Seasonal variability of the surface ocean carbon cycle: A synthesis

Abstract The seasonal cycle is the dominant mode of variability in the air‐sea CO 2 flux in most regions of the global ocean, yet discrepancies between different seasonality estimates are rather large. As part of the Regional Carbon Cycle Assessment and Processes phase 2 project (RECCAP2), we synthe...

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Published in:Global Biogeochemical Cycles
Main Authors: Rodgers, Keith, B, Schwinger, Jörg, Fassbender, Andrea, J, Landschützer, Peter, Yamaguchi, Ryohei, Frenzel, Hartmut, Stein, Karl, Müller, Jens, Daniel, Goris, Nadine, Sharma, Sahil, Bushinsky, Seth, Chau, Thi‐tuyet‐trang, Gehlen, Marion, Gallego, M. Angeles, Gloege, Lucas, Gregor, Luke, Gruber, Nicolas, Hauck, Judith, Iida, Yosuke, Ishii, Masao, Keppler, Lydia, Kim, Ji‐eun, Schlunegger, Sarah, Tjiputra, Jerry, Toyama, Katsuya, Vaittinada Ayar, Pradeebane, Velo, Antón
Other Authors: Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics (MERMAID), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), NORCE Norwegian Research Center, Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2023
Subjects:
Online Access:https://hal.science/hal-04191390
https://hal.science/hal-04191390/document
https://hal.science/hal-04191390/file/Global%20Biogeochemical%20Cycles%20-%202023%20-%20Rodgers.pdf
https://doi.org/10.1029/2023gb007798
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record_format openpolar
institution Open Polar
collection HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives)
op_collection_id ftceafr
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
Rodgers, Keith, B
Schwinger, Jörg
Fassbender, Andrea, J
Landschützer, Peter
Yamaguchi, Ryohei
Frenzel, Hartmut
Stein, Karl
Müller, Jens, Daniel
Goris, Nadine
Sharma, Sahil
Bushinsky, Seth
Chau, Thi‐tuyet‐trang
Gehlen, Marion
Gallego, M. Angeles
Gloege, Lucas
Gregor, Luke
Gruber, Nicolas
Hauck, Judith
Iida, Yosuke
Ishii, Masao
Keppler, Lydia
Kim, Ji‐eun
Schlunegger, Sarah
Tjiputra, Jerry
Toyama, Katsuya
Vaittinada Ayar, Pradeebane
Velo, Antón
Seasonal variability of the surface ocean carbon cycle: A synthesis
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
description Abstract The seasonal cycle is the dominant mode of variability in the air‐sea CO 2 flux in most regions of the global ocean, yet discrepancies between different seasonality estimates are rather large. As part of the Regional Carbon Cycle Assessment and Processes phase 2 project (RECCAP2), we synthesize surface ocean p CO 2 and air‐sea CO 2 flux seasonality from models and observation‐based estimates, focusing on both a present‐day climatology and decadal changes between the 1980s and 2010s. Four main findings emerge: First, global ocean biogeochemistry models (GOBMs) and observation‐based estimates ( p CO 2 products) of surface p CO 2 seasonality disagree in amplitude and phase, primarily due to discrepancies in the seasonal variability in surface DIC. Second, the seasonal cycle in p CO 2 has increased in amplitude over the last three decades in both p CO 2 products and GOBMs. Third, decadal increases in p CO 2 seasonal cycle amplitudes in subtropical biomes for both p CO 2 products and GOBMs are driven by increasing DIC concentrations stemming from the uptake of anthropogenic CO 2 (C ant ). In subpolar and Southern Ocean biomes, however, the seasonality change for GOBMs is dominated by C ant invasion, whereas for p CO 2 products an indeterminate combination of C ant invasion and climate change modulates the changes. Fourth, biome‐aggregated decadal changes in the amplitude of p CO 2 seasonal variability are largely detectable against both mapping uncertainty (reducible) and natural variability uncertainty (irreducible), but not at the gridpoint scale over much of the northern subpolar oceans and over the Southern Ocean, underscoring the importance of sustained high‐quality seasonally‐resolved measurements over these regions.
