Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › Research
Numerical simulation of the sensitivity of the mean meridional circulation in the middle atmosphere to the mountain waves during stratospheric warmings. / Koval, Andrey ; Gavrilov, Nikolai ; Pogoreltsev, Alexander .
EGU General Assembly 2019. 2019. 2743 (Geophysical Research Abstracts; Vol. 21).Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › Research
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TY - GEN
T1 - Numerical simulation of the sensitivity of the mean meridional circulation in the middle atmosphere to the mountain waves during stratospheric warmings
AU - Koval, Andrey
AU - Gavrilov, Nikolai
AU - Pogoreltsev, Alexander
N1 - Conference code: 21
PY - 2019
Y1 - 2019
N2 - Dynamical interactions between tropospheric and stratospheric layers have recently received increasing attention. These interactions intensify during stratospheric warming (SW) events. In this study, numerical simulations have been performed to estimate the transformation of the mean meridional circulation in altitude range 0 – 100 km at different phases of simulated SW events in January-February including and excluding impact of mesoscale orographic gravity waves (OGWs). To achieve statistical significance an ensemble of 12 pairs of model runs with and without a parameterization of OGW effects has been performed using the numerical middle and upper atmosphere model (MUAM).
AB - Dynamical interactions between tropospheric and stratospheric layers have recently received increasing attention. These interactions intensify during stratospheric warming (SW) events. In this study, numerical simulations have been performed to estimate the transformation of the mean meridional circulation in altitude range 0 – 100 km at different phases of simulated SW events in January-February including and excluding impact of mesoscale orographic gravity waves (OGWs). To achieve statistical significance an ensemble of 12 pairs of model runs with and without a parameterization of OGW effects has been performed using the numerical middle and upper atmosphere model (MUAM).
UR - https://meetingorganizer.copernicus.org/EGU2019/EGU2019-2743.pdf
M3 - Conference contribution
T3 - Geophysical Research Abstracts
BT - EGU General Assembly 2019
T2 - EGU General Assembly 2019
Y2 - 7 April 2019 through 12 April 2019
ER -
ID: 51042067