Alternate histories: synthetic large ensembles of sea-air CO 2 flux

International audience We use a statistical emulation technique to construct synthetic ensembles of global and regional sea-air carbon dioxide (CO 2 ) flux from four observation-based products over 1985-2014. Much like ensembles of Earth system models that are constructed by perturbing their initial...

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Published in:Global Biogeochemical Cycles
Main Authors: Olivarez, Holly C., Lovenduski, Nicole S., Brady, Riley X., Fay, Amanda R., Gehlen, Marion, Gregor, Luke, Landschützer, Peter, Mckinley, Galen A., Mckinnon, Karen A., Munro, David R.
Other Authors: University of Colorado Boulder, Department of Atmospheric and Oceanic Sciences and Institute of Arctic and Alpine Research, Columbia University New York, Lamont-Doherty Earth Observatory (LDEO), Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Institute of Biogeochemistry and Pollutant Dynamics ETH Zürich (IBP), Department of Environmental Systems Science ETH Zürich (D-USYS), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)-Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich), Max Planck Institute for Meteorology (MPI-M), Max-Planck-Gesellschaft, Department of Statistics Los Angeles, University of California Los Angeles (UCLA), University of California (UC)-University of California (UC), National Oceanic and Atmospheric Administration (NOAA)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2022
Subjects:
Online Access:https://insu.hal.science/insu-03721925
https://insu.hal.science/insu-03721925/document
https://insu.hal.science/insu-03721925/file/Global%20Biogeochemical%20Cycles%20-%202022%20-%20Olivarez%20-%20Alternate%20Histories%20Synthetic%20Large%20Ensembles%20of%20Sea%25E2%2580%2590Air%20CO2%20Flux.pdf
https://doi.org/10.1029/2021GB007174
id ftceafr:oai:HAL:insu-03721925v1
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 global carbon cycle
air-sea CO 2 flux
ocean carbon uptake
large ensemble
Earth system modeling
decadal trends
[SDU]Sciences of the Universe [physics]
spellingShingle global carbon cycle
air-sea CO 2 flux
ocean carbon uptake
large ensemble
Earth system modeling
decadal trends
[SDU]Sciences of the Universe [physics]
Olivarez, Holly C.
Lovenduski, Nicole S.
Brady, Riley X.
Fay, Amanda R.
Gehlen, Marion
Gregor, Luke
Landschützer, Peter
Mckinley, Galen A.
Mckinnon, Karen A.
Munro, David R.
Alternate histories: synthetic large ensembles of sea-air CO 2 flux
topic_facet global carbon cycle
air-sea CO 2 flux
ocean carbon uptake
large ensemble
Earth system modeling
decadal trends
[SDU]Sciences of the Universe [physics]
description International audience We use a statistical emulation technique to construct synthetic ensembles of global and regional sea-air carbon dioxide (CO 2 ) flux from four observation-based products over 1985-2014. Much like ensembles of Earth system models that are constructed by perturbing their initial conditions, our synthetic ensemble members exhibit different phasing of internal variability and a common externally forced signal. Our synthetic ensembles illustrate an important role for internal variability in the temporal evolution of global and regional CO 2 flux and produce a wide range of possible trends over 1990-1999 and 2000-2009. We assume a specific externally forced signal and calculate the rank of the observed trends within the distribution of statistically modeled synthetic trends during these periods. Over the decade 1990-1999, three of four observation-based products exhibit small negative trends in globally integrated sea-air CO 2 flux (i.e., enhanced ocean CO 2 absorption with time) that are within one standard deviation of the mean in their respective synthetic ensembles. Over the decade 2000-2009, however, three products show large negative trends in globally integrated sea-air CO 2 flux that have a low rate of occurrence in their synthetic ensembles. The largest positive trends in global and Southern Ocean flux over 1990-1999 and the largest negative trends over 2000-2009 fall nearly two standard deviations away from the mean in their ensembles. Our approach provides a new perspective on the important role of internal variability in sea-air CO 2 flux trends, and furthers understanding of the role of internal and external processes in driving observed sea-air CO 2 flux variability.
author2 University of Colorado Boulder
Department of Atmospheric and Oceanic Sciences and Institute of Arctic and Alpine Research
Columbia University New York
Lamont-Doherty Earth Observatory (LDEO)
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
Institute of Biogeochemistry and Pollutant Dynamics ETH Zürich (IBP)
Department of Environmental Systems Science ETH Zürich (D-USYS)
Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)-Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)
Max Planck Institute for Meteorology (MPI-M)
Max-Planck-Gesellschaft
Department of Statistics Los Angeles
University of California Los Angeles (UCLA)
University of California (UC)-University of California (UC)
National Oceanic and Atmospheric Administration (NOAA)
format Article in Journal/Newspaper
author Olivarez, Holly C.
Lovenduski, Nicole S.
Brady, Riley X.
Fay, Amanda R.
Gehlen, Marion
Gregor, Luke
Landschützer, Peter
Mckinley, Galen A.
Mckinnon, Karen A.
Munro, David R.
author_facet Olivarez, Holly C.
Lovenduski, Nicole S.
Brady, Riley X.
Fay, Amanda R.
Gehlen, Marion
Gregor, Luke
Landschützer, Peter
Mckinley, Galen A.
Mckinnon, Karen A.
