Hurricane Maria

Total Page:16

File Type:pdf, Size:1020Kb

Hurricane Maria eVENT Hurricane Tracking Advisory Hurricane Maria Information from NHC Advisory 27, 5:00 PM AST Fri September 22, 2017 Maria is moving toward the north-northwest near 9 mph (15 km/h), and this general motion is expected to continue through Saturday. A turn toward the north is forecast by Saturday night. Maximum sustained winds are near 125 mph (205 km/h) with higher gusts. Maria is a category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale. A gradual weakening is forecast during the next 48 hours. Intensity Measures Position & Heading U.S. Landfall (NHC) 115 miles ENE of the southeastern Max Sustained Wind 125 mph Position Relative to Bahamas Speed: (Category 3) Land: 395 miles ESE of Nassau Est. Time & Region: N/A Min Central Pressure: 959 mb Coordinates: 23.3 N, 71.4 W Trop. Storm Force Est. Max Sustained 160 miles Bearing/Speed: NNW or 335 degrees at 9 mph N/A Winds Extent: Wind Speed: Forecast Summary ■ The NHC forecast map (below left) and the wind-field map (below right) both show Maria now moving northwest through Saturday. To illustrate the uncertainty in Maria’s forecast track, forecast tracks for all current models are shown on the wind-field map (below right) in pale gray. ■ Tropical storm conditions will continue to occur over portions of the Turks and Caicos Islands and the southeastern Bahamas through tonight. Tropical storm conditions are expected in the central Bahamas beginning tonight. ■ Maria is expected to produce the following rain accumulations through Saturday: 8-16 inches on the Turks and Caicos Islands, 4-8 inches on Mayaguana in the Bahamas, 1-3 inches on Puerto Rico along with the eastern Bahamas, 2-6 inches on Inagua Islands and Crooked Islands in the Bahamas. Rainfall on these islands will continue to cause life- threatening flash floods and mudslides. Forecast Track for Hurricane Maria Forecast Wind-field for Hurricane Maria TD TS Ca t 1 Ca t 2 Ca t 3 Ca t 4 Watch/Warn Al l F c st Tr ac ks © Copyright 2016 Willis Limited / Willis Re Inc. All rights reserved: No part of this publication may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, whether electronic, mechanical, photocopying, recording, or otherwise, without the permission of Willis Limited/Willis Re Inc. Some information contained in this report may be compiled from third party sources; however, we do not guarantee and are not responsible for the accuracy of Hazard and damage potential maps such. This report is for general information only, is not intended to be relied upon, and any action based on or in connection with anything contained herein should be taken only after obtaining specific advice. The views expressed in this produced by Willis are based on numerical report are not necessarily those of Willis Limited/Willis Re Inc., or any of its/their parent or sister companies, subsidiaries or affiliates, Willis Towers Watson PLC or any member companies thereof (hereinafter “Willis Towers Watson”). modeling results from Kinetic Analysis Willis Towers Watson accepts no responsibility for the content or quality of any third party websites to which we refer. Corporation. The TAOS real-time hazard and impact forecast information is provided "as is" and without warranties as to performance or any other warranties whether expressed or implied. The user is strongly cautioned to recognize that natural hazards modeling and analysis are subject to many uncertainties. These uncertainties include, but are not limited to, the uncertainties inherent in weather and climate, incomplete or inaccurate weather data, changes to the natural and built environment, limited historical records, and limitations in the state of the art of modeling, as well as limits to the scientific understanding of storm weather phenomena. Anyone making use of the hazard and impact information provided by KAC, or the information contained within, assumes all liability deriving from such use, and agrees to "hold harmless" any and all agencies or individuals associated with its creation. The user agrees to provide any subsequent users of this data with this disclaimer. The publication of the material contained herein is not intended as a representation or warranty that this information is suitable for any general or particular use. Coastal Watches and Warnings A Tropical Storm Warning – meaning that tropical storm conditions are expected within the warning area - is in effect for Turks and Caicos Islands, the southeastern and central Bahamas. Summary of Atlantic Hurricane Activity to Date Benchmarking the 2017 Atlantic Season to Date 