Repozitorij Univerze v Novi Gorici

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Naslov:Orographic gravity waves in OH-airglow imaging systems
Avtorji:ID Wuest, Sabine, Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen (DLR-DFD), Germany (Avtor)
ID Till, Jonas, Institut für Physik, Universität Augsburg, 86159 Augsburg, Germany (Avtor)
ID Sedlak, René, Institut für Physik, Universität Augsburg, 86159 Augsburg, Germany (Avtor)
ID Hannawald, Patrick, Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen (DLR-DFD), Germany (Avtor)
ID Schmidt, Carsten, Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen (DLR-DFD), Germany (Avtor)
ID Stanič, Samo, Center for Astrophysics and Cosmology, University of Nova Gorica, 5270 Ajdovščina, Slovenia (Avtor)
ID Bittner, Michael, Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen (DLR-DFD), Germany (Avtor)
Datoteke: Gradivo nima datotek, ki so prostodostopne za javnost. Gradivo je morda fizično dosegljivo v knjižnici fakultete, zalogo lahko preverite v COBISS-u. Povezava se odpre v novem oknu
Jezik:Angleški jezik
Vrsta gradiva:Delo ni kategorizirano
Tipologija:1.12 - Objavljeni povzetek znanstvenega prispevka na konferenci
Organizacija:UNG - Univerza v Novi Gorici
Opis:Atmospheric dynamics is strongly influenced by waves on different scales. Airflow over mountains can lead to all kinds of atmospheric waves, planetary and gravity waves as well as infrasound. Under certain circumstances these waves can propagate through the atmosphere and lead to a re- distribution of energy. In the case of gravity waves, a stably stratified atmosphere is a mandatory requirement for their generation and vertical propagation. Additionally, the vertical propagation depends on the horizontal wind field. In the Alpine and pre-Alpine region, we currently operate five OH-airglow imaging systems, which allow the investigation of orographic gravity waves. Depending on tropo-, strato- and mesospheric wind and temperature, it is checked which wavelengths can propagate into the fields of view of our instruments. This is done for a whole year in order to take into account annual and semi- annual cycles in wind and temperature. Concerning the generation of gravity waves, we put our focus on our OH-airglow imager (FAIM) deployed at Otlica (45.9°N, 13.9°E), Slovenia. Here, we also have additional measurements of an OH-airglow spectrometer (GRIPS). In case studies, we investigate whether strong wind events (Bora) lead to strong gravity waves activity or enhanced potential energy density.
Ključne besede:Orographic gravity waves, Bora, Otlica, Slovenia, OH-airglow imaging
Status publikacije:Objavljeno
Leto izida:2020
Št. strani:1
PID:20.500.12556/RUNG-5883 Novo okno
COBISS.SI-ID:31741955 Novo okno
DOI:https://doi.org/10.5194/egusphere-egu2020-2878 Novo okno
NUK URN:URN:SI:UNG:REP:UJMSS2FC
Datum objave v RUNG:08.10.2020
Število ogledov:2427
Število prenosov:0
Metapodatki:XML RDF-CHPDL DC-XML DC-RDF
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Vaša ocena:Ocenjevanje je dovoljeno samo prijavljenim uporabnikom.
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Gradivo je del monografije

Naslov:European Geophysics Union, General Assembly 2020, 4–8 May 2020
Kraj izida:Online
Založnik:Copernicus GmbH
Leto izida:2020
Prireditelj konference:European Geophysics Union

Gradivo je financirano iz projekta

Financer:ARRS - Agencija za raziskovalno dejavnost Republike Slovenije
Številka projekta:P1-0031
Naslov:Astrofizika osnovnih delcev

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