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Figure 2.14: Schematic of the surface temperature and wind fields associated with a tropical cyclone (top) and an autumn marine extratropical cyclone, such as might result from an extratropical transformation of the tropical cyclone (bottom), adapted from Mook (1955). The structure of the extratropical cyclone and the sizes of both cyclone types can vary considerably from this example.

fig2_14a.gif (121918 bytes)

fig2_14b.gif (121918 bytes)


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