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  2. Dew point - Wikipedia

    en.wikipedia.org/wiki/Dew_point

    The dew point of a given body of air is the temperature to which it must be cooled to become saturated with water vapor. This temperature depends on the pressure and water content of the air. When the air is cooled below the dew point, its moisture capacity is reduced and airborne water vapor will condense to form liquid water known as dew. [1]

  3. Climate of Florida - Wikipedia

    en.wikipedia.org/wiki/Climate_of_Florida

    Florida counties with tropical climates include Miami-Dade, Broward, Palm Beach, Lee, Collier, and Monroe counties. A narrow eastern part of the state including Orlando and Jacksonville receives between 2,400 and 2,800 hours of sunshine annually. The rest of the state, including Miami, receives between 2,800 and 3,200 hours annually. [45]

  4. Climate of the Tampa Bay area - Wikipedia

    en.wikipedia.org/wiki/Climate_of_the_Tampa_Bay_area

    Cumulus clouds building over the Tampa Convention Center on a summer afternoon. The warm and rainy season typically begins in late May and runs through October. [5] Average high temperatures are in the low 90s °F (around 32 °C) with lows in the mid-70s °F (around 24 °C) during this period, and the combination of warm temperatures and high humidity brings an almost daily chance of rain and ...

  5. Glossary of meteorology - Wikipedia

    en.wikipedia.org/wiki/Glossary_of_meteorology

    Also dewpoint or dew-point. The temperature to which an air parcel must be cooled, at constant pressure and moisture content, in order for saturation to occur. Continued cooling below the dew point will cause condensation of water droplets if atmospheric conditions are favorable. Dew point is often used as a proxy by which to indicate the ...

  6. Station model - Wikipedia

    en.wikipedia.org/wiki/Station_model

    Station model plots use an internationally accepted coding convention that has changed little since August 1, 1941. Elements in the plot show the key weather elements, including temperature, dew point, wind, cloud cover, air pressure, pressure tendency, and precipitation. [2] [3]

  7. Dry-bulb temperature - Wikipedia

    en.wikipedia.org/wiki/Dry-bulb_temperature

    The dry-bulb temperature (DBT) is the temperature of air measured by a thermometer freely exposed to the air, but shielded from radiation. [1] The dry-bulb temperature is the temperature that is usually thought of as air temperature, and it is the true thermodynamic temperature.

  8. Dew - Wikipedia

    en.wikipedia.org/wiki/Dew

    This process distinguishes dew from those hydrometeors (meteorological occurrences of water), which form directly in air that has cooled to its dew point (typically around condensation nuclei), such as fog or clouds. The thermodynamic principles of formation, however, are the same. Dew is commonly formed during select times of the day.

  9. List of weather records - Wikipedia

    en.wikipedia.org/wiki/List_of_weather_records

    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. [ 200 ] Highest heat index : In the observation above at Dhahran, Saudi Arabia, the heat index ("feels like" temperature) was 81.1 °C (178.0 °F).

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