Pregled bibliografske jedinice broj: 391261
How realistic is the meandering reproduced by a numerical model?
How realistic is the meandering reproduced by a numerical model? // European Geosciences Union General Assembly 2009
Beč, 2009. (poster, nije recenziran, sažetak, znanstveni)
CROSBI ID: 391261 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
How realistic is the meandering reproduced by a numerical model?
Autori
Belušić, Danijel ; Güttler, Ivan
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
European Geosciences Union General Assembly 2009
/ - Beč, 2009
Skup
European Geosciences Union General Assembly 2009
Mjesto i datum
Beč, Austrija, 19.04.2009. - 24.04.2009
Vrsta sudjelovanja
Poster
Vrsta recenzije
Nije recenziran
Ključne riječi
submesoscale motions; WRF/Chem
Sažetak
It has been shown that meandering motions in the boundary layer influence horizontal dispersion to a large extent. They are frequently characterized by sudden shifts of wind direction and the related frequency distributions are often bi- or multi-modal. Unlike turbulence, which is dealt with through its more or less known scaling properties, it seems that no local similarity applies to meandering. Additionally, these motions are of generally unknown origin and numerical modelling at various scales also fails to reproduce them. Nevertheless, recent modelling efforts show that it is possible to reproduce the variability related to meandering under certain conditions. Namely, with reduced horizontal diffusion, or in its absence, the modelled fields are naturally more variable. It has been shown that the strength of this variability matches the measured variability at the same submeso scales. Here we inspect how realistic this variability is. The agreement of the modelled and measured submesoscale variability during a CASES-99 night is examined in details. Aside of the behaviour of the wind speed components at various levels in the atmosphere, an important test takes into account the dynamics of a plume under these conditions. To the degree that the modelled results are realistic, they may be used for understanding the basic mechanisms of meandering motions.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
119-1193086-1323 - Kakvoća zraka nad kompleksnom topografijom (Bencetić-Klaić, Zvjezdana, MZOS ) ( CroRIS)
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb