Water turbulence affects wind fetch badly. The rising and falling peaks and troughs mess up the flow big time. Contrast that to say, Sandy Point where there is an open fetch with wind coming of a solid sand-bank. Ther eis no disturbance to the flow there, and the wind can really get itself organised. The results prove that.
Get stuck in the trough of a big set of waves and there is no wind. You can feel the dramatic difference as you rise up onto the crest of a swell. You get the same compression effect as a dune or hill gives. So a steady 12kts at 10m up feels like 6 in the trough and 16-17 on the crest.
Places like Elliott Hds where you get a ton of tall wind chop right in the river mouth, especially on a wind against tide, suffer a lot. It an be a solid 30kt howler, and there will be dead spots that nearly kill you.
It's not always a sunny well-mixed day and I'm not really a flat water, large gear sailor either.
Sure, those conditions are easy to call, and I'm not saying that me or anyone else can never estimate wind right.
It's more that some conditions can be difficult to gauge accurately, and then it's nice to have an objective measure to help.
All weather systems are emergent. That is, while there it is possible to define the set of rules that make it function, there is such a high level of complexity that you have to run the system to see what will actually happen.
More than 3 days out and it becomes chaotic.
Which is why 7 day forecasts are rarely if ever on the money.
Ian K said...
Ken. Why would there be good wind at 10 metres but none at the surface? The ratio varies a bit but surely not not by that much on a sunny well-mixed day over the same patch of water. What do the kiters say, they can sample both heights very easily?
Not sure that wind qualifies as an emergent system type of behaviour, it's bad but not that bad, that's more global economy sort of unpredicability.