George Dyson's Turing's Cathedral describes how a "two and two-thirds dimensional model" but not a "two and a half dimensional model" was able to catch this process by using data from Thanksgiving Day 1950.
George Dyson's Turing's Cathedral describes how a "two and two-thirds dimensional model" but not a "two and a half dimensional model" was able to catch this process by using data from Thanksgiving Day 1950. Reginald Sutcliffe and Sverre Petterssen found that this process occurs through a "bootstrapping" procedure that was eventually termed "self-development". The formation of the most damaging localized surface winds, which is called a "sting", is ascribed to the formation of a "back-bent" structure in the Shapiro-Keyser model of this process. In Jule Charney's treatment, the formation of a large enough temperature gradient drives the spontaneous production of the Rossby Waves that then undergo this process. One of the oldest treatments of this process was proposed by the Bergen School of meteorologists; that treatment holds that this process involves the development of a structure in a barotropically cold environment. During this process, a cold front overtakes a warm front to create an occluded front. For 10 points, name this process of creating of circular storms.
George Dyson's Turing's Cathedral describes how a "two and two-thirds dimensional model" but not a "two and a half dimensional model" was able to catch this process by using data from Thanksgiving Day 1950.
cyclogenesis [or cyclone formation; accept equivalents]