation cover, ocean temperature, and sea ice at boreal latitudes, but in the subtropics, the atmosphere–vegetation feedback is most important. Moreover, a reduction of the thermohaline circulation in the Atlantic Ocean leads to a warming of the Southern Hemisphere.

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Metadata

Authors
Ganopolski, A., Kubatzki, C., Claussen, M., Brovkin, V., & Petoukhov, V.
Venue
Science
Published
1998-06-19
Volume
280
Issue
5371
Pages
1916-1919
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2085482846
Cited by
368
References
0
FWCI
14.79
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: The Influence of Vegetation-Atmosphere-Ocean Interaction on Climate During the Mid-Holocene. https://app.cochat.ai/papers/10.1126/science.280.5371.1916
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Ganopolski, A., Kubatzki, C., Claussen, M., Brovkin, V., & Petoukhov, V. (1998). The Influence of Vegetation-Atmosphere-Ocean Interaction on Climate During the Mid-Holocene. Science. https://doi.org/10.1126/science.280.5371.1916

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.