Pregled bibliografske jedinice broj: 1105844
Gravity waves excited during a minor sudden stratospheric warming
Gravity waves excited during a minor sudden stratospheric warming // Atmospheric chemistry and physics, 18 (2018), 17; 12915-12931 doi:10.5194/acp-18-12915-2018 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 1105844 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Gravity waves excited during a minor sudden
stratospheric warming
Autori
Dörnbrack, Andreas ; Gisinger, Sonja ; Kaifler, Natalie ; Portele, Tanja Christina ; Bramberger, Martina ; Rapp, Markus ; Gerding, Michale ; Söder, Jens ; Žagar, Nedjeljka ; and Jelić, Damjan
Izvornik
Atmospheric chemistry and physics (1680-7316) 18
(2018), 17;
12915-12931
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Gravity waves
Sažetak
An exceptionally deep upper-air sounding launched from Kiruna airport (67.82∘ N, 20.33∘ E) on 30 January 2016 stimulated the current investigation of internal gravity waves excited during a minor sudden stratospheric warming (SSW) in the Arctic winter 2015/16. The analysis of the radiosonde profile revealed large kinetic and potential energies in the upper stratosphere without any simultaneous enhancement of upper tropospheric and lower stratospheric values. Upward- propagating inertia-gravity waves in the upper stratosphere and downward-propagating modes in the lower stratosphere indicated a region of gravity wave generation in the stratosphere. Two- dimensional wavelet analysis was applied to vertical time series of temperature fluctuations in order to determine the vertical propagation direction of the stratospheric gravity waves in 1-hourly high-resolution meteorological analyses and short-term forecasts. The separation of upward- and downward-propagating waves provided further evidence for a stratospheric source of gravity waves. The scale-dependent decomposition of the flow into a balanced component and inertia-gravity waves showed that coherent wave packets preferentially occurred at the inner edge of the Arctic polar vortex where a sub-vortex formed during the minor SSW.
Izvorni jezik
Engleski
Znanstvena područja
Geofizika
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus