Articles | Volume 18, issue 6
https://doi.org/10.5194/bg-18-2181-2021
https://doi.org/10.5194/bg-18-2181-2021
Research article
 | 
25 Mar 2021
Research article |  | 25 Mar 2021

Examining the sensitivity of the terrestrial carbon cycle to the expression of El Niño

Lina Teckentrup, Martin G. De Kauwe, Andrew J. Pitman, and Benjamin Smith

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (09 Dec 2020) by Alexandra Konings
AR by Lina Teckentrup on behalf of the Authors (18 Dec 2020)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (23 Dec 2020) by Alexandra Konings
RR by Anonymous Referee #1 (06 Jan 2021)
RR by Anonymous Referee #2 (14 Jan 2021)
ED: Publish subject to technical corrections (24 Jan 2021) by Alexandra Konings
AR by Lina Teckentrup on behalf of the Authors (02 Feb 2021)  Author's response   Manuscript 
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Short summary
The El Niño–Southern Oscillation (ENSO) describes changes in the sea surface temperature patterns of the Pacific Ocean. This influences the global weather, impacting vegetation on land. There are two types of El Niño: central Pacific (CP) and eastern Pacific (EP). In this study, we explored the long-term impacts on the carbon balance on land linked to the two El Niño types. Using a dynamic vegetation model, we simulated what would happen if only either CP or EP El Niño events had occurred.
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