2017 Activity versus Average Activity for the years 1950 – 2011 Tropical Total Cat 3-5 16 Tropical Storm avg '50-'11 Tropical Storm 2017 Storms Hurricanes Hurricanes Hurricane avg '50-'11 Hurricane 2017 TS Maria Major Hurricane avg '50-'11 Major Hurricane 2017 2017 year to date (1/1/17 – 09/22/17) 13 7 4 12 TS Lee TS Katia 2016 year to date (1/1/16 – 09/22/16) 12 4 1 TS Jose TS Irma 8 TS Harvey 1995-2011 season average 14.7 7.9 3.8 TS Gert HU Maria TS FranklinHU Katia 10.7 6.2 2.7 Hu Jose 1950-2011 season average TS Emily 4 TS Don HU Irma Major HU Maria HU Harvey 2017 CSU season forecasts 13 6 2 TS Cindy Major HU Jose TS Bret HU Gert Major HU Irma (Colorado State University at June 1,‘17) HU Franklin Major HU Harvey 2017 NOAA season forecasts 11-17 5-9 2-4 0 May Jun Jul Aug Sep Oct Nov (May25, 2017) Tropical Storm Activity to Date 2017 Tropical Storm Activity versus Average Activity Maria is the thirteenth named storm, seventh hurricane, and fourth major The graph above shows 2017 Atlantic Hurricane Season activity and average occurrence rates since 1950 by date, category and order. It shows, for example, that hurricane of the 2017 Atlantic Hurricane Season. Last year saw twelve named storms four hurricanes and one major hurricane by September 22. Maria became the season’s seventh named hurricane on September 17. It also shows the average season has 10.7 tropical storms, 6.2 hurricanes and 2.7 major hurricanes (categories 3-5). New Tropical Cyclone Potential and Most Likely Arrival Time of Tropical Storm Force WiFive Day d Tropical Weather Outlook Most Likely Arrival Time of Tropical-Storm-Force Winds A small area of low pressure, associated with the remnants of Lee, is located over the The graphic below shows the most likely arrival time of tropical storm for winds - the central Atlantic Ocean almost a thousand miles east-southeast of Bermuda. The low time before or after which the onset of tropical-storm-force winds is equally likely. It also is producing a concentrated area of showers and thunderstorms, although the shows probabilities of sustained (1-minute average) surface wind speeds equal to or circulation appears somewhat elongated. Some additional development of this exceeding 34 kt (39 mph) for the next five days. This graphic is based on the official system is possible during the next few days while it moves slowly northward through National Hurricane Center (NHC) track, intensity, and wind radii forecasts, and on NHC early next week. forecast error statistics for those forecast variables during recent years. * Formation chance through 48 hours...medium...40 percent. * Formation chance through 5 days...medium...50 percent. Contact us Roy Cloutier Ryan Vesledahl Matt Nicolai roy.cloutier@ willistowerswatson.com [email protected] [email protected] +1 (952) 841-6652 +1 (952) 841-6672 +1 (952) 841-6657 2 .
Recommended publications
  • Hurricane & Tropical Storm
    5.8 HURRICANE & TROPICAL STORM SECTION 5.8 HURRICANE AND TROPICAL STORM 5.8.1 HAZARD DESCRIPTION A tropical cyclone is a rotating, organized system of clouds and thunderstorms that originates over tropical or sub-tropical waters and has a closed low-level circulation. Tropical depressions, tropical storms, and hurricanes are all considered tropical cyclones. These storms rotate counterclockwise in the northern hemisphere around the center and are accompanied by heavy rain and strong winds (NOAA, 2013). Almost all tropical storms and hurricanes in the Atlantic basin (which includes the Gulf of Mexico and Caribbean Sea) form between June 1 and November 30 (hurricane season). August and September are peak months for hurricane development. The average wind speeds for tropical storms and hurricanes are listed below: . A tropical depression has a maximum sustained wind speeds of 38 miles per hour (mph) or less . A tropical storm has maximum sustained wind speeds of 39 to 73 mph . A hurricane has maximum sustained wind speeds of 74 mph or higher. In the western North Pacific, hurricanes are called typhoons; similar storms in the Indian Ocean and South Pacific Ocean are called cyclones. A major hurricane has maximum sustained wind speeds of 111 mph or higher (NOAA, 2013). Over a two-year period, the United States coastline is struck by an average of three hurricanes, one of which is classified as a major hurricane. Hurricanes, tropical storms, and tropical depressions may pose a threat to life and property. These storms bring heavy rain, storm surge and flooding (NOAA, 2013). The cooler waters off the coast of New Jersey can serve to diminish the energy of storms that have traveled up the eastern seaboard.
