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  2. 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.

  3. Cold wave - Wikipedia

    en.wikipedia.org/wiki/Cold_wave

    Winter of 1917–1918 – The winter was very frigid across the East and created a heating fuel crisis equaled only in January 1977. Severe cold wave in December 1917 and January 1918 in northeast. December 30 set a number of record lows at the time in New York City (−13 °F, −25 °C) and Boston (−15 °F, −26 °C). [20]

  4. El Niño–Southern Oscillation - Wikipedia

    en.wikipedia.org/wiki/El_Niño–Southern...

    This process cools the East Pacific because the thermocline is closer to the ocean surface, leaving relatively little separation between the deeper cold water and the ocean surface. [24] Additionally, the northward-flowing Humboldt Current carries colder water from the Southern Ocean to the tropics in the East Pacific . [ 22 ]

  5. Atmospheric circulation - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_circulation

    The Pacific Ocean cell plays a particularly important role in Earth's weather. This entirely ocean-based cell comes about as the result of a marked difference in the surface temperatures of the western and eastern Pacific. Under ordinary circumstances, the western Pacific waters are warm, and the eastern waters are cool.

  6. Polar climate - Wikipedia

    en.wikipedia.org/wiki/Polar_climate

    As such, the climate of much of the Arctic is moderated by the ocean water, which can never have a temperature below −2 °C (28 °F). In winter, this relatively warm water, even though covered by the polar ice pack , keeps the North Pole from being the coldest place in the Northern Hemisphere , and it is also part of the reason that ...

  7. Atmospheric tide - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_tide

    Figure 2. Eigenvalue ε of wave modes of zonal wave number s = 1 vs. normalized frequency ν = ω/Ω where Ω = 7.27 × 10 −5 s −1 is the angular frequency of one solar day. Waves with positive (negative) frequencies propagate to the east (west). The horizontal dashed line is at ε c ≃ 11 and indicates the transition from internal to ...

  8. I've been to over 50 countries. Here are my 4 favorite ... - AOL

    www.aol.com/ive-over-50-countries-4-142701216.html

    After visiting over 50 countries, I've learned which spots are great for escaping the cold winter. The Gold Coast in Queensland, Australia, is a great sunny spot for outdoor activities.

  9. Glossary of meteorology - Wikipedia

    en.wikipedia.org/wiki/Glossary_of_meteorology

    In surface weather analysis, cold fronts are symbolized by a blue line with triangles pointing in the direction of travel. cold wave. Also cold spell and cold snap. A period of weather characterized by excessively low temperatures, which may or may not also be accompanied by changes in humidity. Very cold weather is often only referred to as a ...