<p>MM5 wind intensities and directions, clockwise from the north in degrees, computed (3 km resolution) every 3 hours at 10 m above sea level at a location corresponding to Somlit station; a) forcing conditions for the computation of June 2008; b) forcing conditions for the computation of October 2011; times for particle release (WWTP outlet) and model outputs (current fields and particle trajectories) are mentioned in each time series; Note the different scale of wind vectors in Figs 3a and 3b.</p
In order to evaluate the accuracy of offshore wind simulation with the mesoscale model MM5, long-ter...
Special issue The Copernicus Marine Environment Monitoring Service (CMEMS): scientific advances.-- 22...
Lagrangian trajectories of three particles launched at 500, 1500 and 3000m levels. Particles are the...
Presentation at the EAWE PhD Seminar 2021 Understanding the in-situ wind conditions and climatology...
ERA5 atmospheric fields showing the development of the PL on 25 March 2019 at (a) 0000 UTC, (b) 0600...
Offshore wind power projects are critically reliant on accurate wind resources assessment and large ...
To date, evaluation studies of global circulation models (GCMs) generally focus on large-scale circu...
Terrain from the 36 km domain is shaded every 500 m using the inset key. The surface and upper-air s...
Hybrid Coordinate Ocean Model (HYCOM) output from 2 forced regional simulations of the Agulhas Curre...
In the context of FLEXIPAC project funded by "RELIABLE" program of Walloon Region (Belgium), the Lab...
13 pages, 6 figures, 1 appendixAt the OSI SAF 3rd user workshop in Amsterdam (September 2007), sever...
Time series of the (a) RMSE-VWD of the simulated and ERA5 10-m wind, and RMSE of the simulated and E...
Climatological surface wind speed probability density functions (PDFs) estimated from observations a...
Herewith we present the dataset of wind measurements from a Skipheia meteorological station on the i...
<p>Superimposed are wind vectors (pink) at 10 m above ground level, generated from 12 km re-analysis...
In order to evaluate the accuracy of offshore wind simulation with the mesoscale model MM5, long-ter...
Special issue The Copernicus Marine Environment Monitoring Service (CMEMS): scientific advances.-- 22...
Lagrangian trajectories of three particles launched at 500, 1500 and 3000m levels. Particles are the...
Presentation at the EAWE PhD Seminar 2021 Understanding the in-situ wind conditions and climatology...
ERA5 atmospheric fields showing the development of the PL on 25 March 2019 at (a) 0000 UTC, (b) 0600...
Offshore wind power projects are critically reliant on accurate wind resources assessment and large ...
To date, evaluation studies of global circulation models (GCMs) generally focus on large-scale circu...
Terrain from the 36 km domain is shaded every 500 m using the inset key. The surface and upper-air s...
Hybrid Coordinate Ocean Model (HYCOM) output from 2 forced regional simulations of the Agulhas Curre...
In the context of FLEXIPAC project funded by "RELIABLE" program of Walloon Region (Belgium), the Lab...
13 pages, 6 figures, 1 appendixAt the OSI SAF 3rd user workshop in Amsterdam (September 2007), sever...
Time series of the (a) RMSE-VWD of the simulated and ERA5 10-m wind, and RMSE of the simulated and E...
Climatological surface wind speed probability density functions (PDFs) estimated from observations a...
Herewith we present the dataset of wind measurements from a Skipheia meteorological station on the i...
<p>Superimposed are wind vectors (pink) at 10 m above ground level, generated from 12 km re-analysis...
In order to evaluate the accuracy of offshore wind simulation with the mesoscale model MM5, long-ter...
Special issue The Copernicus Marine Environment Monitoring Service (CMEMS): scientific advances.-- 22...
Lagrangian trajectories of three particles launched at 500, 1500 and 3000m levels. Particles are the...