franksingleton
Well-known member
Frank, I've been trying to understand for years why the mesoscale models on let's say WindguruPro are much closer to actual coastal winds than GFS, which on the day almost always seems to be about 1 force too low. Let's take the Devon & Cornwall coast where I am now (Dartmouth to Falmouth). Are the higher res. models taking account of topography as you say, or sea breeze, or what? The fact is that over many years (in West Wales as well) they always seem to give higher forecast values and these are closer to actual in many if not most cases.
The performance of all meso-scale models will depend, ultimately, on the large scale forecast ie they have to take in data from global models or, better still, run globally on a meso-scale size grid. The latter is not possible at present because of computer power.
Meso-scale models do represent topography better than the GFS simply because the grid points are closer together. However, all models can only represent weather and topography on a scale of about 4 or 5 grid lengths. On one of my pages I give the case of the isle of Man. To represent the shape and topography of the IOM would need a very close grid. As far as I am aware the Windguru that you pay for uses a grid of around 10 km. It can only represent topography on a scale of about 40 or 50 km.
The free version of Windguru is, as far as I know, just the GFS interpolated. Hence, I would not expect the free version to be any better than the GFS. I would expect some improvement on the GFS with the paid for version BUT only when the global forecast is good and, usually, when there is a fairly static situation. That is why the SWS will often do better than the GFS through the Gibraltar Strait but be no better in predicting the change from E to W winds through the Strait. That is a result of large scale – “synoptic” scale patterns.
Does that help?