Pregled bibliografske jedinice broj: 87840
Idealised numerical simulations of aerodynamical roughness lenght effects on sea breeze characteristics
Idealised numerical simulations of aerodynamical roughness lenght effects on sea breeze characteristics // Air Pollution Modelling and Simulation – ; Proceedings Second Conference on Air Pollution Modelling and Simulation, APMS'01 / Sportisse, Bruno (ur.).
Pariz: Springer, 2001. str. 553-556 (poster, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
CROSBI ID: 87840 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Idealised numerical simulations of aerodynamical roughness lenght effects on sea breeze characteristics
Autori
Telišman Prtenjak, Maja
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Air Pollution Modelling and Simulation – ; Proceedings Second Conference on Air Pollution Modelling and Simulation, APMS'01
/ Sportisse, Bruno - Pariz : Springer, 2001, 553-556
Skup
Second Conference on Air Pollution Modelling and Simulation, APMS'01,
Mjesto i datum
Pariz, Francuska, 09.04.2001. - 12.04.2001
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Coastal meteorology; roughness length; sea breeze; sea breeze front
Sažetak
A two-dimensional hydrostatic meso-gamma-scale model is used to study possible effects of a step change in roughness on the daytime sea breeze (SB). Idealised numerical simulations with the length of aerodynamical roughness (z0) ranging from 0.05m to 1.0 m and by an increase of 0.05 m in all land surface grid points were made. Two z0 effects could be pointed out: an increase in the mixing process and a reduction in the wind speeds in the surface layer. An increase of both heights and magnitudes of the SB circulation, caused by a vertical extension of the turbulent field, followed by a faster inland penetration of the SB. The second effect resulting from a successive increase in z0 values was a retardation of the sea breeze front near the ground, visible in its slope. This effect allowed the already faster inland penetration of the marine air high above the land.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
119299
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Maja Telišman Prtenjak
(autor)