Forecasting at the National Hurricane Center: Past, Present and Future
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The 2009 Atlantic Hurricane Season in Perspective by Dr
AIRCURRENTS THE 2009 ATLANTIC EDITor’s noTE: November 30 marked the official end of the Atlantic HURRICANE SEASON hurricane season. With nine named storms, including three hurricanes, and no U.S. landfalling hurricanes, this season was the second quietest since IN PERSPECTIVE 1995, the year the present period of above-average sea surface temperatures (SSTs) began. This year’s relative inactivity stands in sharp contrast to the 2008 season, during which Hurricanes Dolly, Gustav, and Ike battered the Gulf Coast, causing well over 10 billion USD in insured losses. With no U.S. landfalling hurricanes in 2009, but a near miss in the Northeast, 2009 reminds us yet again of the dramatic short term variability in hurricane 12.2009 landfalls, regardless of whether SSTs are above or below average. By Dr. Peter S. Dailey HOW DOES ACTIVITY IN 2009 COMPARE TO Hurricanes are much more intense than tropical storms, LONG-TERM AVERAGES? producing winds of at least 74 mph. Only about half of By all standard measures, the 2009 Atlantic hurricane tropical storms reach hurricane strength in a typical year, season was below average. Figure 1 shows the evolution with an average of six hurricanes by year end. Major of a “typical” season, which reflects the long-term hurricanes, with winds of 111 mph or more, are even rarer, climatological average over many decades of activity. with only about three expected in the typical year. Note the Tropical storms, which produce winds of at least 39 mph, sharp increase in activity during the core of the season—the occur rather frequently. -
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 -
The Influences of the North Atlantic Subtropical High and the African Easterly Jet on Hurricane Tracks During Strong and Weak Seasons
Meteorology Senior Theses Undergraduate Theses and Capstone Projects 2018 The nflueI nces of the North Atlantic Subtropical High and the African Easterly Jet on Hurricane Tracks During Strong and Weak Seasons Hannah Messier Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/mteor_stheses Part of the Meteorology Commons Recommended Citation Messier, Hannah, "The nflueI nces of the North Atlantic Subtropical High and the African Easterly Jet on Hurricane Tracks During Strong and Weak Seasons" (2018). Meteorology Senior Theses. 40. https://lib.dr.iastate.edu/mteor_stheses/40 This Dissertation/Thesis is brought to you for free and open access by the Undergraduate Theses and Capstone Projects at Iowa State University Digital Repository. It has been accepted for inclusion in Meteorology Senior Theses by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. The Influences of the North Atlantic Subtropical High and the African Easterly Jet on Hurricane Tracks During Strong and Weak Seasons Hannah Messier Department of Geological and Atmospheric Sciences, Iowa State University, Ames, Iowa Alex Gonzalez — Mentor Department of Geological and Atmospheric Sciences, Iowa State University, Ames Iowa Joshua J. Alland — Mentor Department of Atmospheric and Environmental Sciences, University at Albany, State University of New York, Albany, New York ABSTRACT The summertime behavior of the North Atlantic Subtropical High (NASH), African Easterly Jet (AEJ), and the Saharan Air Layer (SAL) can provide clues about key physical aspects of a particular hurricane season. More accurate tropical weather forecasts are imperative to those living in coastal areas around the United States to prevent loss of life and property. -
ABSTRACT Title of Document: the EFFECT of HURRICANE SANDY
ABSTRACT Title of Document: THE EFFECT OF HURRICANE SANDY ON NEW JERSEY ATLANTIC COASTAL MARSHES EVALUATED WITH SATELLITE IMAGERY Diana Marie Roman, Master of Science, August 2015 Directed By: Professor, Michael S. Kearney, Environmental Science and Technology Hurricane Sandy, one of several large extratropical hurricanes to impact New Jersey since 1900, produced some of the most extensive coastal destruction within the last fifty years. Though the damage to barrier islands from Sandy was well-documented, the effect of Sandy on the New Jersey coastal marshes has not. The objective of this analysis, based on twenty-three Landsat Thematic Mapper (TM) data sets collected between 1984 and 2011 and Landsat 8 Operational Land Imager (OLI) images collected between 2013 and 2014 was to determine the effect of Hurricane Sandy on the New Jersey Atlantic coastal marshes. Image processing was performed using ENVI image analysis software with the NDX model (Rogers and Kearney, 2004). Results support the conclusion that the marshes were stable between 1984 and 2006, but had decreased in vegetation density coverage since 2007. Hurricane Sandy caused the greatest damage to low-lying marshes located close to where landfall occurred. THE EFFECT OF HURRICANE SANDY ON NEW JERSEY ATLANTIC COASTAL MARSHES EVALUATED WITH SATELLITE IMAGERY by Diana Marie Roman Thesis submitted to the Faculty of the Graduate School of the University of Maryland, College Park in partial fulfillment of the requirements for the degree of Masters of Science 2015 Advisory Committee: Professor Michael Kearney, Chair Professor Andrew Baldwin Associate Professor Andrew Elmore © Copyright by Diana Marie Roman 2015 Forward Hurricane storm impacts on coastal salt marshes have increased over time. -
