Articles | Volume 21, issue 5
https://doi.org/10.5194/acp-21-3725-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-21-3725-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
11 Mar 2021
Research article |
| 11 Mar 2021
| 11 Mar 2021
Influence of the El Niño–Southern Oscillation on entry stratospheric water vapor in coupled chemistry–ocean CCMI and CMIP6 models
Chaim I. Garfinkel
CORRESPONDING AUTHOR
The Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University of Jerusalem, Jerusalem, Israel
Ohad Harari
The Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University of Jerusalem, Jerusalem, Israel
Shlomi Ziskin Ziv
The Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University of Jerusalem, Jerusalem, Israel
Department of Physics, Ariel University, Ariel, Israel
Eastern R&D center, Ariel, Israel
The Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University of Jerusalem, Jerusalem, Israel
Key Laboratory of Meteorological Disaster of China Ministry of Education (KLME), Joint International Research Laboratory of Climate and Environment Change (ILCEC), Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science & Technology, Nanjing 210044, China
Olaf Morgenstern
National Institute of Water and Atmospheric Research, Wellington, New Zealand
Guang Zeng
National Institute of Water and Atmospheric Research, Wellington, New Zealand
Simone Tilmes
National Center for Atmospheric Research, Boulder, Colorado, USA
Douglas Kinnison
National Center for Atmospheric Research, Boulder, Colorado, USA
Fiona M. O'Connor
Met Office Hadley Centre, Exeter, UK
Neal Butchart
Met Office Hadley Centre, Exeter, UK
Makoto Deushi
Meteorological Research Institute, Tsukuba, Japan
Patrick Jöckel
Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany
Andrea Pozzer
Atmospheric Chemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany
International Centre for Theoretical Physics, Trieste, Italy
Sean Davis
NOAA Chemical Sciences Laboratory, Boulder, CO, USA
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Cited
12 citations as recorded by crossref.
- Contrasting Effects of Indian Ocean Basin and Dipole Modes on the Stratosphere R. Huang et al. 10.1029/2021JD035156
- Role of Stratospheric Processes in Climate Change: Advances and Challenges W. Tian et al. 10.1007/s00376-023-2341-1
- Response of stratospheric water vapour to warming constrained by satellite observations P. Nowack et al. 10.1038/s41561-023-01183-6
- 大气水汽稳定同位素: 特征、机制与前景 白. 尚 et al. 10.1360/N072023-0271
- The Influence of Internal Climate Variability on Stratospheric Water Vapor Increases After Large‐Magnitude Explosive Tropical Volcanic Eruptions X. Zhou et al. 10.1029/2023GL103076
- The roles of the Quasi-Biennial Oscillation and El Niño for entry stratospheric water vapor in observations and coupled chemistry–ocean CCMI and CMIP6 models S. Ziskin Ziv et al. 10.5194/acp-22-7523-2022
- Stable isotopes in atmospheric water vapour: Patterns, mechanisms and perspectives B. Shang et al. 10.1007/s11430-023-1410-6
- Secular changes in the tropical stratospheric water vapour entry induced by the Indo-Pacific warm pool warming Y. Jiang et al. 10.1016/j.atmosres.2024.107381
- Significant Stratospheric Moistening Following Extreme El Niño Events Q. Chen et al. 10.3390/rs15133346
- A revisit and comparison of the quasi-biennial oscillation (QBO) disruption events in 2015/16 and 2019/20 Y. Wang et al. 10.1016/j.atmosres.2023.106970
- Interannual Variability of Zonal Mean Temperature, Water Vapor, and Clouds in the Tropical Tropopause Layer A. Sweeney & Q. Fu 10.1029/2023JD039002
- Variability of Water Vapor in the Tropical Middle Atmosphere Observed From Satellites and Interpreted Using SD‐WACCM Simulations W. Yu et al. 10.1029/2022JD036714
11 citations as recorded by crossref.
- Contrasting Effects of Indian Ocean Basin and Dipole Modes on the Stratosphere R. Huang et al. 10.1029/2021JD035156
- Role of Stratospheric Processes in Climate Change: Advances and Challenges W. Tian et al. 10.1007/s00376-023-2341-1
- Response of stratospheric water vapour to warming constrained by satellite observations P. Nowack et al. 10.1038/s41561-023-01183-6
- 大气水汽稳定同位素: 特征、机制与前景 白. 尚 et al. 10.1360/N072023-0271
- The Influence of Internal Climate Variability on Stratospheric Water Vapor Increases After Large‐Magnitude Explosive Tropical Volcanic Eruptions X. Zhou et al. 10.1029/2023GL103076
- The roles of the Quasi-Biennial Oscillation and El Niño for entry stratospheric water vapor in observations and coupled chemistry–ocean CCMI and CMIP6 models S. Ziskin Ziv et al. 10.5194/acp-22-7523-2022
- Stable isotopes in atmospheric water vapour: Patterns, mechanisms and perspectives B. Shang et al. 10.1007/s11430-023-1410-6
- Secular changes in the tropical stratospheric water vapour entry induced by the Indo-Pacific warm pool warming Y. Jiang et al. 10.1016/j.atmosres.2024.107381
- Significant Stratospheric Moistening Following Extreme El Niño Events Q. Chen et al. 10.3390/rs15133346
- A revisit and comparison of the quasi-biennial oscillation (QBO) disruption events in 2015/16 and 2019/20 Y. Wang et al. 10.1016/j.atmosres.2023.106970
- Interannual Variability of Zonal Mean Temperature, Water Vapor, and Clouds in the Tropical Tropopause Layer A. Sweeney & Q. Fu 10.1029/2023JD039002
Latest update: 30 May 2025
Short summary
Water vapor is the dominant greenhouse gas in the atmosphere, and El Niño is the dominant mode of variability in the ocean–atmosphere system. The connection between El Niño and water vapor above ~ 17 km is unclear, with single-model studies reaching a range of conclusions. This study examines this connection in 12 different models. While there are substantial differences among the models, all models appear to capture the fundamental physical processes correctly.
Water vapor is the dominant greenhouse gas in the atmosphere, and El Niño is the dominant mode...
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