Explanation:
Tropical desert climates (Köppen BWh) are characterized by very low rainfall (less than 250 mm per year) and high temperatures, with large diurnal temperature ranges.
Explanation:
The polar jet stream forms due to the strong temperature contrast between polar air and tropical air, creating a steep pressure gradient and strong winds, which are then deflected by the Coriolis force.
Explanation:
The ITCZ is also known as the doldrums because the converging winds create calm conditions with little to no wind, historically making it difficult for sailing ships.
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