Pregled bibliografske jedinice broj: 299716
"Comparison of the Prandtl model with K(z) and non-zero f with Doppler sodar observations"
"Comparison of the Prandtl model with K(z) and non-zero f with Doppler sodar observations" // 29th International Conference on Alpine Meteorology - Extended Abstracts
Chambéry, Francuska: Météo-France, 2007. str. 597-600 (poster, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
CROSBI ID: 299716 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
"Comparison of the Prandtl model with K(z) and non-zero f with Doppler sodar observations"
Autori
Kavčič, Iva ; Grisogono, Branko ; Renfrew, Ian A. ; Anderson, Philip S. ; Večenaj, Željko ; Stiperski, Ivana
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
29th International Conference on Alpine Meteorology - Extended Abstracts
/ - : Météo-France, 2007, 597-600
Skup
29th International Conference on Alpine Meteorology
Mjesto i datum
Chambéry, Francuska, 04.06.2007. - 08.06.2007
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Stable boundary layer; Prandtl model; Doppler sodar data
Sažetak
We present the analytical and numerical solutions for (U, V) depending on (z, t) in the katabatic flow, where U and V are the downslope and cross-slope wind components. The solutions for (U, V) from the recently extended analytical 1D Prandtl model are verified against observations (the 15-min averages) from a novel autonomous Doppler sodar wind profiling system in Antarctica. Two cases of the wintertime, primarily katabatically driven, flows with the different stability values are investigated. The analytical and numerical model parameters are calculated from the Doppler sodar and AWS (automatic weather station) data. Observations of the downslope component are generally better described by the model solutions, especially in the case of the stronger stability. The model solutions for V agree qualitatively with the observations, but are not accurate enough in determining the height and the speed of the V maximum. Therefore, further improvements of the Prandtl model will be amendable as well as recommendations for a better parameterization of katabatic flows in large-scale numerical models.
Izvorni jezik
Engleski
Znanstvena područja
Matematika, Geologija
POVEZANOST RADA
Projekti:
037-1193086-2771 - Numeričke metode u geofizičkim modelima (Singer, Saša, MZOS ) ( CroRIS)
119-1193086-1311 - Bazične ORografske Atmosferske cirkulacije u Hrvatskoj (BORA) (Grisogono, Branko, MZOS ) ( CroRIS)
004-1193086-3036 - Oluje i prirodne katastrofe u Hrvatskoj (Ivančan-Picek, Branka, MZOS ) ( CroRIS)
Ustanove:
Državni hidrometeorološki zavod,
Prirodoslovno-matematički fakultet, Matematički odjel, Zagreb,
Prirodoslovno-matematički fakultet, Zagreb