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  2. Dew point depression - Wikipedia

    en.wikipedia.org/wiki/Dew_point_depression

    The dew point depression (T-Td) is the difference between the temperature and dew point temperature at a certain height in the atmosphere. A lower dew point depression indicates that the air is more moist at a given temperature. [1]: 83

  3. Dew point - Wikipedia

    en.wikipedia.org/wiki/Dew_point

    Highest dew point temperature: A dew point of 35 °C (95 °F) — while the temperature was 42 °C (108 °F) — was observed at Dhahran, Saudi Arabia, at 3:00 p.m. on 8 July 2003. [ 14 ] [ 15 ] Measurement

  4. Cloud base - Wikipedia

    en.wikipedia.org/wiki/Cloud_base

    Find the difference between the surface temperature and the dew point. This value is known as the "spread". Divide the spread by 4.4 (if temperatures are in °F) or 2.5 (if temperatures are in °C), then multiply by 1000. This will give the altitude of the cloud base in feet above ground level. Put in a simpler way, 400 feet for every 1°C dew ...

  5. Rain spreads into Southern California - AOL

    www.aol.com/weather/beneficial-rain-way-southern...

    Rising dew points and measurable rainfall will expand across the parched valleys, while mountain snow can develop in the cooler spots above 3,000-4,000 Rain spreads into Southern California Skip ...

  6. Get the Boydton, VA local weather forecast by the hour and the next 10 days.

  7. Weather forecasting - Wikipedia

    en.wikipedia.org/wiki/Weather_forecasting

    The low temperature forecast for the current day is calculated using the lowest temperature found between 7 pm that evening through 7 am the following morning. [95] So, in short, today's forecasted low is most likely tomorrow's low temperature.

  8. Convective available potential energy - Wikipedia

    en.wikipedia.org/wiki/Convective_available...

    The red line is temperature, the green line is the dew point, and the black line is the air parcel lifted. In meteorology, convective available potential energy (commonly abbreviated as CAPE), [1] is a measure of the capacity of the atmosphere to support upward air movement that can lead to cloud formation and storms.

  9. Convective condensation level - Wikipedia

    en.wikipedia.org/wiki/Convective_condensation_level

    The LCL is less than or equal to the CCL depending on the temperature profile. Both condensation levels indicate the altitude (or pressure) where relative humidity reaches 100%. However, since the actual condensation level depends on the availability of condensation nuclei, clouds typically do not form until the relative humidity is somewhat ...