This nonfiction collection examines the five persistent oceanic high-pressure belts and how wind, temperature differences, and the rotation of the Earth interact to create lasting patterns. It presents historical hypotheses and modern reasoning, weighing the ideas of Ferrel and Angot against observed data to explain why these highs stay put and how they affect nearby continents.

The text blends theory with data, offering a clear look at how convection, temperature gradients, and planetary rotation combine to drive large-scale atmospheric motion. You’ll see step-by-step reasoning about why surface and upper-level winds behave as they do, and how these forces contribute to the climate influence of the world’s major oceans.

Understand why certain latitudes foster permanent high-pressure belts
Learn how temperature gradients and rotation shape atmospheric circulation
See how competing hypotheses account for oceanic highs and their continental effects
Get a grounded view of the reasoning behind early meteorological theories

Ideal for readers of historical meteorology and science history, this edition helps map the roots of ongoing climate science and weather prediction.

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