    [Show full text]
  • 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.
    [Show full text]
  • Regional Overview: Impact of Hurricanes Irma and Maria
    REGIONAL OVERVIEW: IMPACT OF MISSION TO HURRICANES IRMA AND MARIA CONFERENCE SUPPORTING DOCUMENT 1 The report was prepared with support of ACAPS, OCHA and UNDP 2 CONTENTS SITUATION OVERVIEW ......................................................................................................................... 4 KEY FINDINGS ............................................................................................................................................ 5 Overall scope and scale of the impact ....................................................................................... 5 Worst affected sectors ...................................................................................................................... 5 Worst affected islands ....................................................................................................................... 6 Key priorities ......................................................................................................................................... 6 Challenges for Recovery ................................................................................................................. 7 Information Gaps ................................................................................................................................. 7 RECOMMENDATIONS FOR RECOVERY ................................................................................ 10 Infrastructure ......................................................................................................................................
    [Show full text]
  • Hurricane Maria Situation Report #1 As of 9:00Pm Ast on September 20, 2017
    Resilience Way, Lower Estate, St. Michael Tel: (246) 434-4880 Fax: (246) 271-3660 Email: [email protected] Visit our website: www.cdema.org HURRICANE MARIA SITUATION REPORT #1 AS OF 9:00PM AST ON SEPTEMBER 20, 2017 SYNOPSIS OF HURRICANE MARIA Maria, the 13th named hurricane of the 2017 Atlantic Hurricane Season, became a category 5 hurricane near the Leeward Islands on Monday September 18th, 2017. Hurricane Maria impacted Dominica at approximately 9:35pm on September 18th as an extremely strong hurricane with wind speeds of 155 mph. Maria then impacted St. Kitts and Nevis and Antigua and Barbuda on September 19th, 2017 and the Virgin Islands September 19 – 20, 2017. At 800 PM AST (2100 UTC), the eye of Hurricane Maria was located near latitude 18.9 North, longitude 67.5 West. Maria is moving toward the northwest near 12 mph (19 km/h), and this general motion with a decrease in forward speed is expected through Thursday night. Data from an Air Force Reserve Hurricane Hunter aircraft indicate that maximum sustained winds remain 110 mph (175 km/h) with higher gusts. Hurricane-force winds extend outward up to 60 miles (95 km) from the center, and tropical storm- force winds extend outward up to 150 miles (240 km). The minimum central pressure based on data from the Air Force aircraft remains at 958 mb (28.29 inches). PROGNOSIS: The National Hurricane Center (NHC) indicates that on the forecast track, the core of Hurricane Maria will continue to move away from the northwestern coast of Puerto Rico this evening.
    [Show full text]
  • Bridges – Winter 2018
    Brethren Disaster Ministries Rebuilding Homes • Nurturing Children • Responding Globally Vol. 19, Winter 2018 Another record year for INSIDE Children’s Disaster Services CDS 2017 Response Statistics ........2 by Kathy Fry-Miller CDS Spring 2018 workshops ..........3 Children’s Disaster Services (CDS) had Several volunteers served on more CDS 2017 Workshops ....................3 an exceptionally full year again in 2017 than one response in 2017. One repeat Hurricane Maria Response and with a record number of 16 domestic responder, Pat Krabacher, shared, “In Recovery in Puerto Rico ................4 disaster responses, including two critical both California and Texas we saw Rebuild Program Updates................5 responses—the mass casualty shooting in amazing generosity poured out all around Hurricane Response in the U.S. October in Las Vegas, Nev., and the us with ordinary Americans doing Virgin Islands ................................6 Amtrak derailment in Tacoma, Wash., something to help. We were loved by Mission Alive conference ................6 in December. CDS had been able to people who served us and provided food, Volunteering at any age can be build up our volunteer base and a place to lay our heads, and security guys life-changing ..................................7 leadership support over the past few who sat up all night out in the cold while BDM 2017 Rebuild Responses ......7 years with support from the Christian we slept. As we were loved, so we too BDM 2017 Project Expenses ..........8 Church (Disciples of Christ) and United were changed by that love.” BDM 2017 Project Funding ..........8 Methodist Committee on Relief. This Both CDS associate director Kathy BDM 2017 Project Expenses ........8 gave us the capacity to respond to these Fry-Miller and program assistant Sherry Hope is alive in Eureka, Mo.
