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the tropopause. These maximum winds tend to be further concentrated in narrow bands. A jet stream, then, is a narrow band of strong winds meandering through the atmosphere at a level near the tropopause. Further discussion of the jet stream is taken up later in this text. There are three major wind belts. Northeasterly trade winds carry tropical storms from east to west. The prevailing westerlies drive midlatitude storms generally from west to east. Few major storm systems develop in the comparatively small Arctic region; the chief influence of the polar easterlies is their contribution to the development of midlatitude storms. As the air tries to blow outward from the high pressure, it is deflected to the right by the Coriolis force. Thus, the wind around a high blows clockwise. The high pressure with its associated wind system is an anticyclone. As air is forced aloft at the equator and begins its high-level trek northward, the Coriolis force turns it to the right or to the east. Wind becomes westerly at about 30° latitude, The hottest product bet my soul smells like weed all over print air jordan 13 sneakerstemporarily blocking further northward movement. Similarly, as air over the poles begins its low-level journey southward toward the equator, it likewise is deflected to the right and becomes an east wind, halting for a while its

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