The global atmospheric circulation carries the an gular momentum to higher latitudes where it is put back into the continents and oceans the tropics is home to some circulation phenomena that do not occur in higher latitudes most famously tropical cyclones produce tremendous amounts of rainfall and strong winds. Despite major advances in the observation and numerical simulation of the atmosphere basic features of the earths climate remain poorly understood integrating the available data and computational resources to improve our understanding of the global circulation of the atmosphere remains a challenge theory must play a critical role in meeting this challenge. Buy the global circulation of the atmosphere 9780691121819 nhbs edited by tapio schneider and adam h sobel princeton university press. Global atmospheric circulation polar ferrel and hadley cells the movement of air across the planet occurs in a specific pattern the whole system is driven by the equator which is the hottest
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