UB Powerpoint Template
converge.colorado.edu CONVERGE ethical, coordinated, and scientifically rigorous social science, engineering, and interdisciplinary extreme events research Lori Peek Principal Investigator, CONVERGE, SSEER, and ISEEER Director, Natural Hazards Center Professor, Department of Sociology University of Colorado Boulder Session 2: Collecting, Managing, and Archiving Social and Behavioral Science Data Describe opportunities for identifying and coordinating social science researchers so that we can best share information and publish our data as well as data collection protocols using DOIs, repositories, etc. Discuss some of the overarching challenges and concerns with sharing social science data, such as privacy, data management plans and related IRB policies, duplication vs. replication, etc. converge.colorado.edu 4 Things converge.colorado.edu 1. NSF has funded the CONVERGE initiative converge.colorado.edu Why CONVERGE? Why CONVERGE? • identify and coordinate researchers and research teams; • advance hazards and disaster research; • encourage the publication of data and data collection instruments and protocols (DesignSafe Cyberinfrastructure + CONVERGE). • support and accelerate training and mentoring; • fund virtual reconnaissance, field research, and the development of novel research instruments and data collection protocols; • accelerate the development of mobile applications for social science data collection (NHERI RAPID); Why CONVERGE? 2. NSF Supports Extreme Events Research (EER) Networks converge.colorado.edu Why the EER’s? Disciplinary -
Florida Housing Coalition Hurricane Member Update Webinar May 1, 2020 Sponsored by Fannie Mae AGENDA
Florida Housing Coalition Hurricane Member Update Webinar May 1, 2020 Sponsored by Fannie Mae AGENDA • COVID-19 Updates • NOAA, National Hurricane Center, and National Weather Service: Preparing for Hurricane Season COVID-19 SHIP Frequently Asked Questions New Content on Topics Including: • File Documentation • Technical Revisions • Rental Assistance • Mortgage Assistance • Foreclosure Counseling • Reporting COVID SHIP Assistance FAQ File Documentation Question Upcoming COVID-19 Trainings “Implementing Effective Rental Assistance Programs with Federal and State Resources” May 13 at 10:00 am https://attendee.gotowebinar.com/register/7291419462613166863 “COVID-19 SHIP Rent Assistance Implementation" May 18 at 2:00 pm https://attendee.gotowebinar.com/register/7691296448631153675 “COVID-19 SHIP Mortgage Assistance Implementation" May 20 at 2:00 pm https://attendee.gotowebinar.com/register/620374553799087627 Recent COVID-19 Trainings Recordings: • Emergency SHIP Assistance for Renters https://vimeo.com/403418248 • Helping Homeowners with COVID-19 SHIP Emergency Assistance https://vimeo.com/407646578 • Assisting Homeless and Special Needs Populations through COVID-19 https://vimeo.com/405609513 • Virtual SHIP https://vimeo.com/410260129 NOAA, National Hurricane Center, and National Weather Service: Preparing for Hurricane Season Andrew Latto NHC Hurricane Specialist [email protected] Regarding evacuations and planning: • https://www.weather.gov/wrn/2020-hurricane- evacuation Regarding Evacuations and Planning Regarding evacuations and planning: -
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. -
Downloaded 10/05/21 07:00 AM UTC 3074 MONTHLY WEATHER REVIEW VOLUME 145
AUGUST 2017 H A Z E L T O N E T A L . 3073 Analyzing Simulated Convective Bursts in Two Atlantic Hurricanes. Part I: Burst Formation and Development a ANDREW T. HAZELTON Department of Earth, Ocean and Atmospheric Science, The Florida State University, Tallahassee, Florida ROBERT F. ROGERS NOAA/AOML/Hurricane Research Division, Miami, Florida ROBERT E. HART Department of Earth, Ocean and Atmospheric Science, The Florida State University, Tallahassee, Florida (Manuscript received 15 July 2016, in final form 21 April 2017) ABSTRACT Understanding the structure and evolution of the tropical cyclone (TC) inner core remains an elusive challenge in tropical meteorology, especially the role of transient asymmetric features such as localized strong updrafts known as convective bursts (CBs). This study investigates the formation of CBs and their role in TC structure and evolution using high-resolution simulations of two Atlantic hurricanes (Dean in 2007 and Bill in 2009) with the Weather Research and Forecasting (WRF) Model. Several different aspects of the dynamics and thermodynamics of the TC inner-core region are investigated with respect to their influence on TC convective burst development. Composites with CBs show stronger radial inflow in the lowest 2 km, and stronger radial outflow from the eye to the eyewall around z 5 2–4 km, than composites without CBs. Asymmetric vorticity associated with eyewall mesovortices appears to be a major factor in some of the radial flow anomalies that lead to CB development. The anomalous outflow from these mesovortices, along with outflow from supergradient parcels above the boundary layer, favors low-level convergence and also appears to mix high-ue air from the eye into the eyewall. -
