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An upper-branch Brewer-Dobson circulation index for attribution of stratospheric variability and improved ozone and temperature trend analysis

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F16%3A10334379" target="_blank" >RIV/00216208:11320/16:10334379 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.5194/acp-16-15485-2016" target="_blank" >http://dx.doi.org/10.5194/acp-16-15485-2016</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.5194/acp-16-15485-2016" target="_blank" >10.5194/acp-16-15485-2016</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    An upper-branch Brewer-Dobson circulation index for attribution of stratospheric variability and improved ozone and temperature trend analysis

  • Original language description

    We find that wintertime temperature anomalies near 4 hPa and 50 degrees N/S are related, through dynamics, to anomalies in ozone and temperature, particularly in the tropical stratosphere but also throughout the upper stratosphere and mesosphere. These mid-latitude anomalies occur on timescales of up to a month, and are related to changes in wave forcing. A change in the meridional Brewer-Dobson circulation extends from the middle stratosphere into the mesosphere and forms a temperature-change quadrupole from Equator to pole. We develop a dynamical index based on detrended, deseasonalised mid-latitude temperature. When employed in multiple linear regression, this index can account for up to 60% of the total variability of temperature, peaking at similar to 5 hPa and dropping to 0 at similar to 50 and similar to 0.5 hPa, respectively, and increasing again into the mesosphere. Ozone similarly sees up to an additional 50% of variability accounted for, with a slightly higher maximum and strong altitude dependence, with zero improvement found at 10 hPa. Further, the uncertainty on all equatorial multiple-linear regression coefficients can be reduced by up to 35 and 20% in temperature and ozone, respectively, and so this index is an important tool for quantifying current and future ozone recovery.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DG - Atmospheric sciences, meteorology

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GC16-01562J" target="_blank" >GC16-01562J: Middle atmosphere effects of localized gravity wave forcing</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2016

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Atmospheric Chemistry and Physics

  • ISSN

    1680-7316

  • e-ISSN

  • Volume of the periodical

    16

  • Issue of the periodical within the volume

    24

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    16

  • Pages from-to

    15485-15500

  • UT code for WoS article

    000391486900004

  • EID of the result in the Scopus database

    2-s2.0-85003982882