Hurricane Threat to Florida Climate Change Or Demographics?
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Conference Poster Production
65th Interdepartmental Hurricane Conference Miami, Florida February 28 - March 3, 2011 Hurricane Earl:September 2, 2010 Ocean and Atmospheric Influences on Tropical Cyclone Predictions: Challenges and Recent Progress S E S S Session 2 I The 2010 Tropical Cyclone Season in Review O N 2 The 2010 Atlantic Hurricane Season: Extremely Active but no U.S. Hurricane Landfalls Eric Blake and John L. Beven II ([email protected]) NOAA/NWS/National Hurricane Center The 2010 Atlantic hurricane season was quite active, with 19 named storms, 12 of which became hurricanes and 5 of which reached major hurricane intensity. These totals are well above the long-term normals of about 11 named storms, 6 hurricanes, and 2 major hurricanes. Although the 2010 season was considerably busier than normal, no hurricanes struck the United States. This was the most active season on record in the Atlantic that did not have a U.S. landfalling hurricane, and was also the second year in a row without a hurricane striking the U.S. coastline. A persistent trough along the east coast of the United States steered many of the hurricanes out to sea, while ridging over the central United States kept any hurricanes over the western part of the Caribbean Sea and Gulf of Mexico farther south over Central America and Mexico. The most significant U.S. impacts occurred with Tropical Storm Hermine, which brought hurricane-force wind gusts to south Texas along with extremely heavy rain, six fatalities, and about $240 million dollars of damage. Hurricane Earl was responsible for four deaths along the east coast of the United States due to very large swells, although the center of the hurricane stayed offshore. -
Resilience Potential: Assessing Jamaica's “Bounce-Back” from Hurricane Dean
Resilience Potential: Assessing Jamaica’s “Bounce-Back” from Hurricane Dean CaPRI is a Caribbean think tank that promotes evidence- based policymaking in the region. CaPRI espouses a methodology which is built on the values of multi- disciplinary work, team work and the utilization of the diaspora in our search for evidence. Committed to the region’s development, CaPRI has strong linkages with the academic community, the private sector and civil society. For information and feedback, please contact: Caribbean Policy Research Institute GUANGO TREE HOUSE, 29 MUNROE ROAD, KINGSTON 6 JAMAICA, W.I. TEL: (876) 970-3447 (876) 970-2910 FAX: (876) 970-4544 E-mail: [email protected] WEBSITE: http://www.takingresponsibility.org 2 Table of Contents Pages List of Figures, Tables and Boxes .............................................................4 Preface......................................................................................................5 Executive Summary .................................................................................6-7 Introduction: Resilience Potential ...........................................................8-9 1. Natural Disasters: The Global Context................................................10-13 2. Natural Disasters in the Caribbean .....................................................14-18 3. Changing Practices in Disaster Management…………………………19-20 4. Disaster Management in Jamaica .....................................................21 4.1 National Disaster Plan…………………………………………….21 -
© Mitigation of Cyclonic Activity Lawrence Sirovich, Rockefeller University Abstract Under Realistic Estimates of Geophysical
Management of Cyclonic Activity Lawrence Sirovich, Rockefeller University Abstract Based on realistic estimates of geophysical conditions, we demonstrate that the intensity of a hurricane may be diminished before reaching landfall, and under other circumstances, might be quenched in an incipient stage. It will be shown that with present-day technology, it is possible to mix the cold deep ocean with the warm surface layer sufficiently, and in a timely manner, in order to decrease cyclonic intensity. Two strategies will be presented: (1) In a manner similar to hurricane weakening by landfall, a virtual early landfall is created on the hurricane path, before true landfall; (2) An