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  2. Trough (meteorology) - Wikipedia

    en.wikipedia.org/wiki/Trough_(meteorology)

    A lee trough, also known as a dynamic trough, is "A pressure trough formed on the lee side of a mountain range in situations where the wind is blowing with a substantial component across the mountain ridge; often seen on United States weather maps east of the Rocky Mountains, and sometimes east of the Appalachians, where it is less pronounced."

  3. Ridge (meteorology) - Wikipedia

    en.wikipedia.org/wiki/Ridge_(meteorology)

    Ridge line extending to the left of the high pressure center (H). In meteorology a ridge or barometric ridge is an elongated area of relatively high atmospheric pressure compared to the surrounding environment, without being a closed circulation. [1] It is associated with an area of maximum anticyclonic curvature of wind flow.

  4. Col (meteorology) - Wikipedia

    en.wikipedia.org/wiki/Col_(meteorology)

    A col, also called saddle point or neutral point, is in meteorology, the point of intersection of a trough and a ridge in the pressure pattern of a weather map. It takes the form of a saddle where the air pressure is relatively higher than that of the low-pressure regions, but lower than that of the anticyclonic zones. [1]

  5. Lau–Colville Ridge - Wikipedia

    en.wikipedia.org/wiki/Lau–Colville_Ridge

    The southern Colville Ridge (also known as Khrebet Kolvil-Lau from Russian Хребет Колвил-Лау [1])forms the western boundary of the Havre Trough. [ 8 ] [ 9 ] The Havre Trough has had rift extension for the last 2 million years between the Australian plate and the Kermadec microplate and this extends into Zealandia 's continental ...

  6. Shortwave (meteorology) - Wikipedia

    en.wikipedia.org/wiki/Shortwave_(meteorology)

    Shortwave trough with associated vorticity. A shortwave or shortwave trough is an embedded kink in the trough / ridge pattern. Its length scale is much smaller than that of and is embedded within longwaves, which are responsible for the largest scale (synoptic scale) weather systems.

  7. Cold-air damming - Wikipedia

    en.wikipedia.org/wiki/Cold-air_damming

    Cold air damming, or CAD, is a meteorological phenomenon that involves a high-pressure system (anticyclone) accelerating equatorward east of a north-south oriented mountain range due to the formation of a barrier jet behind a cold front associated with the poleward portion of a split upper level trough. Initially, a high-pressure system moves ...

  8. Clear-air turbulence - Wikipedia

    en.wikipedia.org/wiki/Clear-air_turbulence

    When the CAT is associated with a sharp trough, the plane must go through the low-pressure region instead of around it. The pilot may issue a Pilot Report (PIREP), communicating position, altitude and severity of the turbulence to warn other aircraft entering the region.

  9. Horsetrough Mountain - Wikipedia

    en.wikipedia.org/wiki/Horsetrough_Mountain

    The Appalachian Trail follows the main ridge line of the mountain but does not cross the summit. Horsetrough Falls is located on the southern side of the mountain.