Articles | Volume 17, issue 13
https://doi.org/10.5194/acp-17-8031-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-17-8031-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
04 Jul 2017
Research article |
| 04 Jul 2017
Contribution of different processes to changes in tropical lower-stratospheric water vapor in chemistry–climate models
Department of Atmospheric Sciences,
Texas A&M, College Station, Texas, USA
Andrew E. Dessler
Department of Atmospheric Sciences,
Texas A&M, College Station, Texas, USA
Slimane Bekki
LATMOS, Institut Pierre Simon Laplace (IPSL), Paris, France
Makoto Deushi
Meteorological Research Institute, 1-1 Nagamine, Tsukuba, Ibaraki 305-0052, Japan
Marion Marchand
LATMOS, Institut Pierre Simon Laplace (IPSL), Paris, France
Olaf Morgenstern
National Institute of Water and Atmospheric Research (NIWA), Wellington, New Zealand
David A. Plummer
Canadian Centre for Climate Modelling and Analysis, Environment and Climate Change Canada, Montreal, Canada
Kiyotaka Shibata
School of Environmental Science and Engineering, Kochi University of Technology, Kami, Japan
Yousuke Yamashita
National Institute for Environmental Studies (NIES), Tsukuba, Japan
now at: Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama, Japan
Guang Zeng
National Institute of Water and Atmospheric Research (NIWA), Wellington, New Zealand
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Cited
20 citations as recorded by crossref.
- The Impact of Continuing CFC‐11 Emissions on Stratospheric Ozone E. Fleming et al. 10.1029/2019JD031849
- The Surface Warming Attributable to Stratospheric Water Vapor in CO2‐Caused Global Warming Y. Wang & Y. Huang 10.1029/2020JD032752
- Interpol-IAGOS: a new method for assessing long-term chemistry–climate simulations in the UTLS based on IAGOS data, and its application to the MOCAGE CCMI REF-C1SD simulation Y. Cohen et al. 10.5194/gmd-14-2659-2021
- Stratospheric radiative feedback limited by the tropospheric influence in global warming Y. Wang & Y. Huang 10.1007/s00382-020-05390-4
- The response of stratospheric water vapor to climate change driven by different forcing agents X. Wang & A. Dessler 10.5194/acp-20-13267-2020
- Inconsistencies between chemistry–climate models and observed lower stratospheric ozone trends since 1998 W. Ball et al. 10.5194/acp-20-9737-2020
- Water vapor and lapse rate feedbacks in the climate system R. Colman & B. Soden 10.1103/RevModPhys.93.045002
- Elliptical Structures of Gravity Waves Produced by Typhoon Soudelor in 2015 near Taiwan F. Chane Ming et al. 10.3390/atmos10050260
- Stratospheric Water Vapor Feedback Disclosed by a Locking Experiment Y. Huang et al. 10.1029/2020GL087987
- Robust Acceleration of Stratospheric Moistening and Its Radiative Feedback Under Greenhouse Warming Y. Xia et al. 10.1029/2020JD033090
- Modeling the TTL at Continental Scale for a Wet Season: An Evaluation of the BRAMS Mesoscale Model Using TRO‐Pico Campaign, and Measurements From Airborne and Spaceborne Sensors A. Behera et al. 10.1002/2017JD027969
- 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
- Multi-decadal variability controls short-term stratospheric water vapor trends M. Tao et al. 10.1038/s43247-023-01094-9
- Seasonal effects of atmospheric waves over tropical tropopause using radiosonde observations at Hyderabad, India S. Mohammad et al. 10.1007/s00703-022-00918-1
- Evaluating stratospheric ozone and water vapour changes in CMIP6 models from 1850 to 2100 J. Keeble et al. 10.5194/acp-21-5015-2021
- Effects of convective ice evaporation on interannual variability of tropical tropopause layer water vapor H. Ye et al. 10.5194/acp-18-4425-2018
- Stratospheric water vapor: an important climate feedback A. Banerjee et al. 10.1007/s00382-019-04721-4
- Significant Contribution of Stratospheric Water Vapor to the Poleward Expansion of the Hadley Circulation in Autumn Under Greenhouse Warming Y. Xia et al. 10.1029/2021GL094008
- Linking uncertainty in simulated Arctic ozone loss to uncertainties in modelled tropical stratospheric water vapour L. Thölix et al. 10.5194/acp-18-15047-2018
- Response of stratospheric water vapour to warming constrained by satellite observations P. Nowack et al. 10.1038/s41561-023-01183-6
20 citations as recorded by crossref.