author2 Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)
Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics (MERMAID)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)
NORCE Norwegian Research Center
Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR)
format Article in Journal/Newspaper
author Rodgers, Keith, B
Schwinger, Jörg
Fassbender, Andrea, J
Landschützer, Peter
Yamaguchi, Ryohei
Frenzel, Hartmut
Stein, Karl
Müller, Jens, Daniel
Goris, Nadine
Sharma, Sahil
Bushinsky, Seth
Chau, Thi‐tuyet‐trang
Gehlen, Marion
Gallego, M. Angeles
Gloege, Lucas
Gregor, Luke
Gruber, Nicolas
Hauck, Judith
Iida, Yosuke
Ishii, Masao
Keppler, Lydia
Kim, Ji‐eun
Schlunegger, Sarah
Tjiputra, Jerry
Toyama, Katsuya
Vaittinada Ayar, Pradeebane
Velo, Antón
author_facet Rodgers, Keith, B
Schwinger, Jörg
Fassbender, Andrea, J
Landschützer, Peter
Yamaguchi, Ryohei
Frenzel, Hartmut
Stein, Karl
Müller, Jens, Daniel
Goris, Nadine
Sharma, Sahil
Bushinsky, Seth
Chau, Thi‐tuyet‐trang
Gehlen, Marion
Gallego, M. Angeles
Gloege, Lucas
Gregor, Luke
Gruber, Nicolas
Hauck, Judith
Iida, Yosuke
Ishii, Masao
Keppler, Lydia
Kim, Ji‐eun
Schlunegger, Sarah
Tjiputra, Jerry
Toyama, Katsuya
Vaittinada Ayar, Pradeebane
Velo, Antón
author_sort Rodgers, Keith, B
title Seasonal variability of the surface ocean carbon cycle: A synthesis
title_short Seasonal variability of the surface ocean carbon cycle: A synthesis
title_full Seasonal variability of the surface ocean carbon cycle: A synthesis
title_fullStr Seasonal variability of the surface ocean carbon cycle: A synthesis
title_full_unstemmed Seasonal variability of the surface ocean carbon cycle: A synthesis
title_sort seasonal variability of the surface ocean carbon cycle: a synthesis
publisher HAL CCSD
publishDate 2023
url https://hal.science/hal-04191390
https://hal.science/hal-04191390/document
https://hal.science/hal-04191390/file/Global%20Biogeochemical%20Cycles%20-%202023%20-%20Rodgers.pdf
https://doi.org/10.1029/2023gb007798
geographic Southern Ocean
geographic_facet Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_source ISSN: 0886-6236
EISSN: 1944-8224
Global Biogeochemical Cycles
https://hal.science/hal-04191390
Global Biogeochemical Cycles, In press, ⟨10.1029/2023gb007798⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2023gb007798
hal-04191390
https://hal.science/hal-04191390
https://hal.science/hal-04191390/document
https://hal.science/hal-04191390/file/Global%20Biogeochemical%20Cycles%20-%202023%20-%20Rodgers.pdf
doi:10.1029/2023gb007798
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/2023gb007798
container_title Global Biogeochemical Cycles
container_volume 37
container_issue 9
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spelling ftceafr:oai:HAL:hal-04191390v1 2023-10-09T21:56:01+02:00 Seasonal variability of the surface ocean carbon cycle: A synthesis Rodgers, Keith, B Schwinger, Jörg Fassbender, Andrea, J Landschützer, Peter Yamaguchi, Ryohei Frenzel, Hartmut Stein, Karl Müller, Jens, Daniel Goris, Nadine Sharma, Sahil Bushinsky, Seth Chau, Thi‐tuyet‐trang Gehlen, Marion Gallego, M. Angeles Gloege, Lucas Gregor, Luke Gruber, Nicolas Hauck, Judith Iida, Yosuke Ishii, Masao Keppler, Lydia Kim, Ji‐eun Schlunegger, Sarah Tjiputra, Jerry Toyama, Katsuya Vaittinada Ayar, Pradeebane Velo, Antón Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics (MERMAID) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) NORCE Norwegian Research Center Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR) 2023-08-23 https://hal.science/hal-04191390 https://hal.science/hal-04191390/document https://hal.science/hal-04191390/file/Global%20Biogeochemical%20Cycles%20-%202023%20-%20Rodgers.pdf https://doi.org/10.1029/2023gb007798 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2023gb007798 hal-04191390 https://hal.science/hal-04191390 https://hal.science/hal-04191390/document https://hal.science/hal-04191390/file/Global%20Biogeochemical%20Cycles%20-%202023%20-%20Rodgers.pdf doi:10.1029/2023gb007798 info:eu-repo/semantics/OpenAccess ISSN: 0886-6236 EISSN: 1944-8224 Global Biogeochemical Cycles https://hal.science/hal-04191390 Global Biogeochemical Cycles, In press, ⟨10.1029/2023gb007798⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2023 ftceafr https://doi.org/10.1029/2023gb007798 2023-09-20T16:27:59Z Abstract The seasonal cycle is the dominant mode of variability in the air‐sea CO 2 flux in most regions of the global ocean, yet discrepancies between different seasonality estimates are rather large. As part of the Regional Carbon Cycle Assessment and Processes phase 2 project (RECCAP2), we synthesize surface ocean p CO 2 and air‐sea CO 2 flux seasonality from models and observation‐based estimates, focusing on both a present‐day climatology and decadal changes between the 1980s and 2010s. Four main findings emerge: First, global ocean biogeochemistry models (GOBMs) and observation‐based estimates ( p CO 2 products) of surface p CO 2 seasonality disagree in amplitude and phase, primarily due to discrepancies in the seasonal variability in surface DIC. Second, the seasonal cycle in p CO 2 has increased in amplitude over the last three decades in both p CO 2 products and GOBMs. Third, decadal increases in p CO 2 seasonal cycle amplitudes in subtropical biomes for both p CO 2 products and GOBMs are driven by increasing DIC concentrations stemming from the uptake of anthropogenic CO 2 (C ant ). In subpolar and Southern Ocean biomes, however, the seasonality change for GOBMs is dominated by C ant invasion, whereas for p CO 2 products an indeterminate combination of C ant invasion and climate change modulates the changes. Fourth, biome‐aggregated decadal changes in the amplitude of p CO 2 seasonal variability are largely detectable against both mapping uncertainty (reducible) and natural variability uncertainty (irreducible), but not at the gridpoint scale over much of the northern subpolar oceans and over the Southern Ocean, underscoring the importance of sustained high‐quality seasonally‐resolved measurements over these regions. Article in Journal/Newspaper Southern Ocean HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) Southern Ocean Global Biogeochemical Cycles 37 9