Articles | Volume 13, issue 2
https://doi.org/10.5194/gmd-13-717-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-13-717-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Development and technical paper
| 
24 Feb 2020
Development and technical paper |
| 24 Feb 2020
| 24 Feb 2020
A comprehensive assessment of tropical stratospheric upwelling in the specified dynamics Community Earth System Model 1.2.2 – Whole Atmosphere Community Climate Model (CESM (WACCM))
Cooperative Institute for Research in Environmental Sciences (CIRES), Chemical Sciences Division, NOAA Earth System Research Laboratory (ESRL), University of Colorado, Boulder, CO, USA
now at: Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
Sean M. Davis
Chemical Sciences Division, NOAA Earth System Research Laboratory (ESRL), Boulder, CO, USA
Robert W. Portmann
Chemical Sciences Division, NOAA Earth System Research Laboratory (ESRL), Boulder, CO, USA
Cooperative Institute for Research in Environmental Sciences (CIRES), Chemical Sciences Division, NOAA Earth System Research Laboratory (ESRL), University of Colorado, Boulder, CO, USA
Karen H. Rosenlof
Chemical Sciences Division, NOAA Earth System Research Laboratory (ESRL), Boulder, CO, USA
Pengfei Yu
Cooperative Institute for Research in Environmental Sciences (CIRES), Chemical Sciences Division, NOAA Earth System Research Laboratory (ESRL), University of Colorado, Boulder, CO, USA
now at: Institute for Environmental and Climate Research, Jinan University, Guangzhou, GD, China
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Cited
14 citations as recorded by crossref.
- The role of tropical upwelling in explaining discrepancies between recent modeled and observed lower-stratospheric ozone trends S. Davis et al. 10.5194/acp-23-3347-2023
- Opinion: The scientific and community-building roles of the Geoengineering Model Intercomparison Project (GeoMIP) – past, present, and future D. Visioni et al. 10.5194/acp-23-5149-2023
- Robust Enhancement of Tropical Convective Activity by the 2019 Antarctic Sudden Stratospheric Warming S. Noguchi et al. 10.1029/2020GL088743
- Evaluating the Impact of Chemical Complexity and Horizontal Resolution on Tropospheric Ozone Over the Conterminous US With a Global Variable Resolution Chemistry Model R. Schwantes et al. 10.1029/2021MS002889
- Mechanisms Linked to Recent Ozone Decreases in the Northern Hemisphere Lower Stratosphere C. Orbe et al. 10.1029/2019JD031631
- 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
- A decline in global CFC-11 emissions during 2018−2019 S. Montzka et al. 10.1038/s41586-021-03260-5
- Very short-lived halogens amplify ozone depletion trends in the tropical lower stratosphere J. Villamayor et al. 10.1038/s41558-023-01671-y
- Perturbation of Tropical Stratospheric Ozone Through Homogeneous and Heterogeneous Chemistry Due To Pinatubo Y. Peng et al. 10.1029/2023GL103773
- Potential Stratospheric Ozone Depletion Due To Iodine Injection From Small Satellites W. Feng et al. 10.1029/2022GL102300
- Specified dynamics scheme impacts on wave-mean flow dynamics, convection, and tracer transport in CESM2 (WACCM6) N. Davis et al. 10.5194/acp-22-197-2022
- Numerical impacts on tracer transport: Diagnosing the influence of dynamical core formulation and resolution on stratospheric transport A. Gupta et al. 10.1175/JAS-D-21-0085.1
- Continental-scale contributions to the global CFC-11 emission increase between 2012 and 2017 L. Hu et al. 10.5194/acp-22-2891-2022
- The advective Brewer–Dobson circulation in the ERA5 reanalysis: climatology, variability, and trends M. Diallo et al. 10.5194/acp-21-7515-2021
14 citations as recorded by crossref.
- The role of tropical upwelling in explaining discrepancies between recent modeled and observed lower-stratospheric ozone trends S. Davis et al. 10.5194/acp-23-3347-2023
- Opinion: The scientific and community-building roles of the Geoengineering Model Intercomparison Project (GeoMIP) – past, present, and future D. Visioni et al. 10.5194/acp-23-5149-2023
- Robust Enhancement of Tropical Convective Activity by the 2019 Antarctic Sudden Stratospheric Warming S. Noguchi et al. 10.1029/2020GL088743
- Evaluating the Impact of Chemical Complexity and Horizontal Resolution on Tropospheric Ozone Over the Conterminous US With a Global Variable Resolution Chemistry Model R. Schwantes et al. 10.1029/2021MS002889
- Mechanisms Linked to Recent Ozone Decreases in the Northern Hemisphere Lower Stratosphere C. Orbe et al. 10.1029/2019JD031631
- 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
- A decline in global CFC-11 emissions during 2018−2019 S. Montzka et al. 10.1038/s41586-021-03260-5
- Very short-lived halogens amplify ozone depletion trends in the tropical lower stratosphere J. Villamayor et al. 10.1038/s41558-023-01671-y
- Perturbation of Tropical Stratospheric Ozone Through Homogeneous and Heterogeneous Chemistry Due To Pinatubo Y. Peng et al. 10.1029/2023GL103773
- Potential Stratospheric Ozone Depletion Due To Iodine Injection From Small Satellites W. Feng et al. 10.1029/2022GL102300
- Specified dynamics scheme impacts on wave-mean flow dynamics, convection, and tracer transport in CESM2 (WACCM6) N. Davis et al. 10.5194/acp-22-197-2022
- Numerical impacts on tracer transport: Diagnosing the influence of dynamical core formulation and resolution on stratospheric transport A. Gupta et al. 10.1175/JAS-D-21-0085.1
- Continental-scale contributions to the global CFC-11 emission increase between 2012 and 2017 L. Hu et al. 10.5194/acp-22-2891-2022
- The advective Brewer–Dobson circulation in the ERA5 reanalysis: climatology, variability, and trends M. Diallo et al. 10.5194/acp-21-7515-2021
Latest update: 18 Apr 2024
Short summary
Large-scale waves drive upward motion in the tropical stratosphere, with major impacts on stratospheric chemistry and climate. However, some of the modeling methods which attempt to simulate the past evolution of the stratosphere do not seem to be able to recreate important trends. We believe this is due to disagreements between the basic climate of the model and observations, but if the method is constructed more carefully, the disagreement becomes smaller and the trends become more realistic.
Large-scale waves drive upward motion in the tropical stratosphere, with major impacts on...