Munro, David R.
author_sort Olivarez, Holly C.
title Alternate histories: synthetic large ensembles of sea-air CO 2 flux
title_short Alternate histories: synthetic large ensembles of sea-air CO 2 flux
title_full Alternate histories: synthetic large ensembles of sea-air CO 2 flux
title_fullStr Alternate histories: synthetic large ensembles of sea-air CO 2 flux
title_full_unstemmed Alternate histories: synthetic large ensembles of sea-air CO 2 flux
title_sort alternate histories: synthetic large ensembles of sea-air co 2 flux
publisher HAL CCSD
publishDate 2022
url https://insu.hal.science/insu-03721925
https://insu.hal.science/insu-03721925/document
https://insu.hal.science/insu-03721925/file/Global%20Biogeochemical%20Cycles%20-%202022%20-%20Olivarez%20-%20Alternate%20Histories%20Synthetic%20Large%20Ensembles%20of%20Sea%25E2%2580%2590Air%20CO2%20Flux.pdf
https://doi.org/10.1029/2021GB007174
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://insu.hal.science/insu-03721925
Global Biogeochemical Cycles, 2022, 36 (6), pp.e2021GB007174. ⟨10.1029/2021GB007174⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2021GB007174
insu-03721925
https://insu.hal.science/insu-03721925
https://insu.hal.science/insu-03721925/document
https://insu.hal.science/insu-03721925/file/Global%20Biogeochemical%20Cycles%20-%202022%20-%20Olivarez%20-%20Alternate%20Histories%20Synthetic%20Large%20Ensembles%20of%20Sea%25E2%2580%2590Air%20CO2%20Flux.pdf
BIBCODE: 2022GBioC.3607174O
doi:10.1029/2021GB007174
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/2021GB007174
container_title Global Biogeochemical Cycles
container_volume 36
container_issue 6
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spelling ftceafr:oai:HAL:insu-03721925v1 2024-06-09T07:49:45+00:00 Alternate histories: synthetic large ensembles of sea-air CO 2 flux Olivarez, Holly C. Lovenduski, Nicole S. Brady, Riley X. Fay, Amanda R. Gehlen, Marion Gregor, Luke Landschützer, Peter Mckinley, Galen A. Mckinnon, Karen A. Munro, David R. University of Colorado Boulder Department of Atmospheric and Oceanic Sciences and Institute of Arctic and Alpine Research Columbia University New York Lamont-Doherty Earth Observatory (LDEO) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Institute of Biogeochemistry and Pollutant Dynamics ETH Zürich (IBP) Department of Environmental Systems Science ETH Zürich (D-USYS) Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)-Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich) Max Planck Institute for Meteorology (MPI-M) Max-Planck-Gesellschaft Department of Statistics Los Angeles University of California Los Angeles (UCLA) University of California (UC)-University of California (UC) National Oceanic and Atmospheric Administration (NOAA) 2022 https://insu.hal.science/insu-03721925 https://insu.hal.science/insu-03721925/document https://insu.hal.science/insu-03721925/file/Global%20Biogeochemical%20Cycles%20-%202022%20-%20Olivarez%20-%20Alternate%20Histories%20Synthetic%20Large%20Ensembles%20of%20Sea%25E2%2580%2590Air%20CO2%20Flux.pdf https://doi.org/10.1029/2021GB007174 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2021GB007174 insu-03721925 https://insu.hal.science/insu-03721925 https://insu.hal.science/insu-03721925/document https://insu.hal.science/insu-03721925/file/Global%20Biogeochemical%20Cycles%20-%202022%20-%20Olivarez%20-%20Alternate%20Histories%20Synthetic%20Large%20Ensembles%20of%20Sea%25E2%2580%2590Air%20CO2%20Flux.pdf BIBCODE: 2022GBioC.3607174O doi:10.1029/2021GB007174 info:eu-repo/semantics/OpenAccess ISSN: 0886-6236 EISSN: 1944-8224 Global Biogeochemical Cycles https://insu.hal.science/insu-03721925 Global Biogeochemical Cycles, 2022, 36 (6), pp.e2021GB007174. ⟨10.1029/2021GB007174⟩ global carbon cycle air-sea CO 2 flux ocean carbon uptake large ensemble Earth system modeling decadal trends [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/article Journal articles 2022 ftceafr https://doi.org/10.1029/2021GB007174 2024-05-16T13:48:08Z International audience We use a statistical emulation technique to construct synthetic ensembles of global and regional sea-air carbon dioxide (CO 2 ) flux from four observation-based products over 1985-2014. Much like ensembles of Earth system models that are constructed by perturbing their initial conditions, our synthetic ensemble members exhibit different phasing of internal variability and a common externally forced signal. Our synthetic ensembles illustrate an important role for internal variability in the temporal evolution of global and regional CO 2 flux and produce a wide range of possible trends over 1990-1999 and 2000-2009. We assume a specific externally forced signal and calculate the rank of the observed trends within the distribution of statistically modeled synthetic trends during these periods. Over the decade 1990-1999, three of four observation-based products exhibit small negative trends in globally integrated sea-air CO 2 flux (i.e., enhanced ocean CO 2 absorption with time) that are within one standard deviation of the mean in their respective synthetic ensembles. Over the decade 2000-2009, however, three products show large negative trends in globally integrated sea-air CO 2 flux that have a low rate of occurrence in their synthetic ensembles. The largest positive trends in global and Southern Ocean flux over 1990-1999 and the largest negative trends over 2000-2009 fall nearly two standard deviations away from the mean in their ensembles. Our approach provides a new perspective on the important role of internal variability in sea-air CO 2 flux trends, and furthers understanding of the role of internal and external processes in driving observed sea-air CO 2 flux variability. Article in Journal/Newspaper Southern Ocean HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) Southern Ocean Global Biogeochemical Cycles 36 6