The impact of structural changes in the middle atmosphere on the Brewer-Dobson circulation Article Swipe
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· 2023
· Open Access
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· DOI: https://doi.org/10.5194/egusphere-egu23-4513
Changes in atmospheric composition affect surface climate and alter atmospheric structure, dynamics, and transport, which in turn further affect the composition. In the middle atmosphere, the composition is influenced by the Brewer-Dobson circulation (BDC), a global-scale interhemispheric meridional overturning circulation. Namely, the BDC controls the distribution and trends of radiatively important gases like ozone and water vapour. Another robust aspect of the changes in greenhouse gas concentrations is the changing structure of the atmosphere across layers. The troposphere is thermally expanding, the stratosphere is cooling and contracting and this is then reflected in the mesosphere and above as a downward shift of the height of pressure levels. Particularly, the tropospheric expansion and the stratospheric contraction has been shown to interfere with diagnosed BDC trends. We developed an analytical methodology that allows us to partition between the pure acceleration of the circulation and other kinematic factors (vertical shift, widening) contributing to the net advective mass flux changes and quantify their roles precisely. We apply this methodology to different datasets (ERA5, CMIP6, CCMI-1) to analyze the variability and trends of advective transport between different layers of the middle atmosphere. Finally, we discuss how the net advective transport and the individual kinematic mechanisms contributing to it respond to external forcings.
Related Topics
- Type
- preprint
- Language
- en
- Landing Page
- https://doi.org/10.5194/egusphere-egu23-4513
- OA Status
- gold
- Related Works
- 10
- OpenAlex ID
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Raw OpenAlex JSON
- OpenAlex ID
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https://openalex.org/W4321489689Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.5194/egusphere-egu23-4513Digital Object Identifier
- Title
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The impact of structural changes in the middle atmosphere on the Brewer-Dobson circulationWork title
- Type
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preprintOpenAlex work type
- Language
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enPrimary language
- Publication year
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2023Year of publication
- Publication date
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2023-02-22Full publication date if available
- Authors
-
Radek Zajíček, Petr Šácha, Petr Pišoft, Roland Eichinger, Harald E. Rieder, Aleš KuchařList of authors in order
- Landing page
-
https://doi.org/10.5194/egusphere-egu23-4513Publisher landing page
- Open access
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YesWhether a free full text is available
- OA status
-
goldOpen access status per OpenAlex
- OA URL
-
https://doi.org/10.5194/egusphere-egu23-4513Direct OA link when available
- Concepts
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Troposphere, Stratosphere, Advection, Atmosphere (unit), Atmospheric sciences, Environmental science, Atmospheric circulation, Climatology, Greenhouse gas, Zonal and meridional, Climate change, Geology, Meteorology, Geography, Physics, Oceanography, ThermodynamicsTop concepts (fields/topics) attached by OpenAlex
- Cited by
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0Total citation count in OpenAlex
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10Other works algorithmically related by OpenAlex
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| abstract_inverted_index.roles | 159 |
| abstract_inverted_index.shift | 100 |
| abstract_inverted_index.shown | 117 |
| abstract_inverted_index.their | 158 |
| abstract_inverted_index.water | 55 |
| abstract_inverted_index.which | 14 |
| abstract_inverted_index.(BDC), | 33 |
| abstract_inverted_index.(ERA5, | 168 |
| abstract_inverted_index.CMIP6, | 169 |
| abstract_inverted_index.across | 74 |
| abstract_inverted_index.affect | 4, 18 |
| abstract_inverted_index.allows | 130 |
| abstract_inverted_index.aspect | 59 |
| abstract_inverted_index.height | 103 |
| abstract_inverted_index.layers | 182 |
