Download Hurricane! Coping with Disaster: Progress and Challenges by Robert Simpson, Richard Anthes, Michael Garstan, Joanne PDF

By Robert Simpson, Richard Anthes, Michael Garstan, Joanne Simpson

Published through the yankee Geophysical Union as a part of the Special courses Series.

Hurricane examine implicates anything greater than technological know-how. it's the key to saving lives and mitigating financial harm. From the Galveston disaster of 1900, the place greater than 8,000 humans died, to the industrial devastation wrought via storm Andrew in 1992 within the usa, scientists have striven to appreciate and music hurricanes whereas charting their societal results. storm! dealing with catastrophe tells the dramatic historical past of that attempt by way of top meteorologists?the women and men who introduced typhoon technological know-how into the twenty first century, and those that maintain it at the present time. for readers in all places drawn to climatology, storm examine, the ancient history, and more.Content:
Chapter 1 20th Century demanding situations and Milestones (pages 3–37): William M. Gray
Chapter 2 influence of applied sciences from global Wars (pages 39–61): Edward N. Rappaport and Robert H. Simpson
Chapter three storm Surveillance through especially Instrumented airplane (pages 63–101): Robert C. Sheets
Chapter four Evolution of Prediction types (pages 103–126): Mark DeMaria and James M. Gross
Chapter five the good Galveston storm of 1900 (pages 128–140): Neil L. Frank
Chapter 6 Social selection in facing Hurricanes (pages 141–153): Mary Frances Myers and Gilbert F. White
Chapter 7 speaking harm Potentials and Minimizing typhoon harm (pages 155–164): Herbert S. Saffir
Chapter eight decreasing Vulnerability (pages 165–173): Roger A. Pielke
Chapter nine A Century of clinical growth: An overview (pages 177–204): Kerry Emanuel
Chapter 10 A Century of development in monitoring and caution: advancements in Observations, types, and Forecasts (pages 205–216): H.E. Willoughby
Chapter eleven The Burgeoning position of climate Satellites (pages 217–247): C. Velden, J. Simpson, W. Timothy Liu, J. Hawkins, ok. Brueske and R. Athens
Chapter 12 contemporary satellite tv for pc know-how for storm study: a better examine Formation and Intensification (pages 249–289): E.A. Ritchie, J. Simpson, W.T. Liu, J. Halverson, C.S. Velden, K.F. Brueske and H. Pierce
Chapter thirteen non-stop tracking of the typhoon middle: Availability of recent Long?Endurance Small Drone plane (pages 291–304): Greg Tyrrell and Greg Holland
Chapter 14 typhoon top point Wind Measurements: functions of Doppler Lidar (pages 305–315): G. David Emmitt
Chapter 15 A Century After Galveston, 1900: a private viewpoint and Outlook (pages 317–334): Greg Holland

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Extra info for Hurricane! Coping with Disaster: Progress and Challenges Since Galveston, 1900

Example text

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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