Trends and variability in the ocean carbon sink ...

The ocean has absorbed 25 ± 2% of the total anthropogenic CO2 emissions from the early 1960s to the late 2010s, with rates more than tripling over this period and with a mean uptake of –2.7 ± 0.3 Pg C year–1 for the period 1990 through 2019. This growth of the ocean sink matches expectations based o...

Full description

Bibliographic Details
Main Authors: Gruber, Nicolas, Bakker, Dorothee C.E., DeVries, Tim, Gregor, Luke, Hauck, Judith, Landschützer, Peter, McKinley, Galen A., Müller, Jens Daniel
Format: Article in Journal/Newspaper
Language:English
Published: ETH Zurich 2023
Subjects:
Online Access:https://dx.doi.org/10.3929/ethz-b-000595538
http://hdl.handle.net/20.500.11850/595538
id ftdatacite:10.3929/ethz-b-000595538
record_format openpolar
spelling ftdatacite:10.3929/ethz-b-000595538 2024-04-28T08:39:35+00:00 Trends and variability in the ocean carbon sink ... Gruber, Nicolas Bakker, Dorothee C.E. DeVries, Tim Gregor, Luke Hauck, Judith Landschützer, Peter McKinley, Galen A. Müller, Jens Daniel 2023 application/pdf 38 p. accepted version https://dx.doi.org/10.3929/ethz-b-000595538 http://hdl.handle.net/20.500.11850/595538 en eng ETH Zurich Ocean carbon cycle Carbon budget Oceanography FOS Earth and related environmental sciences Climate infoeu-repo/classification/ddc/550 Earth sciences article-journal Text ScholarlyArticle Journal Article 2023 ftdatacite https://doi.org/10.3929/ethz-b-000595538 2024-04-02T12:32:08Z The ocean has absorbed 25 ± 2% of the total anthropogenic CO2 emissions from the early 1960s to the late 2010s, with rates more than tripling over this period and with a mean uptake of –2.7 ± 0.3 Pg C year–1 for the period 1990 through 2019. This growth of the ocean sink matches expectations based on the increase in atmospheric CO2, but research has shown that the sink is more variable than long assumed. In this Review, we discuss trends and variations in the ocean carbon sink. The sink stagnated during the 1990s with rates hovering around –2 Pg C year–1, but strengthened again after approximately 2000, taking up around –3 Pg C year–1 for 2010–2019. The most conspicuous changes in uptake occurred in the high latitudes, especially the Southern Ocean. These variations are caused by changes in weather and climate, but a volcanic eruption-induced reduction in the atmospheric CO2 growth rate and the associated global cooling contributed as well. Understanding the variability of the ocean carbon sink is crucial ... : Nature Reviews Earth & Environment, 4 ... Article in Journal/Newspaper Southern Ocean DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Ocean carbon cycle
Carbon budget
Oceanography
FOS Earth and related environmental sciences
Climate
infoeu-repo/classification/ddc/550
Earth sciences
spellingShingle Ocean carbon cycle
Carbon budget
Oceanography
FOS Earth and related environmental sciences
Climate
infoeu-repo/classification/ddc/550
Earth sciences
Gruber, Nicolas
Bakker, Dorothee C.E.
DeVries, Tim
Gregor, Luke
Hauck, Judith
Landschützer, Peter
McKinley, Galen A.
Müller, Jens Daniel
Trends and variability in the ocean carbon sink ...
topic_facet Ocean carbon cycle
Carbon budget
Oceanography
FOS Earth and related environmental sciences
Climate
infoeu-repo/classification/ddc/550
Earth sciences
description The ocean has absorbed 25 ± 2% of the total anthropogenic CO2 emissions from the early 1960s to the late 2010s, with rates more than tripling over this period and with a mean uptake of –2.7 ± 0.3 Pg C year–1 for the period 1990 through 2019. This growth of the ocean sink matches expectations based on the increase in atmospheric CO2, but research has shown that the sink is more variable than long assumed. In this Review, we discuss trends and variations in the ocean carbon sink. The sink stagnated during the 1990s with rates hovering around –2 Pg C year–1, but strengthened again after approximately 2000, taking up around –3 Pg C year–1 for 2010–2019. The most conspicuous changes in uptake occurred in the high latitudes, especially the Southern Ocean. These variations are caused by changes in weather and climate, but a volcanic eruption-induced reduction in the atmospheric CO2 growth rate and the associated global cooling contributed as well. Understanding the variability of the ocean carbon sink is crucial ... : Nature Reviews Earth & Environment, 4 ...
format Article in Journal/Newspaper
author Gruber, Nicolas
Bakker, Dorothee C.E.
DeVries, Tim
Gregor, Luke
Hauck, Judith
Landschützer, Peter
McKinley, Galen A.
Müller, Jens Daniel
author_facet Gruber, Nicolas
Bakker, Dorothee C.E.
DeVries, Tim
Gregor, Luke
Hauck, Judith
Landschützer, Peter
McKinley, Galen A.
Müller, Jens Daniel
author_sort Gruber, Nicolas
title Trends and variability in the ocean carbon sink ...
title_short Trends and variability in the ocean carbon sink ...
title_full Trends and variability in the ocean carbon sink ...
title_fullStr Trends and variability in the ocean carbon sink ...
title_full_unstemmed Trends and variability in the ocean carbon sink ...
title_sort trends and variability in the ocean carbon sink ...
publisher ETH Zurich
publishDate 2023
url https://dx.doi.org/10.3929/ethz-b-000595538
http://hdl.handle.net/20.500.11850/595538
genre Southern Ocean
genre_facet Southern Ocean
op_doi https://doi.org/10.3929/ethz-b-000595538
_version_ 1797570552655773696