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  Earth system model simulations show different feedback strengths of the terrestrial carbon cycle under glacial and interglacial conditions

Adloff, M., Reick, C. H., & Claussen, M. (2018). Earth system model simulations show different feedback strengths of the terrestrial carbon cycle under glacial and interglacial conditions. Earth System Dynamics, 9, 413-425. doi:10.5194/esd-9-413-2018.

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Item Permalink: https://hdl.handle.net/21.11116/0000-0001-3758-F Version Permalink: https://hdl.handle.net/21.11116/0000-000B-0A9D-A
Genre: Journal Article

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esd-9-413-2018.pdf (Publisher version), 3MB
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 Creators:
Adloff, M.1, Author
Reick, Christian H.2, Author           
Claussen, Martin3, Author                 
Affiliations:
1MPI for Meteorology, Max Planck Society, Bundesstraße 53, 20146 Hamburg, DE, ou_913545              
2Global Vegetation Modelling, The Land in the Earth System, MPI for Meteorology, Max Planck Society, ou_913562              
3Director’s Research Group LES, The Land in the Earth System, MPI for Meteorology, Max Planck Society, ou_913564              

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Language(s): eng - English
 Dates: 2018-042018-04
 Publication Status: Issued
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 Table of Contents: -
 Rev. Type: Peer
 Identifiers: DOI: 10.5194/esd-9-413-2018
BibTex Citekey: esd-9-413-2018
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Title: Earth System Dynamics
Source Genre: Journal
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Pages: - Volume / Issue: 9 Sequence Number: - Start / End Page: 413 - 425 Identifier: -