Articles | Volume 18, issue 3
https://doi.org/10.5194/acp-18-1457-2018
© Author(s) 2018. 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-18-1457-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Assessing the ability to derive rates of polar middle-atmospheric descent using trace gas measurements from remote sensors
Niall J. Ryan
CORRESPONDING AUTHOR
Institute of Environmental Physics, University of Bremen, Bremen,
28359, Germany
Douglas E. Kinnison
Atmospheric Chemistry Observations and Modeling Laboratory, National
Center for Atmospheric Research, Boulder, Colorado, USA
Rolando R. Garcia
Atmospheric Chemistry Observations and Modeling Laboratory, National
Center for Atmospheric Research, Boulder, Colorado, USA
Christoph G. Hoffmann
Institute of Physics, University of Greifswald,
Felix-Hausdorff-Str. 6, 17489, Greifswald, Germany
Mathias Palm
Institute of Environmental Physics, University of Bremen, Bremen,
28359, Germany
Uwe Raffalski
Swedish Institute of Space Physics, Box 812, 981 28 Kiruna, Sweden
Justus Notholt
Institute of Environmental Physics, University of Bremen, Bremen,
28359, Germany
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16 citations as recorded by crossref.
- Winter 2018 major sudden stratospheric warming impact on midlatitude mesosphere from microwave radiometer measurements Y. Wang et al. 10.5194/acp-19-10303-2019
- New Global Meteoric Smoke Observations From SOFIE: Insight Regarding Chemical Composition, Meteoric Influx, and Hemispheric Asymmetry M. Hervig et al. 10.1029/2021JD035007
- Comparison of Major Sudden Stratospheric Warming Impacts on the Mid-Latitude Mesosphere Based on Local Microwave Radiometer CO Observations in 2018 and 2019 Y. Shi et al. 10.3390/rs12233950
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- Seasonal, interannual and long-term changes in the middle atmospheric carbon monoxide in the tropics O. Nath et al. 10.1016/j.atmosenv.2023.119958
- Observations and Modeling of Increased Nitric Oxide in the Antarctic Polar Middle Atmosphere Associated With Geomagnetic Storm‐Driven Energetic Electron Precipitation D. Newnham et al. 10.1029/2018JA025507
- The data processing and analysis methods for stratospheric ozone and planetary wave study Y. Shi et al. 10.33275/1727-7485.2.2022.698
- Effects of a Short-Term Increase in the Intensity of 630.0-nm Emissions of Atomic Oxygen [OI] at Lower Thermospheric Altitudes due to Anthropogenic Activity A. Mikhalev et al. 10.1134/S0016793220010107
- Evaluation of CESM1 (WACCM) free-running and specified dynamics atmospheric composition simulations using global multispecies satellite data records L. Froidevaux et al. 10.5194/acp-19-4783-2019
- Transport of Nitric Oxide Via Lagrangian Coherent Structures Into the Top of the Polar Vortex V. Harvey et al. 10.1029/2020JD034523
- Solar cycle variations in mesospheric carbon monoxide J. Lee et al. 10.1016/j.jastp.2018.02.001
- Mesospheric Water Vapor From SABER as a Tracer for the Residual Mean Circulation During SSW Events J. Zhang et al. 10.1029/2023JD039526
- Ozone and water vapor variability in the polar middle atmosphere observed with ground-based microwave radiometers G. Shi et al. 10.5194/acp-23-9137-2023
- Ground-based millimetre-wave measurements of middle-atmospheric carbon monoxide above Ny-Ålesund (78.9° N, 11.9° E) N. Ryan et al. 10.5194/amt-12-4077-2019
- Connections Between Stratospheric Ozone Concentrations Over the Arctic and Sea Surface Temperatures in the North Pacific M. Liu et al. 10.1029/2019JD031690
- Investigation of Arctic middle-atmospheric dynamics using 3 years of H<sub>2</sub>O and O<sub>3</sub> measurements from microwave radiometers at Ny-Ålesund F. Schranz et al. 10.5194/acp-19-9927-2019
Latest update: 14 Dec 2024
Short summary
We used model output and instrument data to assess how well polar atmospheric descent rates can be derived using concentration measurements of long-lived gases in the atmosphere. The results indicate that the method incurs errors as large as the descent rates, and often leads to a misinterpretation of the direction of air motion. The rates derived using this method do not appear to represent the mean vertical wind in the middle atmosphere, and we suggest an alternate definition.
We used model output and instrument data to assess how well polar atmospheric descent rates can...
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