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  2. Middle latitudes - Wikipedia

    en.wikipedia.org/wiki/Middle_latitudes

    World map with the middle latitudes highlighted in red Extratropical cyclone formation areas. The middle latitudes (also called the mid-latitudes, sometimes midlatitudes, or moderate latitudes) are a spatial region on Earth located between the Tropic of Cancer (latitudes 23°26′09.9″) to the Arctic Circle (66°33′50.1″), and Tropic of Capricorn (-23°26′09.9″) to the Antarctic ...

  3. Extratropical cyclone - Wikipedia

    en.wikipedia.org/wiki/Extratropical_cyclone

    They are termed mid-latitude cyclones if they form within those latitudes, or post-tropical cyclones if a tropical cyclone has intruded into the mid latitudes. [1] [2] Weather forecasters and the general public often describe them simply as "depressions" or "lows". Terms like frontal cyclone, frontal depression, frontal low, extratropical low ...

  4. Westerlies - Wikipedia

    en.wikipedia.org/wiki/Westerlies

    The westerlies, anti-trades, [2] or prevailing westerlies, are prevailing winds from the west toward the east in the middle latitudes between 30 and 60 degrees latitude. They originate from the high-pressure areas in the horse latitudes and trend towards the poles and steer extratropical cyclones in this general manner. [3]

  5. Temperate climate - Wikipedia

    en.wikipedia.org/wiki/Temperate_climate

    Precipitation. Topics. Glossaries. Weather portal. v. t. e. In geography, the temperate climates of Earth occur in the middle latitudes (approximately 23.5° to 66.5° N/S of Equator), which span between the tropics and the polar regions of Earth. [1] These zones generally have wider temperature ranges throughout the year and more distinct ...

  6. Cyclogenesis - Wikipedia

    en.wikipedia.org/wiki/Cyclogenesis

    Cyclogenesis is an umbrella term for at least three different processes, all of which result in the development of some sort of cyclone, and at any size from the microscale to the synoptic scale. Tropical cyclones form due to latent heat driven by significant thunderstorm activity, developing a warm core.

  7. Baroclinity - Wikipedia

    en.wikipedia.org/wiki/Baroclinity

    A rotating tank experiment modelling baroclinic eddies in the atmosphere. In fluid dynamics, the baroclinity (often called baroclinicity) of a stratified fluid is a measure of how misaligned the gradient of pressure is from the gradient of density in a fluid. [1][2] In meteorology a baroclinic flow is one in which the density depends on both ...

  8. Continental climate - Wikipedia

    en.wikipedia.org/wiki/Continental_climate

    Continental climate has at least one month averaging below 0 °C (32 °F) and at least one month averaging above 10 °C (50 °F). [4][5] Regions where the continental climates (Dfa, Dfb, Dfc, Dfd) are found. Dfa = Hot-summer humid continental climate; coldest month averaging below 0 °C (32 °F) (or −3 °C (27 °F)), at least one month's ...

  9. Mediterranean climate - Wikipedia

    en.wikipedia.org/wiki/Mediterranean_climate

    Mediterranean climate. A Mediterranean climate (/ ˌmɛdɪtəˈreɪniən / MED-ih-tə-RAY-nee-ən), also called a dry summer climate, described by Köppen as Cs, is a temperate climate type that occurs in the lower mid-latitudes (normally 30 to 44 north and south latitude). Such climates typically have dry summers and wet winters, with summer ...

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