identified tropical depression might be quenched, by cyclonic or anti- cyclonic means, and timely intervention. Estimates of the power needed to perform the needed ocean mixing, in a timely manner, show that this might be accomplished by employing a sufficient number of high-performance submarines. The achievement of this goal is made possible by an unusually high coefficient of performance, O(10^4). The destructive power of the hurricane is a function of a hurricane’s maximal wind speed, Vm. It will be shown that even a 20% reduction in this wind speed produces a ~50% reduction in destructive costs. On the flip side of these considerations, there is the possibility of using such means, under favorable circumstances, to initiate rainfall for relief of drought areas. Novel vessel modifications are introduced to achieve the mixing process It is the contention of this paper that a practical framework now exists for sensibly exploring means by which to reduce the tragedy and devastation caused by hurricanes. -
1858 San Diego Hurricane and Not Be Sur- Documented to Be Real
THE SAN DIEGO HURRICANE OF 2 OCTOBER 1858 BY MICHAEL CHENOWETH AND CHRISTOPHER LANDSEA The discovery of a hurricane that directly impacted San Diego, California, nearly 150 yr ago has implications for residents and risk managers in their planning for extreme events for the region. ropical cyclones forming in the eastern North 10 September 1976 in California and Arizona, and Pacific Ocean are occasional visitors to the Hurricane Nora in September 1997 in Arizona. Only T southwestern United States. By the time these the 1939 tropical storm made a direct landfall in coastal systems travel far enough to the north to bring their California (Smith 1986), because the other three sys- associated moisture to the United States, the tropical tems entered the United States after first making land- cyclones have normally diminished below tropical fall in Mexico. storm strength over Mexico or over the colder waters The 1939 tropical storm caused $2 million in prop- of the California Current that flows southward along erty damage in California, mostly to shipping, shore the California coast. Rain, sometimes locally excessive, structures, power and communication lines, and crops. is frequently observed in many areas of the southwest- Ships in coastal waters of southern California reported ern United States when tropical cyclone remnants en- southeast winds between 34 and 47 kt (Hurd 1939). ter the region (Blake 1935; Smith 1986). However, no tropical cyclones are recorded or esti- Four tropical cyclones have managed to bring tropi- mated to have made landfall in the southwestern cal storm–force winds to the southwestern United United States as a hurricane, with maximum 1-min States during the twentieth century: a tropical storm surface (10 m) winds of at least 64 kt. -
Geographical and Historical Variation in Hurricanes Across the Yucatán Peninsula
Chapter 27 Geographical and Historical Variation in Hurricanes Across the Yucatán Peninsula Emery R. Boose David R. Foster Audrey Barker Plotkin Brian Hall INTRODUCTION Disturbance is a continual though varying theme in the history of the Yucatán Peninsula. Ancient Maya civilizations cleared and modified much of the forested landscape for millennia, and then abruptly abandoned large areas nearly 1,000 years ago, allowing forests of native species to reestablish and mature (Turner 1974; Hodell, Curtis, and Brenner 1995). More recently, late twentieth century population growth has fueled a resurgence of land-use activity including logging, slash-and-burn agriculture, large mechanized agricultural projects, tourism, and urban expansion (Turner et al. 2001; Turner, Geoghegan, and Foster 2002). Throughout this lengthy history, fires have affected the region—ignited purposefully or accidentally by humans, and occasionally by lightning (Lundell 1940; Snook 1998). And, as indicated by ancient Maya records, historical accounts, and contemporary observations, intense winds associated with hurricanes have repeatedly damaged forests and human settlements (Wilson 1980; Morales 1993). Despite the generally acknowledged importance of natural and human disturbance in the Yucatán Peninsula, there has been little attempt to quantify This research was supported by grants from the National Aeronautics and Space Agency (Land Cover Land-Use Change Program), the National Science Foundation (DEB-9318552, DEB-9411975), and the A. W. Mellon Foundation, and is a contribution from the Harvard Forest Long-Term Ecological Research Program. 495 496 THE LOWLAND MAYA AREA the spatial and temporal distribution of this activity, or to interpret its relationship to modern vegetation patterns (cf. Lundell 1937, 1938; Cairns et al. -