    [Show full text]
  • Upgrades to the GFDL/GFDN Hurricane Model for 2014 (A JHT Funded Project) Morris A
    Upgrades to the GFDL/GFDN Hurricane Model for 2014 (A JHT Funded Project) Morris A. Bender, Matthew Morin, Timothy Marchok, Isaac Ginis, Biju Thomas, Richard Yablonsky and Robert Tuleya 68th Interdepartmenal Hurricane Conference Tuesday, March 5th GFDL 2014 Hurricane Model Upgrade • Increased horizontal resolution of inner nest from 1/12th to 1/18th degree with reduced damping of gravity waves in advection scheme • Improved specification of surface exchange coefficients (ch, cd) and surface stress computation in surface physics • Improved specification of surface roughness and wetness over land. • Modified PBL with variable Critical Richardson Number. • Advection of individual micro-physics species. (Yet to test impact of Rime Factor Advection) • Improved targeting of initial storm maximum wind and storm structure in initialization. (Reduces negative intensity bias in vortex specification) • Remove vortex specification in Atlantic for storms of 40 knots and less • Upgrade ocean model to 1/12th degree MPI POM with unified trans-Atlantic basin and 3D ocean for Eastern Pacific basin • Remove global_chgres in analysis step (direct interpolation from hybrid to sigma coordinates) New Cd and Ch formulation New Ch New Cd Current HWRF and GFDL Cd Current HWRF Ch Comparison of New cd and ch with Recent Referenced Studies Cd Ch Impact of Bogusing on Intensity Errors For Storms 40 knots or less Bogus No Bogus Bogusing Significantly Atlantic Degraded performance in Atlantic for weak systems No Bogus Bogus Bogusing Eastern Significantly Improved Pacific
    [Show full text]
  • Met Office Unified Model Tropical Cyclone Performance Following Major Changes to the Initialization Scheme and a Model Upgrade
    OCTOBER 2016 H E M I N G 1433 Met Office Unified Model Tropical Cyclone Performance Following Major Changes to the Initialization Scheme and a Model Upgrade JULIAN T. HEMING Met Office, Exeter, Devon, United Kingdom (Manuscript received 1 March 2016, in final form 27 June 2016) ABSTRACT The Met Office has used various schemes to initialize tropical cyclones (TCs) in its numerical weather pre- diction models since the 1980s. The scheme introduced in 1994 was particularly successful in reducing track forecast errors in the model. Following modifications in 2007 the scheme was still beneficial, although to a lesser degree than before. In 2012 a new trial was conducted that showed that the scheme now had a detrimental impact on TC track forecasts. As a consequence of this, the scheme was switched off. The Met Office Unified Model (MetUM) underwent a major upgrade in 2014 including a new dynamical core, changes to the model physics, an increase in horizontal resolution, and changes to satellite data usage. An evaluation of the impact of this change on TC forecasts found a positive impact both on track and particularly intensity forecasts. Following implementation of the new model formulation in 2014, a new scheme for initialization of TCs in the MetUM was developed that involved the assimilation of central pressure estimates from TC warning centers. A trial showed that this had a positive impact on both track and intensity predictions from the model. Operational results from the MetUM in 2014 and 2015 showed that the combined impact of the model upgrade and new TC initialization scheme was a dramatic cut in both TC track forecast errors and intensity forecast bias.
