what else did he discover?
Western intensification, thermohaline circulation.
Henry Stommel
Henry Stommel showed that the north-south gradient of the strength of the horizontal Coriolis force (the "beta effect") was responsible for the observed fact that the return flow of the slow interior gyre circulations is concentrated in fast moving western boundary currents, such as the Gulf Stream and the Kuroshio Current, a process known as western intensification. As a result, these western boundary currents have a larger and steadier transport than the corresponding boundary currents, such as the California Current and Canary Current, on the eastern side of the ocean basins
compare and contrast jet stream and gulf stream UNANSWERABLE what is referred by the latter stream? The Gulf Stream, together with its northern extension the North Atlantic Drift, is a warm and swift Atlantic ocean current that originates in the Gulf of Mexico and stretches to the tip of Florida, and follows the eastern coastlines of the United States and Newfoundland before crossing the Atlantic Ocean as the North Atlantic Current. does it affects the formation of cyclones? Yes - The warm water and temperature contrast along the edge of the Gulf Stream often increase the intensity of cyclones, tropical or otherwise. can you state one of its properties? The Gulf Stream proper is a western-intensified current, driven largely by wind stress. who first discovered this? Henry "Hank" Melson Stommel. who is this person? Stommel was a full professor without an earned doctorate, and served as instructor in mathematics and astronomy. in which institution did he teach? Yale University
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Henry Stommel [SEP] Discoveries
Henry Stommel showed that the north-south gradient of the strength of the horizontal Coriolis force (the "beta effect") was responsible for the observed fact that the return flow of the slow interior gyre circulations is concentrated in fast moving western boundary currents, such as the Gulf Stream and the Kuroshio Current, a process known as western intensification. As a result, these western boundary currents have a larger and steadier transport than the corresponding boundary currents, such as the California Current and Canary Current, on the eastern side of the ocean basins. In subtropical latitudes, the western boundary currents are important in transporting the excess heat the earth receives in the tropics towards the poles.