Intensification of terrestrial carbon cycle related to El Niño–Southern Oscillation under greenhouse warming
- Standort
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Deutsche Nationalbibliothek Frankfurt am Main
- ISSN
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2041-1723
- Umfang
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Online-Ressource
- Sprache
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Englisch
- Anmerkungen
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online resource.
- Erschienen in
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Intensification of terrestrial carbon cycle related to El Niño–Southern Oscillation under greenhouse warming ; volume:8 ; number:1 ; day:22 ; month:11 ; year:2017 ; pages:1-8 ; date:12.2017
Nature Communications ; 8, Heft 1 (22.11.2017), 1-8, 12.2017
- Klassifikation
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Naturwissenschaften
- Urheber
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Kim, Jin-Soo
- Beteiligte Personen und Organisationen
-
Kug, Jong-Seong
Jeong, Su-Jong
SpringerLink (Online service)
- DOI
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10.1038/s41467-017-01831-7
- URN
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urn:nbn:de:1111-201804093254
- Rechteinformation
-
Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
-
14.08.2025, 10:56 MESZ
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Beteiligte
- Kim, Jin-Soo
- Kug, Jong-Seong
- Jeong, Su-Jong
- SpringerLink (Online service)
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Central-Pacific El Niño-Southern Oscillation less predictable under greenhouse warming
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The quasi-biennial oscillation in a warming climate
El Niño Southern Oscillation (ENSO) and global warming
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Decreased Indian Ocean Dipole variability under prolonged greenhouse warming
Middle Eocene greenhouse warming facilitated by diminished weathering feedback
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Major intensification of Atlantic overturning circulation at the onset of Paleogene greenhouse warmth
Major intensification of Atlantic overturning circulation at the onset of Paleogene greenhouse warmth
Author Correction: Intensification of terrestrial carbon cycle related to El Niño–Southern Oscillation under greenhouse warming
Central-Pacific El Niño-Southern Oscillation less predictable under greenhouse warming
Increased Indian Ocean-North Atlantic Ocean warming chain under greenhouse warming
The quasi-biennial oscillation in a warming climate
El Niño Southern Oscillation (ENSO) and global warming
Robust changes in global subtropical circulation under greenhouse warming
Decreased Indian Ocean Dipole variability under prolonged greenhouse warming
Middle Eocene greenhouse warming facilitated by diminished weathering feedback
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Midlatitude mesoscale thermal Air-sea interaction enhanced by greenhouse warming
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