    [Show full text]
  • Hurricane Interaction with the Upper Ocean in the Amazon-Orinoco Plume Region
    Hurricane interaction with the upper ocean in the Amazon-Orinoco plume region Yannis Androulidakis, Vassiliki Kourafalou, George Halliwell, Matthieu Le Hénaff, Heesook Kang, Michael Mehari & Robert Atlas Ocean Dynamics Theoretical, Computational and Observational Oceanography ISSN 1616-7341 Volume 66 Number 12 Ocean Dynamics (2016) 66:1559-1588 DOI 10.1007/s10236-016-0997-0 1 23 Your article is protected by copyright and all rights are held exclusively by Springer- Verlag Berlin Heidelberg. This e-offprint is for personal use only and shall not be self- archived in electronic repositories. If you wish to self-archive your article, please use the accepted manuscript version for posting on your own website. You may further deposit the accepted manuscript version in any repository, provided it is only made publicly available 12 months after official publication or later and provided acknowledgement is given to the original source of publication and a link is inserted to the published article on Springer's website. The link must be accompanied by the following text: "The final publication is available at link.springer.com”. 1 23 Author's personal copy Ocean Dynamics (2016) 66:1559–1588 DOI 10.1007/s10236-016-0997-0 Hurricane interaction with the upper ocean in the Amazon-Orinoco plume region Yannis Androulidakis1 & Vassiliki Kourafalou 1 & George Halliwell2 & Matthieu Le Hénaff2,3 & Heesook Kang1 & Michael Mehari3 & Robert Atlas2 Received: 3 February 2016 /Accepted: 14 September 2016 /Published online: 6 October 2016 # Springer-Verlag Berlin Heidelberg 2016 Abstract The evolution of three successive hurricanes the amount of ocean thermal energy provided to these storms (Katia, Maria, and Ophelia) is investigated over the river was greatly reduced, which acted to limit intensification.
    [Show full text]
  • Climate Change & Hurricane Risk
    Climate Change and Atlantic Hurricane Risk Risk Prediction Bermuda Institute of Ocean Sciences (BIOS) 17 Biological Station St. George’s GE 01 Bermuda risk.bios.edu Initiative contents Introduction 3 Atlantic Hurricanes Landfall and Intensity 4 Measuring Storm Strength 6 Hurricanes and Climate change 8 Warmer water stronger storms 8 Formation Locations and Maximum Intensity 9 Rainfall 10 Exposure growth and Sea Level Rise 12 Summary 13 References 14 Bermuda Institute of Ocean Sciences (BIOS) 17 Biological Station St. George’s GE 01 Bermuda risk.bios.edu Cover image: NASA satellite image of major Hurricane Florence in 2018. Pg 2 Climate change and Atlantic hurricane risk The 2017 hurricane season highlights most of the impacts suffered by countries with Atlantic, Caribbean or Gulf of Mexico coastlines. Storms in this season caused devastation from major hurricane wind speeds, storm surge and flood-induced flooding, tragic loss of life, disruption to livelihoods and destruction to property. Introduction The 2017 and 2018 hurricane seasons have heralded the end of the period of no US major hurricane landfalls, caused devastating impacts across the Caribbean, Central and North America region, and sparked renewed questions about the impact of climate change on hurricane activity in the public and private sectors. In some cases, the damage inflicted by hurricanes in the last 2 seasons has been unprecedented in scale and impact, with record-breaking rainfall-induced flooding in some coastal communities and the highest wind speeds on record for some island nations. This report will highlight scientific research that reveals recent findings with relevance to these issues, including trends detected in the long-term record, and future projections of changes of hurricane activity.
    [Show full text]
  • 1 Tropical Cyclone Report Hurricane Maria
    Tropical Cyclone Report Hurricane Maria (AL142011) 6-16 September 2011 Michael J. Brennan National Hurricane Center 11 January 2012 Maria formed in the eastern Atlantic Ocean and brought tropical storm conditions to portions of the Lesser Antilles. Maria then became a category 1 hurricane (on the Saffir- Simpson Hurricane Wind Scale) as it recurved through the northwestern Atlantic before it made landfall in Newfoundland as a strong tropical storm. a. Synoptic History Maria originated from a tropical wave that moved across the west coast of Africa on 2 September. The wave moved westward well to the south of the Cape Verde islands on 3-4 September with little in the way of organized deep convection. Thunderstorm activity increased markedly early on 5 September but remained displaced to the west of the broad surface circulation due to strong easterly vertical wind shear. On 6 September, the low-level center became better defined and deep convection increased further and a tropical depression formed by 1800 UTC that day, centered about 700 n mi west-southwest of the southern Cape Verde Islands. The cyclone moved quickly west-northwestward at 15 to 20 kt and reached tropical storm intensity 6 h later, while centered about 790 n mi west-southwest of the southern Cape Verde Islands. The “best track” chart of Maria’s path is given in Fig. 1, with the wind and pressure histories shown in Figs. 2 and 3, respectively. The best track positions and intensities are listed in Table 11. Maria moved quickly west-northwestward to the south of a subtropical ridge on 7 September and reached an intensity of 45 kt around 1200 UTC that day.
