Land/sea breezes Temperature imbalance between land and sea causes onshore wind in the day time and offshore at night. Due to Diurnal variation, maximum wind strength occurs in the afternoon. If you want to shoot a relaxed scene on the top of the cliffs (subject to light), try to shoot in the morning.
Clouds (or how much sunshine can we expect?). There are numerous individual titles for cloud types, but they can be broken down into two main types.
Stratus = layer cloud, no direct sun, amount of light depends on thickness of cloud. Cumulus = towering type, sun then shade etc.
There are also three altitudes 'low' = low, 'alto' = medium, 'cirro' = high. The only other name to remember is 'cumulo numbus' = thunderstorms.
Fog = visibility less than 1,000m. Mist = visibility 1 -10km. The classic localised fairyland mists will only form with overnight clear skies, cool moist air and a light wind. If there is no wind, a dew forms and if a strong wind, cloud forms.
Burn Off is a terms which has more film than meteorological use for the re-absorption of visible moisture and thus improvement in visibility, often confused with thermal lifting of mist as the earth's surface warms. If either hasn't happened by mid-afternoon, forget it.
Finally, there are often request to 'phone around' to get a better forecast. It should be understood that the Met Office compile all the weather data at their headquarters in Bracknell (they have the most powerful computer in the world there). The general situation and forecasts are then transmitted out to the many weather information services. Local airfields may or may not have a Met Office but are often used as a recording centre and have a localised knowledge of the interpretation and how it affects their area; but with the availability of pre-recorded area forecasts, many are now reluctant to help.
Forecasts beyond three days tend to be unreliable, long range non existent.
There are many who study meteorology who believe that in recent years (since they got it so wrong in the storms) that forecasts have tended to become pessimistic. Meteorologists probably work on the theory that you'll never meet a disappointed pessimist.
This is not helpful to us as film makers, thus the more that you can cross reference and self interpret weather charts the better.
At the end of the day and this is entirely serious, especially in hilly and mountainous areas, it is often the local farmer or fisherman who may not know about global climatology but can probably predict more accurately the weather in their specific area. |