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55 Chapter2 Impact of Technologiesfrom Two World Wars Edward N. Rappaportand Robert H. Simpson INTRODUCTION For nearlyhalf a centuryafter the Galvestondisasterof 1900, the struggleto learn how to cope with hurricaneswas slow and painful. The net resultwill be seenin later chaptersdescribingthe science-drivenaccelerationof progressduringthe last half century. 1029/055SP03 39 Special Publications Vol. 55 40 Impact of Technologiesfrom Two World Wars expansionand supremacyin the New World, includingFlorida'searly political fate eventsdescribedin more detail by Rappaportand Fernandez-Partagas [ 1997].

55 Gray 25 6. Besidesthesethermodynamicrequirements,Riehl and Schafer [1944] and Gray [1968, 1979] verified that TC formationrequiredCb convection to occur and be centered in areas of low shear of the horizontal wind throughthe depthof the troposphere. , conditionallyunstable lapseratesand vertical shear)plus the needfor low-level rotationlead to an understanding asto why hurricaneformationis limited to the locations and seasons where these factors co-exist. 7. This condition was fundamentalfor interpretingand explainingthe concentrationof strongwinds near the hurricane'scenter.

Besidesthesethermodynamicrequirements,Riehl and Schafer [1944] and Gray [1968, 1979] verified that TC formationrequiredCb convection to occur and be centered in areas of low shear of the horizontal wind throughthe depthof the troposphere. , conditionallyunstable lapseratesand vertical shear)plus the needfor low-level rotationlead to an understanding asto why hurricaneformationis limited to the locations and seasons where these factors co-exist. 7. This condition was fundamentalfor interpretingand explainingthe concentrationof strongwinds near the hurricane'scenter.

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