enow.com Web Search

Search results

  1. Results from the WOW.Com Content Network
  2. Anabatic wind - Wikipedia

    en.wikipedia.org/wiki/Anabatic_wind

    An anabatic wind, from the Greek anabatos, verbal of anabainein meaning "moving upward", is a warm wind which blows up a steep slope or mountain side, driven by heating of the slope through insolation. [1] [2] It is also known as upslope flow. These winds typically occur during the daytime in calm sunny weather.

  3. Mountain breeze and valley breeze - Wikipedia

    en.wikipedia.org/wiki/Mountain_breeze_and_valley...

    Diurnal wind system variation in the Appalachian mountain range. Mountain and valley breezes form through a process similar to sea and land breezes. During the day, the sun heats up mountain air rapidly while the valley remains relatively cooler. Convection causes it to rise, causing a valley breeze. At night, the process is reversed.

  4. List of local winds - Wikipedia

    en.wikipedia.org/wiki/List_of_local_winds

    Buran (a wind which blows across eastern Asia. It is also known as Purga when over the tundra); Karakaze (strong cold mountain wind from Gunma Prefecture in Japan); East Asian Monsoon, known in China and Taiwan as meiyu (梅雨), in Korea as jangma (), and in Japan as tsuyu (梅雨) when advancing northwards in the spring and shurin (秋霖) when retreating southwards in autumn.

  5. Alpine storms - Wikipedia

    en.wikipedia.org/wiki/Alpine_storms

    In a more general case, several effects may be present and if the synoptic wind is opposed to the anabatic wind, additional convergence occurs at the top of the mountain. [3] It is also possible to create a convergence zone behind the mountain when the synoptic wind can divide and go around it to meet again (ex. Puget Sound Convergence Zone ...

  6. Foehn wind - Wikipedia

    en.wikipedia.org/wiki/Foehn_wind

    The causes of the Foehn effect in the lee of mountains (adapted from: [1]) Dissolving Föhn clouds over Cumbre Nueva, La Palma, at an elevation of 1,400 m (4,600 ft) A Foehn, or Föhn (UK: / f ɜː n /, US: / f eɪ n / fayn, [2] [3] US also / f ʌ n, f ɜːr n / fu(r)n [4] [5]), is a type of dry, relatively warm downslope wind in the lee of a mountain range.

  7. Santa Ana winds: facts and fiction - AOL

    www.aol.com/weather/santa-ana-winds-facts...

    The Santa Ana winds of Southern California can be visualized in several ways. You can see their effects as palm trees sway in the morning light or when clean-up crews arrive to deal with branches ...

  8. What Is Wind Chill And What Makes It So Dangerous? - AOL

    www.aol.com/news/wind-chill-makes-dangerous...

    Wind chill is important for more than just determining how cold – or, if you hate the cold, miserable – it is outside. Wind chill helps us determine the level of threat from hypothermia and ...

  9. List of severe weather phenomena - Wikipedia

    en.wikipedia.org/wiki/List_of_severe_weather...

    Cyclones. Extratropical cyclone. European windstorms; Australian East Coast Low "Medicane", Mediterranean tropical-like cyclones Polar cyclone; Tropical cyclone, also called a hurricane, typhoon, or just "cyclone"

  1. Related searches is anabatic wind dangerous for you essay writing service canada site search

    what is anabatic windgreek anabatic wind
    anabatic wind wikipediaharmattan wind gusts