Nalazite se na CroRIS probnoj okolini. Ovdje evidentirani podaci neće biti pohranjeni u Informacijskom sustavu znanosti RH. Ako je ovo greška, CroRIS produkcijskoj okolini moguće je pristupi putem poveznice www.croris.hr
izvor podataka: crosbi !

Micro-Scale Properties of Different Bora Types (CROSBI ID 249773)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Šoljan, Vinko ; Belušić, Andreina ; Šarović, Kristina ; Nimac, Irena ; Brzaj, Stjepana ; Suhin, Jurica ; Belavić, Martin ; Večenaj, Željko ; Grisogono, Branko Micro-Scale Properties of Different Bora Types // Atmosphere, 9 (2018), 4; 116, 25. doi: 10.3390/atmos9040116

Podaci o odgovornosti

Šoljan, Vinko ; Belušić, Andreina ; Šarović, Kristina ; Nimac, Irena ; Brzaj, Stjepana ; Suhin, Jurica ; Belavić, Martin ; Večenaj, Željko ; Grisogono, Branko

engleski

Micro-Scale Properties of Different Bora Types

In this paper we use 20 Hz wind measurements on three levels (2, 5, and 10 m) to investigate the differences in micro-scale properties of different bora types, i.e., deep and shallow bora with further subdivision to cyclonic and anticyclonic bora cases. Using Fourier spectral analysis, we investigate a suitable turbulence averaging scale and bora gust pulsations. The obtained data set is further used to test the Monin–Obukhov similarity theory, the surface layer stratification, the behavior of the terms in the prognostic turbulence kinetic energy equation, and the wind profiles. One of our main goals is to identify possible micro-scale differences between shallow and deep bora types because of the possible different mountain wave dynamics in those flows. We found that a turbulence averaging scale of 30 min is suitable for this location and is in agreement with previous bora studies. The wind speed power spectral densities of all selected bora episodes showed pulsations with periods of 2–8 min. This suggests that mountain wave breaking was present in all cases, regardless of flow depth and synoptic type. The stability parameter analysis confirmed the near-neutral thermal stratification of bora ; a consequence of intensive mechanical mixing. No significant differences related to bora type were observed in other micro-scale parameters.

bora ; turbulence ; micro-scale ; pulsations ; wind profiles ; surface layer ; mountain wave

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

Podaci o izdanju

9 (4)

2018.

116

25

objavljeno

2073-4433

10.3390/atmos9040116

Povezanost rada

Geofizika

Poveznice
Indeksiranost