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  2. Trade winds - Wikipedia

    en.wikipedia.org/wiki/Trade_winds

    The term originally derives from the early fourteenth century sense of trade (in late Middle English) still often meaning "path" or "track". [2] The Portuguese recognized the importance of the trade winds (then the volta do mar, meaning in Portuguese "turn of the sea" but also "return from the sea") in navigation in both the north and south Atlantic Ocean as early as the 15th century. [3]

  3. North Atlantic oscillation - Wikipedia

    en.wikipedia.org/wiki/North_Atlantic_oscillation

    Through fluctuations in the strength of the Icelandic Low and the Azores High, it controls the strength and direction of westerly winds and location of storm tracks across the North Atlantic. [ 1 ] The NAO was discovered through several studies in the late 19th and early 20th centuries. [ 2 ]

  4. Prevailing winds - Wikipedia

    en.wikipedia.org/wiki/Prevailing_winds

    Prevailing winds are strongly influenced by Earth's overall atmospheric circulation, in addition to smaller-scale and shorter-lived weather phenomena. In meteorology, prevailing wind in a region of the Earth's surface is a surface wind that blows predominantly from a particular direction. The dominant winds are the trends in direction of wind ...

  5. North Atlantic Current - Wikipedia

    en.wikipedia.org/wiki/North_Atlantic_Current

    The North Atlantic Current, together with the Gulf Stream, have a long-lived reputation for having a considerable warming influence on European climate. However, the principal cause for differences in winter climate between North America and Europe seems to be winds rather than ocean currents (although the currents do exert influence at very ...

  6. Atlantic meridional overturning circulation - Wikipedia

    en.wikipedia.org/wiki/Atlantic_meridional...

    AMOC in relation to the global thermohaline circulation . The Atlantic meridional overturning circulation (AMOC) is the main current system in the Atlantic Ocean, [1]: 2238 and is also part of the global thermohaline circulation, which connects the world's oceans with a single "conveyor belt" of continuous water exchange. [18]

  7. Intertropical Convergence Zone - Wikipedia

    en.wikipedia.org/wiki/Intertropical_Convergence_Zone

    The ITCZ is visible as a band of clouds encircling Earth near the Equator. The Intertropical Convergence Zone (ITCZ / ɪ tʃ / ITCH, or ICZ), [1] known by sailors as the doldrums [2] or the calms because of its monotonous windless weather, is the area where the northeast and the southeast trade winds converge.

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    Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!

  9. Winds in the Age of Sail - Wikipedia

    en.wikipedia.org/wiki/Winds_in_the_Age_of_Sail

    North Atlantic: Anyone sailing west from Europe is sailing into the wind. Further north, they are sailing against the Gulf Stream. It is not clear how winds and currents were used in this region. [5] Caribbean: Columbus underestimated the size of the Earth and thought he could reach China by doing a grand volta do mar, going west on the trade ...