Due to the combinate effect of the background wind, the translation of the downburst and the radial nature of the jet after the touchdown, a peculiar characteristic of a signal associated to a thunderstorm outflow measured by an anemometer is the potential variation of direction during the life of the event. Despite this situation, the study of the dynamic response of structures to thunderstorm outflows has traditionally neglected the angle of attack and the effects induced by that, implicitly assuming the response as alongwind. This paper proposes two methods to consider the role of the direction and its possible variation into the evaluation of dynamic response of structures subjected to Aeolian events. In particular, the second one is ba...
The European Projects “Wind and Ports” and “Wind, Ports and Sea” gave rise to an extensive wind moni...
The study aims to estimate the maximum dynamic response of linear elastic SDOF systems subjected to ...
Thunderstorms are destructive phenomena at the mesoscale with extension of few kilometres and short ...
Due to the combined effect of the background wind, the translation of the downburst and the radial n...
Thunderstorm outflows are usually analysed by decomposing their horizontal velocity into a slowly-va...
Thunderstorms are transient events. Design wind velocity and wind-induced damage are often related t...
The study of thunderstorm outflows and their actions on structures is a dominant topic of wind engin...
Thunderstorms are frequent phenomena that cause wind speeds and wind-induced damage often greater th...
Literature is rich about studies which concern the insurgence of instability of structural systems u...
The climatology at mid-latitudes (for instance, Europe) is dominated by both extra-tropical depressi...
This paper presents a review of thunderstorm dynamics through the use of the vorticity equation with...
The study of thunderstorm outflows and their effects on structures is a key topic in modern wind eng...
The dynamic complexity and the limited spatiotemporal structure of thunderstorms make the collection...
The study of thunderstorm outflows and their loading and response of structures is a key topic in mo...
Thunderstorm winds, i.e. downbursts, are cold descending currents originating from cumulonimbus clou...
The European Projects “Wind and Ports” and “Wind, Ports and Sea” gave rise to an extensive wind moni...
The study aims to estimate the maximum dynamic response of linear elastic SDOF systems subjected to ...
Thunderstorms are destructive phenomena at the mesoscale with extension of few kilometres and short ...
Due to the combined effect of the background wind, the translation of the downburst and the radial n...
Thunderstorm outflows are usually analysed by decomposing their horizontal velocity into a slowly-va...
Thunderstorms are transient events. Design wind velocity and wind-induced damage are often related t...
The study of thunderstorm outflows and their actions on structures is a dominant topic of wind engin...
Thunderstorms are frequent phenomena that cause wind speeds and wind-induced damage often greater th...
Literature is rich about studies which concern the insurgence of instability of structural systems u...
The climatology at mid-latitudes (for instance, Europe) is dominated by both extra-tropical depressi...
This paper presents a review of thunderstorm dynamics through the use of the vorticity equation with...
The study of thunderstorm outflows and their effects on structures is a key topic in modern wind eng...
The dynamic complexity and the limited spatiotemporal structure of thunderstorms make the collection...
The study of thunderstorm outflows and their loading and response of structures is a key topic in mo...
Thunderstorm winds, i.e. downbursts, are cold descending currents originating from cumulonimbus clou...
The European Projects “Wind and Ports” and “Wind, Ports and Sea” gave rise to an extensive wind moni...
The study aims to estimate the maximum dynamic response of linear elastic SDOF systems subjected to ...
Thunderstorms are destructive phenomena at the mesoscale with extension of few kilometres and short ...