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| Model: |
GFS (Global Forecast System) Global Model from the "National Centers for Environmental Prediction" (NCEP) |
| Update: |
4 times per day, from 3:30, 09:30, 15:30 und 21:30 GMT |
| Greenwich Mean Time: |
12:00 GMT = 13:00 BST |
| Parameter: |
Dew-point at 2m across the British Isles in hPa/h |
| Description: |
The dew-point is the temperature air would have to be cooled to in order for
saturation to occur. The dew-point temperature assumes there is no change in
air pressure or moisture content of the air. Dew-point does not change with
temperature of the air; very much different from relative humidity.
The dew-point can be used to forecast low temperatures. The low will rarely
fall far below the observed dew-point value in the evening (unless a front
brings in a different air mass). Once the temperature drops to the
dew-point, latent heat must be released to the atmosphere for the
condensation process to take effect. This addition of heat offsets some or
all of further cooling.
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