Revista 224.Indd
U CARIBBEAn TROPICAL STORMS Ecological Implications for Pre-Hispanic and Contemporary Maya Subsistence on the Yucatan Peninsula Herman W. Konrad ABSTRACT The ecological stress factor of hurricanes is examined as a dimension of pre-Hispanic Maya adaptation to a tropical forest habitat in the Yucatan peninsula. Pre-Hispanic, colonial and contemporary texts as well as climatic data from the Caribbean region support the thesis that the hurricane was an integral feature of the pre-Hispanic Maya cosmology and ecological paradigm. The author argues that destruction of forests by tropical storms and subsequent succession cycles mimic not only swidden —"slash- and-burn"— agriculture, but also slower, natural succession cycles. With varying degrees of success, flora and fauna adapt to periodic, radical ecosystem disruption in the most frequently hard-hit areas. While not ignoring more widely-discussed issues surrounding the longevity and decline of pre-Hispanic Maya civilization, such as political development, settlement patterns, migration, demographic stability, warfare and trade, the author suggests that effective adaptation to the ecological effects of tropical storms helped determine the success of pre-Hispanic Herman W. Konrad. university Maya subsistence strategies. of Calgary. Email: [email protected] gary.ca NÚMERO 224 • PRIMER TRIMESTRE DE 2003 • 99 Herman W. Konrad RESuMEn Los efectos ecológicos causados por los huracanes se analizan en el contexto de la adaptación de los mayas prehispánicos a la selva de la península de Yucatán. Textos prehispánicos, coloniales y contemporáneos, así como información climática sobre el Caribe en general, apoyan la hipótesis de que el huracán era un elemento central en la cosmovisión y el paradigma ecológico prehispánico. -
ANNUAL SUMMARY Atlantic Hurricane Season of 2005
MARCH 2008 ANNUAL SUMMARY 1109 ANNUAL SUMMARY Atlantic Hurricane Season of 2005 JOHN L. BEVEN II, LIXION A. AVILA,ERIC S. BLAKE,DANIEL P. BROWN,JAMES L. FRANKLIN, RICHARD D. KNABB,RICHARD J. PASCH,JAMIE R. RHOME, AND STACY R. STEWART Tropical Prediction Center, NOAA/NWS/National Hurricane Center, Miami, Florida (Manuscript received 2 November 2006, in final form 30 April 2007) ABSTRACT The 2005 Atlantic hurricane season was the most active of record. Twenty-eight storms occurred, includ- ing 27 tropical storms and one subtropical storm. Fifteen of the storms became hurricanes, and seven of these became major hurricanes. Additionally, there were two tropical depressions and one subtropical depression. Numerous records for single-season activity were set, including most storms, most hurricanes, and highest accumulated cyclone energy index. Five hurricanes and two tropical storms made landfall in the United States, including four major hurricanes. Eight other cyclones made landfall elsewhere in the basin, and five systems that did not make landfall nonetheless impacted land areas. The 2005 storms directly caused nearly 1700 deaths. This includes approximately 1500 in the United States from Hurricane Katrina— the deadliest U.S. hurricane since 1928. The storms also caused well over $100 billion in damages in the United States alone, making 2005 the costliest hurricane season of record. 1. Introduction intervals for all tropical and subtropical cyclones with intensities of 34 kt or greater; Bell et al. 2000), the 2005 By almost all standards of measure, the 2005 Atlantic season had a record value of about 256% of the long- hurricane season was the most active of record. -
Florida Hurricanes and Tropical Storms
