Transient overturning changes cause an upper-ocean nutrient decline in a warming climate
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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1 Online-Ressource.
- Language
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Englisch
- Bibliographic citation
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Transient overturning changes cause an upper-ocean nutrient decline in a warming climate ; volume:15 ; number:1 ; day:4 ; month:9 ; year:2024 ; pages:1-9 ; date:12.2024
Nature Communications ; 15, Heft 1 (4.9.2024), 1-9, 12.2024
- Classification
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Medizin, Gesundheit
- Creator
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Sun, Shantong
Thompson, Andrew F.
Yu, Jimin
Wu, Lixin
- Contributor
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SpringerLink (Online service)
- DOI
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10.1038/s41467-024-52200-0
- URN
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urn:nbn:de:101:1-2411261258479.804504548142
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
-
15.08.2025, 7:36 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Sun, Shantong
- Thompson, Andrew F.
- Yu, Jimin
- Wu, Lixin
- SpringerLink (Online service)
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A 30-year reconstruction of the Atlantic meridional overturning circulation shows no decline
The evolution of the Atlantic meridional overturning circulation and its implications for surface warming
Model spread in tropical low cloud feedback tied to overturning circulation response to warming
Twenty-first century ocean warming, acidification, deoxygenation, and upper-ocean nutrient and primary production decline from CMIP6 model projections
Role of the Labrador Current in the Atlantic Meridional Overturning Circulation response to greenhouse warming
The role of Atlantic overturning circulation in the recent decline of Atlantic major hurricane frequency
Variations of the Atlantic meridional overturning circulation in control and transient simulations of the last millennium
Acidification, deoxygenation, and nutrient and biomass declines in a warming Mediterranean Sea
Acidification, deoxygenation, nutrient and biomasses decline in a warming Mediterranean Sea
Twenty-first century ocean warming, acidification, deoxygenation, and upper ocean nutrient decline from CMIP6 model projections
Observed decline of the Atlantic meridional overturning circulation 2004–2012
A 30-year reconstruction of the Atlantic meridional overturning circulation shows no decline
A 30-year reconstruction of the Atlantic meridional overturning circulation shows no decline
The evolution of the Atlantic meridional overturning circulation and its implications for surface warming
Model spread in tropical low cloud feedback tied to overturning circulation response to warming
Twenty-first century ocean warming, acidification, deoxygenation, and upper-ocean nutrient and primary production decline from CMIP6 model projections
Role of the Labrador Current in the Atlantic Meridional Overturning Circulation response to greenhouse warming
The role of Atlantic overturning circulation in the recent decline of Atlantic major hurricane frequency
Variations of the Atlantic meridional overturning circulation in control and transient simulations of the last millennium
Acidification, deoxygenation, and nutrient and biomass declines in a warming Mediterranean Sea
Acidification, deoxygenation, nutrient and biomasses decline in a warming Mediterranean Sea
Twenty-first century ocean warming, acidification, deoxygenation, and upper ocean nutrient decline from CMIP6 model projections
Observed decline of the Atlantic meridional overturning circulation 2004–2012
A 30-year reconstruction of the Atlantic meridional overturning circulation shows no decline
A 30-year reconstruction of the Atlantic meridional overturning circulation shows no decline
The evolution of the Atlantic meridional overturning circulation and its implications for surface warming
Model spread in tropical low cloud feedback tied to overturning circulation response to warming
Twenty-first century ocean warming, acidification, deoxygenation, and upper-ocean nutrient and primary production decline from CMIP6 model projections
Role of the Labrador Current in the Atlantic Meridional Overturning Circulation response to greenhouse warming
The role of Atlantic overturning circulation in the recent decline of Atlantic major hurricane frequency
Variations of the Atlantic meridional overturning circulation in control and transient simulations of the last millennium