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  2. Dew point - Wikipedia

    en.wikipedia.org/wiki/Dew_point

    The dew point temperature equals the air temperature when the air is saturated with water; in all other cases the dew point will be less than the air temperature. [ 6 ] : 129 In technical terms, the dew point is the temperature at which the water vapor in a sample of air at constant barometric pressure condenses into liquid water at the same ...

  3. Lifting condensation level - Wikipedia

    en.wikipedia.org/wiki/Lifting_condensation_level

    His equation makes use of the relationship between the LCL and dew point temperature discussed above. In the Earth's atmosphere near the surface, the lapse rate for dry adiabatic lifting is about 9.8 K/km, and the lapse rate of the dew point is about 1.8 K/km (it varies from about 1.6-1.9 K/km). This gives the slopes of the curves shown in the ...

  4. Convective condensation level - Wikipedia

    en.wikipedia.org/wiki/Convective_condensation_level

    The CCL is determined by plotting the dew point (100%RH) versus altitude and locating the intersection with the actual measured temperature sounding. It marks where the cloud base begins when air is heated from below to the convective temperature , without mechanical lift.

  5. Psychrometrics - Wikipedia

    en.wikipedia.org/wiki/Psychrometrics

    Dew point temperature: From the state [clarification needed] point follow the horizontal line of constant humidity ratio to the intercept of 100% RH, also known as the saturation curve. The dew point temperature is equal to the fully saturated dry bulb or wet bulb temperatures.

  6. How much rain did we get? Here’s a breakdown of rainfall ...

    www.aol.com/news/much-rain-did-breakdown...

    Here are rainfall amounts, in inches, from the last 24 hours (unless otherwise noted) by locality, according to National Weather Service St. Louis: Illinois locations Belleville: 6.23, 6.33

  7. 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.

  8. How much rain did Des Moines get? Here are Wednesday's Iowa ...

    www.aol.com/much-rain-did-des-moines-150405273.html

    Some areas saw more than an inch and a half of rain at a time when Iowa is once again facing drought conditions.

  9. How much rain did Des Moines get last night? Here are the ...

    www.aol.com/much-rain-did-des-moines-152144866.html

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