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  2. Humidity - Wikipedia

    en.wikipedia.org/wiki/Humidity

    Water vapor is a lighter gas than other gaseous components of air at the same temperature, so humid air will tend to rise by natural convection. This is a mechanism behind thunderstorms and other weather phenomena. Relative humidity is often mentioned in weather forecasts and reports, as it is an indicator of the likelihood of dew, or fog.

  3. Air mass - Wikipedia

    en.wikipedia.org/wiki/Air_mass

    Different air masses which affect North America as well as other continents, tend to be separated by frontal boundaries. In meteorology, an air mass is a volume of air defined by its temperature and humidity. Air masses cover many hundreds or thousands of square miles, and adapt to the

  4. Humid climate - Wikipedia

    en.wikipedia.org/wiki/Humid_climate

    Humid climate is a climate with an excess of moisture. In the Köppen climate classification system, it is marked with middle letter f, standing for the German word for humid, feucht, unofficially translated to English as f ully humid, though humid subtropical climates bordering tropical monsoon or tropical wet and dry climates have a dry season.

  5. Humid subtropical climate - Wikipedia

    en.wikipedia.org/wiki/Humid_subtropical_climate

    A humid subtropical climate is a subtropical-temperate climate type, characterized by long and hot summers, and cool to mild winters. These climates normally lie on the southeast side of all continents (except Antarctica), generally between latitudes 25° and 40° and are located poleward from adjacent tropical climates, and equatorward from either humid continental (in North America and Asia ...

  6. Humid continental climate - Wikipedia

    en.wikipedia.org/wiki/Humid_continental_climate

    A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, [1] typified by four distinct seasons and large seasonal temperature differences, with warm to hot (and often humid) summers, and cold (sometimes severely cold in the northern areas) and snowy winters. Precipitation is usually ...

  7. Continental climate - Wikipedia

    en.wikipedia.org/wiki/Continental_climate

    Dwa = Monsoon-influenced hot-summer humid continental climate; coldest month averaging below 0 °C (32 °F) (or −3 °C (27 °F)), at least one month's average temperature above 22 °C (71.6 °F), and at least four months averaging above 10 °C (50 °F). At least ten times as much rain in the wettest month of summer as in the driest month of ...

  8. This is why a humid day feels so hot - AOL

    www.aol.com/news/2017-07-12-this-is-why-a-humid...

    But humid air is already chock-full of water so your sweat doesn't really have anywhere to go. Evaporation slows down and all that heat stays stuck to you, so you start cooking.

  9. Köppen climate classification - Wikipedia

    en.wikipedia.org/wiki/Köppen_climate_classification

    Cwa = Monsoon-influenced humid subtropical climate; coldest month averaging above 0 °C (32 °F) (or −3 °C (26.6 °F)), at least one month's average temperature above 22 °C (71.6 °F), and at least four months averaging above 10 °C (50 °F). At least ten times as much rain in the wettest month of summer as in the driest month of winter.