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  2. Tropical rain belt - Wikipedia

    en.wikipedia.org/wiki/Tropical_rain_belt

    The reason the rain belt is situated near the tropics can be attributed to the fact that the Sun's radiation is strongest near the equator, which is located in the middle of the tropics. This solar radiation generates large amounts of heat near the equator. [1] [2] This causes the air at ground level in the tropics to warm up.

  3. Tropical cyclogenesis - Wikipedia

    en.wikipedia.org/wiki/Tropical_cyclogenesis

    In areas with a very small or non-existent Coriolis force (e.g. near the Equator), the only significant atmospheric forces in play are the pressure gradient force (the pressure difference that causes winds to blow from high to low pressure [15]) and a smaller friction force; these two alone would not cause the large-scale rotation required for ...

  4. 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.

  5. Geology of Afghanistan - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Afghanistan

    Afghanistan has numerous Permian rocks. In the west, south of Herat is a 150-meterr sequence of dolomite and limestone. Permian rocks span the areas between the western Hindu Kush, Kandahar, Gardez, Jalalabad, and Moqor. Carboniferous rocks transition to Permian sandstone and shale in the Dasht-i-Nawar and Logar valley areas.

  6. Atmospheric circulation - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_circulation

    The Hadley cell is a closed circulation loop which begins at the equator. There, moist air is warmed by the Earth's surface, decreases in density and rises. A similar air mass rising on the other side of the equator forces those rising air masses to move poleward. The rising air creates a low pressure zone near the equator.

  7. Tropopause - Wikipedia

    en.wikipedia.org/wiki/Tropopause

    The troposphere is the lowest layer of the Earth's atmosphere; it starts at the planetary boundary layer, and is the layer in which most weather phenomena occur. The troposphere contains the boundary layer, and ranges in height from an average of 9 km (5.6 mi; 30,000 ft) at the poles, to 17 km (11 mi; 56,000 ft) at the Equator.

  8. Why Pakistan-Afghanistan Tensions Are Soaring - AOL

    www.aol.com/news/why-pakistan-afghanistan...

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  9. Geographical zone - Wikipedia

    en.wikipedia.org/wiki/Geographical_zone

    Both philosophers theorized the Earth divided into three types of climatic zones based on their distance from the equator. Like Parmeneides, thinking that the area near the equator was too hot for habitation, Aristotle dubbed the region around the equator (from 23.5° N to 23.5° S) the "Torrid Zone."