Bura is strong and gusty wind common for the eastern Adriatic coast, with the most severe events beneath southern part of Velebit mountain. Due to traffic significance of the area and the fact that bura has strong impact on traffic, it is necessary to forecast the bura speed, onset and duration. A mesoscale nonhydrostatic numerical weather prediction model MM5 is employed in order to test and verify the model capabilities of forecasting wind speeds and spatial variabilities on very fine domain resolution of 1 km. During the winter 2003-2004 several bura events were recorded. The longest bura event, taking place from 22-25 December 2003 is analyzed. The model results are compared with the measured data taken from four automatic stations loca...
The results of numerically modeled wind speed climate, a primary component of wind energy resource a...
A combination of recent intensive observations and simulations with two numerical models is used to ...
Five typical north Adriatic bora storms are presented from the period 1957-1986. lt is shown that se...
Bura is strong and gusty wind common for the eastern Adriatic coast, with the most severe events ben...
We investigated the dynamics and structure of a severe bura event. Apart from the routine meteorolog...
Nonhydrostatic mesoscale model MM5 was used in order to model a spatial distribution of bura wind in...
International audienceNumerical simulations of a bora event, recently occurred in the Adriatic area,...
In this paper we explore onset and duration of several severe Bura events, focusing on the circulati...
Bura is a strong wind with severe gusts; it occurs suddenly and affects safety of life at sea. It ha...
Two days with bora has been numerically analysed, using a three dimensional hydrostatic mesoscale mo...
Bora is a cold, strong, low level wind which blows mainly from NE along the Adriatic coast. However,...
We have investigated a strong Bora event over the Northern Adriatic, which occurred on 7 November 19...
Downslope windstorm ( bora wind ) are observed, mostly during the winter season, in the adriatic are...
Bora, a mesoscale wind system on the eastern Adriatic coast, profoundly impacts the local weather co...
This study presents a numerical simulation of the bora wind as it occurs in form of a severe wind bl...
The results of numerically modeled wind speed climate, a primary component of wind energy resource a...
A combination of recent intensive observations and simulations with two numerical models is used to ...
Five typical north Adriatic bora storms are presented from the period 1957-1986. lt is shown that se...
Bura is strong and gusty wind common for the eastern Adriatic coast, with the most severe events ben...
We investigated the dynamics and structure of a severe bura event. Apart from the routine meteorolog...
Nonhydrostatic mesoscale model MM5 was used in order to model a spatial distribution of bura wind in...
International audienceNumerical simulations of a bora event, recently occurred in the Adriatic area,...
In this paper we explore onset and duration of several severe Bura events, focusing on the circulati...
Bura is a strong wind with severe gusts; it occurs suddenly and affects safety of life at sea. It ha...
Two days with bora has been numerically analysed, using a three dimensional hydrostatic mesoscale mo...
Bora is a cold, strong, low level wind which blows mainly from NE along the Adriatic coast. However,...
We have investigated a strong Bora event over the Northern Adriatic, which occurred on 7 November 19...
Downslope windstorm ( bora wind ) are observed, mostly during the winter season, in the adriatic are...
Bora, a mesoscale wind system on the eastern Adriatic coast, profoundly impacts the local weather co...
This study presents a numerical simulation of the bora wind as it occurs in form of a severe wind bl...
The results of numerically modeled wind speed climate, a primary component of wind energy resource a...
A combination of recent intensive observations and simulations with two numerical models is used to ...
Five typical north Adriatic bora storms are presented from the period 1957-1986. lt is shown that se...