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  2. Westerlies - Wikipedia

    en.wikipedia.org/wiki/Westerlies

    The strongest westerly winds in the middle latitudes can come in the roaring forties, between 40 and 50 degrees south latitude. The westerlies play an important role in carrying the warm, equatorial waters and winds to the western coasts of continents, especially in the southern hemisphere because of its vast oceanic expanse.

  3. Antarctic oscillation - Wikipedia

    en.wikipedia.org/wiki/Antarctic_oscillation

    The Southern Annular Mode is usually defined as the difference in the zonal mean sea level pressure at 40°S (mid-latitudes) and 65°S (Antarctica). [1]The Antarctic oscillation (AAO, to distinguish it from the Arctic oscillation or AO), also known as the Southern Annular Mode (SAM), is a low-frequency mode of atmospheric variability of the southern hemisphere that is defined as a belt of ...

  4. Southeast Australian foehn - Wikipedia

    en.wikipedia.org/wiki/Southeast_Australian_foehn

    Foehn winds usually occur when the westerly wind belt moves northwards. [7]The foehn effect on the coastal plains of southeastern Australia is mostly linked with the passage of a deep low pressure system or westerly cold fronts across the Great Australian Bight and southeastern Australia that cause strong winds to reorient virtually perpendicular to some parts of the Great Dividing Range ...

  5. Quasi-biennial oscillation - Wikipedia

    en.wikipedia.org/wiki/Quasi-biennial_oscillation

    The quasi-biennial oscillation (QBO) is a quasiperiodic oscillation of the equatorial zonal wind between easterlies and westerlies in the tropical stratosphere with a mean period of 28 to 29 months. The alternating wind regimes develop at the top of the lower stratosphere and propagate downwards at about 1 km (0.6 mi) per month until they are ...

  6. North Pacific Gyre - Wikipedia

    en.wikipedia.org/wiki/North_Pacific_Gyre

    This two-gyre circulation in the North Pacific is driven by the trade and westerly winds. [2] This is one of the best examples of all of Earth's oceans where these winds drive a two-gyre circulation. Physical characteristics like weak thermohaline circulation in the North Pacific and the fact that it is mostly blocked by land in the north, also ...

  7. Windbelt - Wikipedia

    en.wikipedia.org/wiki/Windbelt

    The inventor's claims that the device is 10–30 times more efficient than small wind turbines have been refuted by tests. [2] The microWindbelt could generate 0.2 mW at a wind speed of 3.5 m/s and 5 mW at 7.5 m/s, which represent efficiencies (ηC p) of 0.21 and 0.53 respectively. Wind turbines typically have efficiencies of 1% to 10%.

  8. North Atlantic oscillation - Wikipedia

    en.wikipedia.org/wiki/North_Atlantic_oscillation

    Westerly winds blowing across the Atlantic bring moist air into Europe. In years when westerlies are strong, summers are cool, winters are mild and rain is frequent. If westerlies are suppressed, the temperature is more extreme in summer and winter leading to heat waves , deep freezes and reduced rainfall.

  9. Westerly wind burst - Wikipedia

    en.wikipedia.org/wiki/Westerly_wind_burst

    A westerly wind burst is defined by Harrison and Vecchi (1997) as sustained winds of 25 km/h (16 mph) over a period of 5–20 days. [3] However, no concrete definition has been determined, with Tziperman and Yu (2007) defining them as having winds of 14 km/h (8.7 mph) and lasting "at least a few days".