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Atmospheric Circulation and Weather Systems
Atmospheric circulation refers to the large-scale movement of air across the Earth, driven primarily by the uneven heating of the planet’s surface by the Sun. This circulation redistributes heat and moisture, creating distinct wind patterns such as the trade winds, westerlies, and polar easterlies. These global wind belts interact with pressure systems—like high-pressure zones that bring clear skies and low-pressure zones that trigger storms—to shape weather conditions. Weather systems, including cyclones, anticyclones, and monsoons, emerge from these interactions, influencing rainfall, temperature, and storm activity across regions. Together, atmospheric circulation and weather systems form the backbone of Earth’s climate dynamics, explaining why certain areas experience deserts, rainforests, or seasonal shifts.
This lecture is part of GEO 202 INTRODUCTORY CLIMATOLOGY AND BIOGEOGRAPHY in the Geology department. The course has 30 recorded lectures across 10 series, all free to watch. Read or download the GEO 202 lecture note to study alongside the video.