FLORIDA HURRICANES AND TROPICAL STORMS 1871-1995: An Historical Survey Fred Doehring, Iver W. Duedall, and John M. Williams '+wcCopy~~ I~BN 0-912747-08-0 Florida SeaGrant College is supported by award of the Office of Sea Grant, NationalOceanic and Atmospheric Administration, U.S. Department of Commerce,grant number NA 36RG-0070, under provisions of the NationalSea Grant College and Programs Act of 1966. This information is published by the Sea Grant Extension Program which functionsas a coinponentof the Florida Cooperative Extension Service, John T. Woeste, Dean, in conducting Cooperative Extensionwork in Agriculture, Home Economics, and Marine Sciences,State of Florida, U.S. Departmentof Agriculture, U.S. Departmentof Commerce, and Boards of County Commissioners, cooperating.Printed and distributed in furtherance af the Actsof Congressof May 8 andJune 14, 1914.The Florida Sea Grant Collegeis an Equal Opportunity-AffirmativeAction employer authorizedto provide research, educational information and other servicesonly to individuals and institutions that function without regardto race,color, sex, age,handicap or nationalorigin. Coverphoto: Hank Brandli & Rob Downey LOANCOPY ONLY Florida Hurricanes and Tropical Storms 1871-1995: An Historical survey Fred Doehring, Iver W. Duedall, and John M. Williams Division of Marine and Environmental Systems, Florida Institute of Technology Melbourne, FL 32901 Technical Paper - 71 June 1994 $5.00 Copies may be obtained from: Florida Sea Grant College Program University of Florida Building 803 P.O. Box 110409 Gainesville, FL 32611-0409 904-392-2801 II Our friend andcolleague, Fred Doehringpictured below, died on January 5, 1993, before this manuscript was completed. Until his death, Fred had spent the last 18 months painstakingly researchingdata for this book. -
Evacuation in Cancun During Hurricane Gilbert*+
International Journalof Mass Emergencies and Disasters March 1991, Vol. 9, NO. 1, pp. 31-45. EVACUATION IN CANCUN DURING HURRICANE GILBERT*+ B. E. Aguirre Department of Sociology Hazard Reduction and Recovery Center Texas A&M University College Station, Texas77843 This paper describes the evacuation of the population of Cancun, Mexico during Hurricane Gilbert, and identifies some of the correlates of their evacuation behavior. The information was collected during a post-disaster visit conducted one week afler impact (September 13, 1988) and as partof a survey a year later of a random sample of 431 persons 18 years old and older who resided in Cancun at the time of the disaster. One-fourth of the respondents evacuated. The majority of the evacuees found shelter in the homes of friends, neighbors, and relatives and were gone from their homes aweek or less. Socio-demographic variables such as thenumber ofpersons in the household gender, age, andmarital status were not very useful predictors of evacuation behavior. Lower socioeco- nomic status (SES) and higher numbers of family contacts did not increase the probability of evacuation. The findings underscore the importance of calculations of rkk for understanding evacuation behavior. The environ- mental context and physical characteristics of residences are significant variables impacting on the perceptions of risk and on subsequent evacu- ation behavior. * This research was supported in part by NSF Grant CES8901262.The author is solely responsible forthe mntentsof this report. The author wishesto express his appreciation to Professor E. L Quarantelli, who offered a number of suggestions to improve the manuscript. I am very grateful to Mr. -
AMS Journals: Unsurpassed Quality, a Lasting Legacy, and Competitive Speed to Publication
LETTER FROM HEADQUARTERS AMS Journals: Unsurpassed Quality, a Lasting Legacy, and Competitive Speed to Publication hile AMS journals have always maintained a that takes the manuscript through editing, typesetting, level of quality that was unsurpassed in the and layout into final form as a high-quality archived W atmospheric and related sciences—by virtu- article in both full-function XML and PDF (plus print ally any measure you might care to focus on—there for those who still receive the journals in this format) was a period when they were less competitive is also occurring in record time—currently on the than some journals in our field when it came to the order of 60 days and improving continually. The level speed of publication. of