Alkalinity responses to climate warming destabilise the Earth’s thermostat
The weathering alkalinity flux from mid-latitudes to the ocean will be strongly altered by climate warming by 2100. Under different emissions scenarios either a strengthening or a weakening of the flux and thus of the oceanic CO2 buffer is predicted.
| Main Authors: | , , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2023-03-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/s41467-023-37165-w |
| _version_ | 1797859923812417536 |
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| author | Nele Lehmann Tobias Stacke Sebastian Lehmann Hugues Lantuit John Gosse Chantal Mears Jens Hartmann Helmuth Thomas |
| author_facet | Nele Lehmann Tobias Stacke Sebastian Lehmann Hugues Lantuit John Gosse Chantal Mears Jens Hartmann Helmuth Thomas |
| author_sort | Nele Lehmann |
| collection | DOAJ |
| description | The weathering alkalinity flux from mid-latitudes to the ocean will be strongly altered by climate warming by 2100. Under different emissions scenarios either a strengthening or a weakening of the flux and thus of the oceanic CO2 buffer is predicted. |
| first_indexed | 2024-04-09T21:37:26Z |
| format | Article |
| id | doaj.art-f4456a7db2d0497389d8f4179c2d2503 |
| institution | Directory Open Access Journal |
| issn | 2041-1723 |
| language | English |
| last_indexed | 2024-04-09T21:37:26Z |
| publishDate | 2023-03-01 |
| publisher | Nature Portfolio |
| record_format | Article |
| series | Nature Communications |
| spelling | doaj.art-f4456a7db2d0497389d8f4179c2d25032023-03-26T11:14:00ZengNature PortfolioNature Communications2041-17232023-03-0114111210.1038/s41467-023-37165-wAlkalinity responses to climate warming destabilise the Earth’s thermostatNele Lehmann0Tobias Stacke1Sebastian LehmannHugues Lantuit2John Gosse3Chantal Mears4Jens Hartmann5Helmuth Thomas6Institute of Carbon Cycles, Helmholtz-Zentrum HereonInstitute of Carbon Cycles, Helmholtz-Zentrum HereonAlfred Wegener Institute Helmholtz Centre for Polar and Marine ResearchDepartment of Earth and Environmental Sciences, Dalhousie UniversityInstitute of Carbon Cycles, Helmholtz-Zentrum HereonInstitute for Geology, Center for Earth System Research and Sustainability (CEN), University HamburgInstitute of Carbon Cycles, Helmholtz-Zentrum HereonThe weathering alkalinity flux from mid-latitudes to the ocean will be strongly altered by climate warming by 2100. Under different emissions scenarios either a strengthening or a weakening of the flux and thus of the oceanic CO2 buffer is predicted.https://doi.org/10.1038/s41467-023-37165-w |
| spellingShingle | Nele Lehmann Tobias Stacke Sebastian Lehmann Hugues Lantuit John Gosse Chantal Mears Jens Hartmann Helmuth Thomas Alkalinity responses to climate warming destabilise the Earth’s thermostat Nature Communications |
| title | Alkalinity responses to climate warming destabilise the Earth’s thermostat |
| title_full | Alkalinity responses to climate warming destabilise the Earth’s thermostat |
| title_fullStr | Alkalinity responses to climate warming destabilise the Earth’s thermostat |
| title_full_unstemmed | Alkalinity responses to climate warming destabilise the Earth’s thermostat |
| title_short | Alkalinity responses to climate warming destabilise the Earth’s thermostat |
| title_sort | alkalinity responses to climate warming destabilise the earth s thermostat |
| url | https://doi.org/10.1038/s41467-023-37165-w |
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