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  2. 35 of the very best outdoorsy gifts for hikers, hunters and ...

    www.aol.com/lifestyle/best-outdoorsy-gifts-for...

    Titan by Arctic Zone. ... Keep food fresh and drinks cold on the road with this zipperless hard-body cooler. It's designed with multiple layers of leakproof lining and insulation that'll keep ice ...

  3. 31 of the best gifts for people who drive a lot - AOL

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    Titan by Arctic Zone. ... Keep food fresh and drinks cold on the road with this zipperless hard-body cooler. It's designed with multiple layers of leakproof lining and insulation that'll keep ice ...

  4. Climate of the Arctic - Wikipedia

    en.wikipedia.org/wiki/Climate_of_the_Arctic

    Monthly precipitation totals over most of the Arctic Basin average about 15 mm (0.59 in) from November through May, and rise to 20 to 30 mm (0.79 to 1.18 in) in July, August, and September. [6] The dry winters result from the low frequency of cyclones in the region during that time, and the region's distance from warm open water that could ...

  5. Polar climate - Wikipedia

    en.wikipedia.org/wiki/Polar_climate

    Some parts of the Arctic are covered by ice (sea ice, glacial ice, or snow) year-round, especially at the most poleward parts; and nearly all parts of the Arctic experience long periods with some form of ice or snow on the surface. Average January temperatures range from about −40 to 0 °C (−40 to 32 °F), and winter temperatures can drop ...

  6. Altitudinal zonation - Wikipedia

    en.wikipedia.org/wiki/Altitudinal_zonation

    Heating of solids, sunlight and shade in different altitudinal zones (Northern hemisphere) [5] A variety of environmental factors determines the boundaries of altitudinal zones found on mountains, ranging from direct effects of temperature and precipitation to indirect characteristics of the mountain itself, as well as biological interactions of the species.

  7. High-pressure area - Wikipedia

    en.wikipedia.org/wiki/High-pressure_area

    The horse latitudes, or torrid zone, [20] is roughly at the 30th parallel and is the source of warm high pressure systems. As the hot air closer to the equator rises, it cools, losing moisture; it is then transported poleward where it descends, creating the high-pressure area. [ 21 ]

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