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  2. Lake-effect snow - Wikipedia

    en.wikipedia.org/wiki/Lake-effect_snow

    A cold northwesterly to westerly wind over all the Great Lakes created the lake-effect snowfall of January 10, 2022. Lake-effect snow is produced during cooler atmospheric conditions when a cold air mass moves across long expanses of warmer lake water. The lower layer of air, heated by the lake water, picks up water vapor from the lake and ...

  3. Bora (wind) - Wikipedia

    en.wikipedia.org/wiki/Bora_(wind)

    Bora seen from an aircraft near Novalja, Croatia (sea with white stripes) Senj during the 2012 European cold wave The bora on the Karst Plateau, depicted in Valvasor's The Glory of the Duchy of Carniola, 17th century. The area where some of the strongest bora winds occur is the Velebit mountain range in Croatia.

  4. Tree line - Wikipedia

    en.wikipedia.org/wiki/Tree_line

    At 71°N, near the coast, the tree-line is below sea level (Arctic tree line). Abisko, Sweden 68°N 650 2,100 Chugach Mountains, Alaska: 61°N 700 2,300 Tree line around 1,500 feet (460 m) or lower in coastal areas Southern Norway 61°N 1,100 3,600 Much lower near the coast, down to 500–600 metres (1,600–2,000 ft). Scotland, United Kingdom

  5. Prevailing winds - Wikipedia

    en.wikipedia.org/wiki/Prevailing_winds

    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 with the highest speed over a particular point on the Earth's surface at any given time. A region's prevailing and dominant winds are the result of ...

  6. Chinook wind - Wikipedia

    en.wikipedia.org/wiki/Chinook_wind

    The reference to "a Chinook" wind or weather system originally meant, to euro-American settlers along the Pacific Northwest coast, a warming wind from the ocean blowing into the interior regions of the Pacific Northwest of the North America. A strong föhn wind can make snow one foot (30 cm) deep almost vanish in one day. [6]

  7. North Atlantic oscillation - Wikipedia

    en.wikipedia.org/wiki/North_Atlantic_oscillation

    The North Atlantic Oscillation ( NAO) is a weather phenomenon over the North Atlantic Ocean of fluctuations in the difference of atmospheric pressure at sea level (SLP) between the Icelandic Low and the Azores High. Through fluctuations in the strength of the Icelandic Low and the Azores High, it controls the strength and direction of westerly ...

  8. Geography of Europe - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Europe

    Topography of Europe. Some geographical texts refer to a Eurasian continent given that Europe is not surrounded by sea and its southeastern border has always been variously defined for centuries. In terms of shape, Europe is a collection of connected peninsulas and nearby islands. The two largest peninsulas are Europe itself and Scandinavia to ...

  9. 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 / ɪtʃ / 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. It encircles Earth near the ...