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1000 Titel
  • Effects of missing gravity waves on stratospheric dynamics; part 1: climatology
1000 Autor/in
  1. Eichinger, Roland |
  2. Garny, Hella |
  3. Šácha, Petr |
  4. Danker, Jessica |
  5. Dietmüller, Simone |
  6. Oberländer-Hayn, Sophie |
1000 Erscheinungsjahr 2020
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2020-02-15
1000 Erschienen in
1000 Quellenangabe
  • 54(5-6):3165-3183
1000 Copyrightjahr
  • 2020
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.1007/s00382-020-05166-w |
1000 Publikationsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • Energy and momentum deposition from planetary-scale Rossby waves as well as from small-scale gravity waves (GWs) largely control stratospheric dynamics. Interactions between these different wave types, however, complicate the quantification of their individual contribution to the overall dynamical state of the middle atmosphere. In state-of-the-art general circulation models (GCMs), the majority of the GW spectrum cannot be resolved and therefore has to be parameterised. This is commonly implemented in two discrete schemes, one for GWs that originate from flow over orographic obstacles and one for all other kinds of GWs (non-orographic GWs). In this study, we attempt to gain a deeper understanding of the interactions of resolved with parameterised wave driving and of their influence on the stratospheric zonal winds and on the Brewer–Dobson circulation (BDC). For this, we set up a GCM time slice experiment with two sensitivity simulations: one without orographic GWs and one without non-orographic GWs. Our findings include an acceleration of the polar vortices, which has historically been one of the main reasons for including explicit GW parameterisations in GCMs. Further, we find inter-hemispheric differences in BDC changes when omitting GWs that can be explained by wave compensation and amplification effects. These are partly evoked through local changes in the refractive properties of the atmosphere caused by the omitted GW drag and a thereby increased planetary wave propagation. However, non-local effects on the flow can act to suppress vertical wave fluxes into the stratosphere for a very strong polar vortex. Moreover, we study mean age of stratospheric air to investigate the impact of missing GWs on tracer transport. On the basis of this analysis, we suggest that the larger ratio of planetary waves to GWs leads to enhanced horizontal mixing, which can have a large impact on stratospheric tracer distributions.
1000 Sacherschließung
lokal Age of air
lokal Stratosphere
lokal Article
lokal Compensation
lokal Gravity waves
lokal Climate modelling
lokal Mixing
lokal Brewer–Dobson circulation
lokal Dynamics
lokal Polar vortex
lokal Transport
1000 Liste der Beteiligten
  1. https://frl.publisso.de/adhoc/uri/RWljaGluZ2VyLCBSb2xhbmQ=|https://frl.publisso.de/adhoc/uri/R2FybnksIEhlbGxh|https://frl.publisso.de/adhoc/uri/xaDDoWNoYSwgUGV0cg==|https://frl.publisso.de/adhoc/uri/RGFua2VyLCBKZXNzaWNh|https://frl.publisso.de/adhoc/uri/RGlldG3DvGxsZXIsIFNpbW9uZQ==|https://frl.publisso.de/adhoc/uri/T2JlcmzDpG5kZXItSGF5biwgU29waGll
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1000 Erstellt am 2023-11-17T03:24:36.441+0100
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1000 Zuletzt bearbeitet 2023-12-01T04:52:56.529+0100
1000 Objekt bearb. Fri Dec 01 04:52:56 CET 2023
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