editorial and produc- As many authors have tion work carried out happily learned in re- on manuscripts ensures cent years, this has not that the resulting article been the reality with is one that authors can AMS journals for some be proud of and one time—but the impres- that reflects well on sion still lingers in some the author when ac- quarters. So forgive cessed by scholars in me if you’ve heard this the future. before, but the steady The AMS journals improvements over re- have a long reputation cent years in the time of publishing seminal to first reviews means works, and the AMS that all the journals imprimatur is synony- making up the AMS mous with quality. AMS suite are now boasting review times in the range of authors do not need to make a choice between speed 50 days on average. -
Mariner's Guide for Hurricane Awareness
Mariner’s Guide For Hurricane Awareness In The North Atlantic Basin Eric J. Holweg [email protected] Meteorologist Tropical Analysis and Forecast Branch Tropical Prediction Center National Weather Service National Oceanic and Atmospheric Administration August 2000 Internet Sites with Weather and Communications Information Of Interest To The Mariner NOAA home page: http://www.noaa.gov NWS home page: http://www.nws.noaa.gov NWS marine dissemination page: http://www.nws.noaa.gov/om/marine/home.htm NWS marine text products: http://www.nws.noaa.gov/om/marine/forecast.htm NWS radio facsmile/marine charts: http://weather.noaa.gov/fax/marine.shtml NWS publications: http://www.nws.noaa.gov/om/nwspub.htm NOAA Data Buoy Center: http://www.ndbc.noaa.gov NOAA Weather Radio: http://www.nws.noaa.gov/nwr National Ocean Service (NOS): http://co-ops.nos.noaa.gov/ NOS Tide data: http://tidesonline.nos.noaa.gov/ USCG Navigation Center: http://www.navcen.uscg.mil Tropical Prediction Center: http://www.nhc.noaa.gov/ High Seas Forecasts and Charts: http://www.nhc.noaa.gov/forecast.html Marine Prediction Center: http://www.mpc.ncep.noaa.gov SST & Gulfstream: http://www4.nlmoc.navy.mil/data/oceans/gulfstream.html Hurricane Preparedness & Tracks: http://www.fema.gov/fema/trop.htm Time Zone Conversions: http://tycho.usno.navy.mil/zones.html Table of Contents Introduction and Purpose ................................................................................................................... 1 Disclaimer ........................................................................................................................................... -
Climate Changes Associated with Increasing CO 2
Welcome to ATMS 111 Global Warming http://www.atmos.washington.edu/2010Q1/111 These slides are preliminary and will likely be revised by class time. Vertical structure of the atmosphere Stratosphere ozone layer / ozone hole ultraviolet solar radiation sulfate aerosols from volcanic eruptions increasing GHG produces cooling Troposphere most clouds and atmospheric water vapor ozone from air pollution short residence time of aerosols Hurricanes and other storms RG p128-146 A taste of things to come? Keeping count: will there be more cyclones in the future? Surges and downpours Coastal concerns beyond the tropics Coastal storm flooding: a deepening problem Tornadoes: an overblown connection? Was Hurricane Katrina related to global warming? http://orca.rsmas.miami.edu/~schen/Isabel/goes_floater030912.avi Photo by UW Prof R. Houze The first storm churns up colder, deeper waters and leaves a trail of cool in its wake. The second storm loses strength when intersects this cold water trail. NASA NASA's Aqua and TRMM of SST. Sea height using the Jason-1 satellite. http://www.nasa.gov/centers/goddard/earthandsun/eye_to_eye.html Another example of cooler SST after storm passes Cold ocean temperature in Katrina’s Wake http://www.gfdl.noaa.gov/visualizations-hurricanes Loop Current 200-300km wide 80-150 m deep warm current ribbon In step 2 it has stretched so that it breaks off an eddy in step 3 Happens about ~6-11 months http://www7320.nrlssc.navy.mil/global_nlom32/ias.html Hurricane Katrina: Ocean Heat Content and wind speed in mph (next to black dots) Hurricane produce oceanic upwelling beneath the eye Upwelling of cold water can provide a strong negative feedback that limits the strength of the hurricane.