Abstract: Especially important for the coastal area of Croatia is the wind forecast, particularly during the bura windstorm episodes. Current operational version of ALADIN model is rather satisfactory for the wind field forecast, although in many cases the wind speed is somewhat overestimated. A modified sub-grid scale orography representation was introduced and tested. The envelope was removed and to compensate for the loss of volume, changes in gravity wave drag parametrisation were introduced. New orography representation resulted in slight enhancement of upstream and general decrease of downstream wind speed, as well as reduction of mountain wave amplitude
The wind output from atmospheric models is instrumental in forcing the oceanic models. Here we consi...
Bora is a cold, strong, low level wind which blows mainly from NE along the Adriatic coast. However,...
The Bora is a cold, strong, low level wind which blows from the northeast along the Adriatic coast (...
Bura is a strong wind with severe gusts; it occurs suddenly and affects safety of life at sea. It ha...
Nonhydrostatic mesoscale model MM5 was used in order to model a spatial distribution of bura wind in...
The results of numerically modeled wind speed climate, a primary component of wind energy resource a...
ALADIN model 10m wind forecast for Dubrovnik area for +3h-72h time range based on 00 and 12 UTC run...
This paper presents the results of the verification of operational 10 m wind forecast obtained with ...
Downslope windstorm ( bora wind ) are observed, mostly during the winter season, in the adriatic are...
Knowing the wind properties is a key to the assessment of wind energy resources and for wind power f...
The ALADIN model was used for downscaling of the ECMWF 40-years re-analysis dataset with a goal to p...
ALADIN model 10m wind forecast for Zadar area for +3h-72h time range based on 00 and 12 UTC run. Th...
This paper describes two numerical models for computing the mesoscale influences of orography, frict...
ALADIN model 10m wind forecast for Istra and Kvarner for +3h-72h time range based on 00 and 12 UTC ...
In order to better understand the influence of initial and boundary conditions on the numerical mode...
The wind output from atmospheric models is instrumental in forcing the oceanic models. Here we consi...
Bora is a cold, strong, low level wind which blows mainly from NE along the Adriatic coast. However,...
The Bora is a cold, strong, low level wind which blows from the northeast along the Adriatic coast (...
Bura is a strong wind with severe gusts; it occurs suddenly and affects safety of life at sea. It ha...
Nonhydrostatic mesoscale model MM5 was used in order to model a spatial distribution of bura wind in...
The results of numerically modeled wind speed climate, a primary component of wind energy resource a...
ALADIN model 10m wind forecast for Dubrovnik area for +3h-72h time range based on 00 and 12 UTC run...
This paper presents the results of the verification of operational 10 m wind forecast obtained with ...
Downslope windstorm ( bora wind ) are observed, mostly during the winter season, in the adriatic are...
Knowing the wind properties is a key to the assessment of wind energy resources and for wind power f...
The ALADIN model was used for downscaling of the ECMWF 40-years re-analysis dataset with a goal to p...
ALADIN model 10m wind forecast for Zadar area for +3h-72h time range based on 00 and 12 UTC run. Th...
This paper describes two numerical models for computing the mesoscale influences of orography, frict...
ALADIN model 10m wind forecast for Istra and Kvarner for +3h-72h time range based on 00 and 12 UTC ...
In order to better understand the influence of initial and boundary conditions on the numerical mode...
The wind output from atmospheric models is instrumental in forcing the oceanic models. Here we consi...
Bora is a cold, strong, low level wind which blows mainly from NE along the Adriatic coast. However,...
The Bora is a cold, strong, low level wind which blows from the northeast along the Adriatic coast (...