| abstract_inverted_index.middle | 23, 185 |
| abstract_inverted_index.robust | 58 |
| abstract_inverted_index.shift, | 146 |
| abstract_inverted_index.trends | 47, 176 |
| abstract_inverted_index.Another | 57 |
| abstract_inverted_index.CCMI-1) | 170 |
| abstract_inverted_index.Changes | 0 |
| abstract_inverted_index.Namely, | 40 |
| abstract_inverted_index.analyze | 172 |
| abstract_inverted_index.between | 134, 180 |
| abstract_inverted_index.changes | 62, 155 |
| abstract_inverted_index.climate | 6 |
| abstract_inverted_index.cooling | 84 |
| abstract_inverted_index.discuss | 189 |
| abstract_inverted_index.factors | 144 |
| abstract_inverted_index.further | 17 |
| abstract_inverted_index.layers. | 75 |
| abstract_inverted_index.levels. | 106 |
| abstract_inverted_index.respond | 203 |
| abstract_inverted_index.surface | 5 |
| abstract_inverted_index.trends. | 123 |
| abstract_inverted_index.vapour. | 56 |
| abstract_inverted_index.Finally, | 187 |
| abstract_inverted_index.changing | 69 |
| abstract_inverted_index.controls | 43 |
| abstract_inverted_index.datasets | 167 |
| abstract_inverted_index.downward | 99 |
| abstract_inverted_index.external | 205 |
| abstract_inverted_index.pressure | 105 |
| abstract_inverted_index.quantify | 157 |
| abstract_inverted_index.(vertical | 145 |
| abstract_inverted_index.advective | 152, 178, 193 |
| abstract_inverted_index.developed | 125 |
| abstract_inverted_index.diagnosed | 121 |
| abstract_inverted_index.different | 166, 181 |
| abstract_inverted_index.dynamics, | 11 |
| abstract_inverted_index.expansion | 110 |
| abstract_inverted_index.forcings. | 206 |
| abstract_inverted_index.important | 50 |
| abstract_inverted_index.interfere | 119 |
| abstract_inverted_index.kinematic | 143, 198 |
| abstract_inverted_index.partition | 133 |
| abstract_inverted_index.reflected | 91 |
| abstract_inverted_index.structure | 70 |
| abstract_inverted_index.thermally | 79 |
| abstract_inverted_index.transport | 179, 194 |
| abstract_inverted_index.widening) | 147 |
| abstract_inverted_index.analytical | 127 |
| abstract_inverted_index.atmosphere | 73 |
| abstract_inverted_index.expanding, | 80 |
| abstract_inverted_index.greenhouse | 64 |
| abstract_inverted_index.individual | 197 |
| abstract_inverted_index.influenced | 28 |
| abstract_inverted_index.mechanisms | 199 |
| abstract_inverted_index.meridional | 37 |
| abstract_inverted_index.mesosphere | 94 |
| abstract_inverted_index.precisely. | 160 |
| abstract_inverted_index.structure, | 10 |
| abstract_inverted_index.transport, | 13 |
| abstract_inverted_index.atmosphere, | 24 |
| abstract_inverted_index.atmosphere. | 186 |
| abstract_inverted_index.atmospheric | 2, 9 |
| abstract_inverted_index.circulation | 32, 140 |
| abstract_inverted_index.composition | 3, 26 |
| abstract_inverted_index.contracting | 86 |
| abstract_inverted_index.contraction | 114 |
| abstract_inverted_index.methodology | 128, 164 |
| abstract_inverted_index.overturning | 38 |
| abstract_inverted_index.radiatively | 49 |
| abstract_inverted_index.troposphere | 77 |
| abstract_inverted_index.variability | 174 |
| abstract_inverted_index.acceleration | 137 |
| abstract_inverted_index.circulation. | 39 |
| abstract_inverted_index.composition. | 20 |
| abstract_inverted_index.contributing | 148, 200 |
| abstract_inverted_index.distribution | 45 |
| abstract_inverted_index.global-scale | 35 |
| abstract_inverted_index.stratosphere | 82 |
| abstract_inverted_index.tropospheric | 109 |
| abstract_inverted_index.Brewer-Dobson | 31 |
| abstract_inverted_index.Particularly, | 107 |
| abstract_inverted_index.stratospheric | 113 |
| abstract_inverted_index.concentrations | 66 |
| abstract_inverted_index.interhemispheric | 36 |
| cited_by_percentile_year | |
| corresponding_author_ids | https://openalex.org/A5072552360, https://openalex.org/A5067727328 |
| countries_distinct_count | 3 |
| institutions_distinct_count | 6 |
| corresponding_institution_ids | https://openalex.org/I21250087, https://openalex.org/I926574661 |
| sustainable_development_goals[0].id | https://metadata.un.org/sdg/13 |
| sustainable_development_goals[0].score | 0.550000011920929 |
| sustainable_development_goals[0].display_name | Climate action |
| citation_normalized_percentile.value | 0.02419313 |
| citation_normalized_percentile.is_in_top_1_percent | False |
| citation_normalized_percentile.is_in_top_10_percent | False |