Comment on cp-2022-35 Article Swipe
Julia E. Weiffenbach
,
Michiel Baatsen
,
Henk A. Dijkstra
,
Anna S. von der Heydt
,
Ayako Abe‐Ouchi
,
Esther C. Brady
,
Wing‐Le Chan
,
Deepak Chandan
,
Mark A. Chandler
,
Camille Contoux
,
Ran Feng
,
Chuncheng Guo
,
Zixuan Han
,
Alan M. Haywood
,
Qiang Li
,
Xiangyu Li
,
Gerrit Lohmann
,
Daniel J. Lunt
,
Kerim H. Nisancioglu
,
Bette L. Otto‐Bliesner
,
W. R. Peltier
,
Gilles Ramstein
,
Linda E. Sohl
,
Christian Stepanek
,
Ning Tan
,
Julia C. Tindall
,
Charles J. R. Williams
,
Qiong Zhang
,
Zhongshi Zhang
·
YOU?
·
· 2022
· Open Access
·
· DOI: https://doi.org/10.5194/cp-2022-35-rc1
YOU?
·
· 2022
· Open Access
·
· DOI: https://doi.org/10.5194/cp-2022-35-rc1
The mid-Pliocene warm period (3.264–3.025 Ma) is the most recent geological period in which the atmospheric CO2 concentration was approximately equal to the concentration we measure today (ca. 400 ppm). Sea surface temperature (SST) proxies indicate above-average warming over the North Atlantic in the mid-Pliocene with respect to the pre-industrial period, which may be linked to an intensified Atlantic Meridional Overturning Circulation (AMOC). Earlier results from the Pliocene Model Intercomparison Project Phase 2 (PlioMIP2) show that the ensemble simulates a stronger AMOC in the mid-Pliocene than in the pre-industrial. However, no consistent relationship between the stronger mid-Pliocene AMOC and either the Atlantic northward ocean heat transport (OHT) or average North Atlantic SSTs has been found. In this study, we look further into the drivers and consequences of a stronger AMOC in mid-Pliocene compared to pre-industrial simulations in PlioMIP2. We find that all model simulations with a closed Bering Strait and Canadian Archipelago show reduced freshwater transport from the Arctic Ocean into the North Atlantic. The resulting increase in salinity in the subpolar North Atlantic and Labrador Sea drives the stronger AMOC in the mid-Pliocene. To investigate the dynamics behind the ensemble's variable response of the total Atlantic OHT to the stronger AMOC, we separate the Atlantic OHT into two components associated with either the overturning circulation or the wind-driven gyre circulation. While the ensemble mean of the overturning component is increased significantly in magnitude in the mid-Pliocene, it is partly compensated by a reduction of the gyre component in the northern subtropical gyre region. This indicates that the lack of relationship between the total OHT and AMOC is due to changes in OHT by the subtropical gyre. The overturning and gyre components should therefore be considered separately to gain a more complete understanding of the OHT response to a stronger mid-Pliocene AMOC. In addition, we show that the AMOC exerts a stronger influence on North Atlantic SSTs in the mid-Pliocene than in the pre-industrial, providing a possible explanation for the improved agreement of the PlioMIP2 ensemble mean SSTs with reconstructions in the North Atlantic.
Related Topics
Concepts
Ocean gyre
North Atlantic Deep Water
Climatology
Oceanography
Archipelago
North Atlantic oscillation
Tropical Atlantic
Thermohaline circulation
Period (music)
Ocean current
Gulf Stream
Coupled model intercomparison project
Geology
Shutdown of thermohaline circulation
Climate model
Sea surface temperature
Climate change
Subtropics
Physics
Fishery
Acoustics
Biology
Metadata
- Type
- peer-review
- Language
- en
- Landing Page
- https://doi.org/10.5194/cp-2022-35-rc1
- OA Status
- gold
- References
- 29
- Related Works
- 10
- OpenAlex ID
- https://openalex.org/W4283079549
All OpenAlex metadata
Raw OpenAlex JSON
- OpenAlex ID
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https://openalex.org/W4283079549Canonical identifier for this work in OpenAlex
- DOI
-
https://doi.org/10.5194/cp-2022-35-rc1Digital Object Identifier
- Title
-
Comment on cp-2022-35Work title
- Type
-
peer-reviewOpenAlex work type
- Language
-
enPrimary language
- Publication year
-
2022Year of publication
- Publication date
-
2022-06-17Full publication date if available
- Authors
-
Julia E. Weiffenbach, Michiel Baatsen, Henk A. Dijkstra, Anna S. von der Heydt, Ayako Abe‐Ouchi, Esther C. Brady, Wing‐Le Chan, Deepak Chandan, Mark A. Chandler, Camille Contoux, Ran Feng, Chuncheng Guo, Zixuan Han, Alan M. Haywood, Qiang Li, Xiangyu Li, Gerrit Lohmann, Daniel J. Lunt, Kerim H. Nisancioglu, Bette L. Otto‐Bliesner, W. R. Peltier, Gilles Ramstein, Linda E. Sohl, Christian Stepanek, Ning Tan, Julia C. Tindall, Charles J. R. Williams, Qiong Zhang, Zhongshi ZhangList of authors in order
- Landing page
-
https://doi.org/10.5194/cp-2022-35-rc1Publisher landing page
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YesWhether a free full text is available
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goldOpen access status per OpenAlex
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https://doi.org/10.5194/cp-2022-35-rc1Direct OA link when available
- Concepts
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Ocean gyre, North Atlantic Deep Water, Climatology, Oceanography, Archipelago, North Atlantic oscillation, Tropical Atlantic, Thermohaline circulation, Period (music), Ocean current, Gulf Stream, Coupled model intercomparison project, Geology, Shutdown of thermohaline circulation, Climate model, Sea surface temperature, Climate change, Subtropics, Physics, Fishery, Acoustics, BiologyTop concepts (fields/topics) attached by OpenAlex
- Cited by
-
0Total citation count in OpenAlex
- References (count)
-
29Number of works referenced by this work
- Related works (count)
-
10Other works algorithmically related by OpenAlex
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| primary_location.license_id | https://openalex.org/licenses/cc-by |
| primary_location.is_accepted | True |
| primary_location.is_published | True |
| primary_location.raw_source_name | |
| primary_location.landing_page_url | https://doi.org/10.5194/cp-2022-35-rc1 |
| publication_date | 2022-06-17 |
| publication_year | 2022 |
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