I would post this query in Science and Technology except it's mostly tumbleweed and low footfall in there nowadays.
In part one of a BBC 4 documentary "Wild Weather" shown yesterday evening, Richard "The Hamster" Hammond claimed that you can forecast oncoming weather trends with some degree of accuacy by standing with your back to the surface wind and observing the direction that higher-level clouds are moving as compared to lower-level ones:
Anyway, while his advice fits for an approaching low pressure (cyclonic) frontal system, where wind shear turns near-ground winds away from the Coriolis effect imposed tendency to follow the isobars and instead makes them tend to head towards the centre of the system (observable as an apparent clockwise turning of higher-level clouds' velocity vectors with respect to those of lower level clouds - anticlockwise in southern hemisphere), I don't see that it works as he describes after the fronts have passed over you and you're still in the low-pressure system (the velocity vectors tend to align again but don't reverse rotation).
His advice also probably works even less well for high pressure (anticyclonic) systems. These can occasionally be associated with persistent stratus or stratocumulus clouds (so-called "anticyclonic gloom") - in maritime Europe for moist, tropical air at least. The velocity vectors would rotate anticlockwise and back again to alignment (clockwise for southern hemisphere). However, I expect there are usually very few clouds to observe at different levels and often there are almost no visible clouds at all in anticyclonic systems.
Anyway, can anyone more versed in meteorological study comment on Hammond's suggested forecasting system?
The whole series is worth watching anyway as there's a lot more interesting stuff on show. The section I'm rattling on about starts at about t=10 minutes.
In part one of a BBC 4 documentary "Wild Weather" shown yesterday evening, Richard "The Hamster" Hammond claimed that you can forecast oncoming weather trends with some degree of accuacy by standing with your back to the surface wind and observing the direction that higher-level clouds are moving as compared to lower-level ones:
- If same direction, likely no change
- If left to right, weather will likely take a turn for the worse
- If right to left, weather will likely improve
Anyway, while his advice fits for an approaching low pressure (cyclonic) frontal system, where wind shear turns near-ground winds away from the Coriolis effect imposed tendency to follow the isobars and instead makes them tend to head towards the centre of the system (observable as an apparent clockwise turning of higher-level clouds' velocity vectors with respect to those of lower level clouds - anticlockwise in southern hemisphere), I don't see that it works as he describes after the fronts have passed over you and you're still in the low-pressure system (the velocity vectors tend to align again but don't reverse rotation).
His advice also probably works even less well for high pressure (anticyclonic) systems. These can occasionally be associated with persistent stratus or stratocumulus clouds (so-called "anticyclonic gloom") - in maritime Europe for moist, tropical air at least. The velocity vectors would rotate anticlockwise and back again to alignment (clockwise for southern hemisphere). However, I expect there are usually very few clouds to observe at different levels and often there are almost no visible clouds at all in anticyclonic systems.
Anyway, can anyone more versed in meteorological study comment on Hammond's suggested forecasting system?
The whole series is worth watching anyway as there's a lot more interesting stuff on show. The section I'm rattling on about starts at about t=10 minutes.
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