- The Impact of Continuing CFC‐11 Emissions on Stratospheric Ozone E. Fleming et al. 10.1029/2019JD031849
- The Surface Warming Attributable to Stratospheric Water Vapor in CO2‐Caused Global Warming Y. Wang & Y. Huang 10.1029/2020JD032752
- Interpol-IAGOS: a new method for assessing long-term chemistry–climate simulations in the UTLS based on IAGOS data, and its application to the MOCAGE CCMI REF-C1SD simulation Y. Cohen et al. 10.5194/gmd-14-2659-2021
- Stratospheric radiative feedback limited by the tropospheric influence in global warming Y. Wang & Y. Huang 10.1007/s00382-020-05390-4
- The response of stratospheric water vapor to climate change driven by different forcing agents X. Wang & A. Dessler 10.5194/acp-20-13267-2020
- Inconsistencies between chemistry–climate models and observed lower stratospheric ozone trends since 1998 W. Ball et al. 10.5194/acp-20-9737-2020
- Water vapor and lapse rate feedbacks in the climate system R. Colman & B. Soden 10.1103/RevModPhys.93.045002
- Elliptical Structures of Gravity Waves Produced by Typhoon Soudelor in 2015 near Taiwan F. Chane Ming et al. 10.3390/atmos10050260
- Stratospheric Water Vapor Feedback Disclosed by a Locking Experiment Y. Huang et al. 10.1029/2020GL087987
- Robust Acceleration of Stratospheric Moistening and Its Radiative Feedback Under Greenhouse Warming Y. Xia et al. 10.1029/2020JD033090
- Modeling the TTL at Continental Scale for a Wet Season: An Evaluation of the BRAMS Mesoscale Model Using TRO‐Pico Campaign, and Measurements From Airborne and Spaceborne Sensors A. Behera et al. 10.1002/2017JD027969
- 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
- Multi-decadal variability controls short-term stratospheric water vapor trends M. Tao et al. 10.1038/s43247-023-01094-9
- Seasonal effects of atmospheric waves over tropical tropopause using radiosonde observations at Hyderabad, India S. Mohammad et al. 10.1007/s00703-022-00918-1
- Evaluating stratospheric ozone and water vapour changes in CMIP6 models from 1850 to 2100 J. Keeble et al. 10.5194/acp-21-5015-2021
- Effects of convective ice evaporation on interannual variability of tropical tropopause layer water vapor H. Ye et al. 10.5194/acp-18-4425-2018
- Stratospheric water vapor: an important climate feedback A. Banerjee et al. 10.1007/s00382-019-04721-4
- Significant Contribution of Stratospheric Water Vapor to the Poleward Expansion of the Hadley Circulation in Autumn Under Greenhouse Warming Y. Xia et al. 10.1029/2021GL094008
- Linking uncertainty in simulated Arctic ozone loss to uncertainties in modelled tropical stratospheric water vapour L. Thölix et al. 10.5194/acp-18-15047-2018
- Response of stratospheric water vapour to warming constrained by satellite observations P. Nowack et al. 10.1038/s41561-023-01183-6
Discussed (preprint)
Latest update: 25 Apr 2024
Short summary
This paper explains a new way to evaluate simulated lower-stratospheric water vapor. We use a multivariate linear regression to predict 21st century lower stratospheric water vapor within 12 chemistry climate models using tropospheric warming, the Brewer–Dobson circulation, and the quasi-biennial oscillation as predictors. This methodology produce strong fits to simulated water vapor, and potentially represents a superior method to evaluate model trends in lower-stratospheric water vapor.
This paper explains a new way to evaluate simulated lower-stratospheric water vapor. We use a...
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