    [Show full text]
  • Hurricanes and Typhoons in the Global Climate System Pier Luigi Vidale 1, Malcolm Roberts2 Kevin Hodges1, P
    Hurricanes and typhoons in the global climate system Pier Luigi Vidale 1, Malcolm Roberts2 Kevin Hodges1, P. Loizou1, Liang Guo1, Armenia Franco-Diaz1, Alex Baker1, Benoit Vanniere1, Rein Haarsma3, Enrico Scoccimarro4, Alessio Bellucci4, Louis-Philippe Caron5 and Jenny Mecking6 (Blue-Action), all PRIMAVERA partners (models and analysis) With many thanks to Suzana Camargo, Tom Knutson and Jim Kosssin 1NCAS-Climate, University of Reading, 2Met Office Hadley Centre, 3Koninklijk Nederlands Meteorologisch Instituut (KNMI), 4Centro Euro-Mediterraneo sui Cambiamenti Climatici S.c.a.r.l (CMCC), 5Barcelona Supercomputing Center (BSC), Barcelona, Spain, 6Southampton Oceanography Centre 7 ECMF 8 ISAC-CNR 9 Oxford University 10 NCAS-CMS Motivation: TCs as rare, albeit significant contributors to climate A B C Contribution of TCs to the extreme rainfall (amount fraction) (%) from July to October, employing TCs tracks from (a) IBTrACS, (b) JRA-55 and (c) ERA-Interim. Climatology for 1998-2015 Franco-Diaz et al. 2019, submitted to Clim Dyn Re-analyses very likely under-estimating the role of TCs in producing precipitation and moisture transports. What is the role of model resolution, model physics, initialisation (Data Assimulation)? Guo et al. 2017 Recent natural catastrophes: comparing 2011 with other years NatCatSERVICE Loss events worldwide 2017 ~300 U$ billion Geographical overview Drought Winter damage, Geophysical events Wildfire Jan – Oct Flood frost (LNU Complex Fires) (Western-, Southern Europe) Jun - Oct (Earthquake, tsunami, 15 Apr - 9 May
    [Show full text]
  • NCST Technical Investigation of Hurricane Maria's Impacts On
    May 16, 2018 NCST Technical NCST Advisory Committee Meeting Investigation of Hurricane Maria’s Impacts on Puerto Rico: Overview of Preliminary Observations and Investigation Goals Judith Mitrani-Reiser, Ph.D. Director, Disaster and Failure Studies Program NIST Long History of Disaster and Failure Studies at NIST Earthquakes Hurricanes Construction & Tornadoes Fires Building San Fernando, CA Camille, MS/LA Skyline Plaza Apartments, Jarrell, TX (1997) DuPont Plaza Hotel, San Juan, (1971) (1969) Bailey’s Crossroads, VA Spencer, SD (1998) PR (1986) (1973) Mexico City, Mexico Alicia, Galveston, TX Oklahoma City, OK First Interstate Bank Building, (1985) (1983) Willow Island Cooling (1999) Los Angeles, CA (1988) Hugo, SC (1989) Tower, WV (1978) Loma Prieta, CA (1989) Joplin, MO (2011) Loma Prieta Earthquake, CA (1989) Northridge, CA (1994) Andrew, FL (1992) Kansas City Hyatt Hillhaven Nursing Home (1989) Regency, Kansas City, MO Moore OK (2013) Kobe, Japan (1995) Fran, NC (1996) (1981) Pulaski Building, Washington, DC (1990) Mitch and Georges, Kocaeli, Turkey (1999) Riley Road Interchange, Happyland Social Club, Bronx, NY (1990) LAC (1998) Maule, Chile (2010) East Chicago, IN (1982) Oakland Hills, CA (1991) Katrina and Rita Christchurch, NZ Harbor Cay Watts St, New York City (1994) (2005) Condominium, Cocoa (2011) Northridge Earthquake, CA (1994) *Matthew, NC Beach, FL (1981) *Puebla, Mexico (2016) Kobe, Japan (1995) (2017) L’Ambiance Plaza, *Harvey, TX (2017) Hartford, CT (1987) Vandalia St, New York City (1998) *Maria, PR (2017) Ashland Oil
    [Show full text]