Evaluation of Response to Hurricane Dean in Three Countries of The
Evaluation of the Response to Hurricane Dean in Jamaica, St. Lucia and Dominica Full Report Oxfam GB Programme Evaluation June 2008 Commissioned by: Oxfam GB LAC Evaluators: Vivien Margaret Walden Executive summary In 2007, Hurricane Dean (category 4 with sustained wind of 150 mph), made landfall in Jamaica on August 19th 2007 leaving a trail of damage along the Southern coast. According to initial reports, as many as 300,000 people were temporarily displaced by Dean. The communities most affected are located in the southern part of the island that was impacted by hurricanes Emily, Ivan, and Wilma in 2004 and 2005. On St. Lucia and Dominica, the hurricane made landfall on August 17th causing widespread damage to the agricultural sector. Most of the damage was caused by the hurricane and tropical storm winds but there were several areas where flooding occurred. The banana crop is the main agricultural activity in both islands and farmers are highly dependent on the benefit from this crop. The majority of them are certified and socially organized as banana Fair Trade farmers. Non-banana farmers were also affected as vegetable crops and animal pens were destroyed. This evaluation carried out after the six-month programmes have closed was to look at the following areas: • To review the project design and implementation • To identify and document innovative and good practices • To identify persistent weaknesses (particularly in internal systems) for organisational learning The evaluation was carried out by semi-structured interviews with key informants and focus groups in the three countries with a variety of stakeholders. -
Hurricane Dorian
eVENT Hurricane Tracking Advisory Hurricane Dorian Information from NHC Advisory 20, 5:00 AM AST Thu Aug 29, 2019 On the forecast track, Dorian should move over the Atlantic well east of the southeastern and central Bahamas today and on Friday, and approach the northwestern Bahamas on Saturday. Maximum sustained winds are near 85 mph (140 km/h) with higher gusts. Strengthening is forecast during the next few days, and Dorian is expected to become a major hurricane on Friday. Intensity Measures Position & Heading U.S. Landfall (NHC) Max Sustained Wind 85 mph Position Relative to 150 mi NNW of San Juan, PR Speed: (Category 1) Land: Est. Time & Region: Monday on Florida Min Central Pressure: 991 mb Coordinates: 20.5 N, 66.6 W Trop. Storm Force Est. Max Sustained 90 miles Bearing/Speed: NW or 325 degrees at 13 mph 111+ mph (Category 3) Winds Extent: Wind Speed: Forecast Summary ■ The NHC forecast map (below left) and the wind-field map (below right), which is based on the NHC’s forecast track, both show Dorian passing east of the central Bahamas today and Friday, and approaching the northwestern Bahamas on Saturday. To illustrate the uncertainty in Dorian’s forecast track, Ï!D Trop Dep forecast tracks for all current models are shown on the wind-field map in pale gray. ■ Maximum sustained winds are near 85 mph with higher gusts. Strengthening is forecast during the next few days, and Dorian is expectedÏ!S Trop Storm to become a 1 major hurricane on Friday. Ï! Ca t 1 ■ Dorian is expected to produce total rain accumulations of 2 to 4 inches in the central Bahamas, 4 to 8 inches in the northwestern BahamasÏ!D Trop Dep and coastal 2 Ï! Ca t 2 sections of the southeast United States Ï!S Trop Storm ■ Swells around the U.S. -
Hurricane Dorian Hits Eastern NC by Chris Collins, Meteorologist
National Weather Service, Newport/Morehead City, NC http://weather.gov/Newport —> Bookmark it!! Fall 2019 Edition Hurricane Dorian hits Eastern NC By Chris Collins, Meteorologist Hurricane Dorian was the fourth named storm, second hurricane, and first major hurri- cane of the 2019 Atlantic hurricane season. Dorian formed on August 24, 2019 from a tropical wave in the Central Atlantic and gradually strengthened as it moved toward the Lesser Antilles, becoming a hurricane on August 28. Rapid intensification occurred, and on August 31, Dorian became a Category 4 hurricane. On September 1, Dorian reached Category 5 intensity, with maximum sustained winds of 185 mph, and a minimum central pressure of 910 mb, while making landfall in Elbow Cay, Bahamas. The ridge of high pressure steering Dorian westward collapsed on September 2, causing Dorian to stall just north of Grand Bahama for about a day. It is the strongest known tropical system to impact the Bahamas. On the morning of September 3, Dorian began to move slowly to- wards the north-northwest. Dorian moved over warmer waters, regaining Category 3 in- tensity by midnight on September 5. In the early hours of September 6, Dorian weakened to Category 1 intensity as it picked up speed and turned northeast. Dorian would pick up speed and move northeast along the North Carolina coast September 6, moving just south of the Crystal Coast, clipping Cape Lookout and eventually making landfall at Cape Hat- teras. CONTENTS Hurricane Dorian 1-2 Skywarn Recognition Day 3 Summer Volunteer 2019 4 Saharan Dust 5 July Heat 6 Path of Hurricane Dorian, August 24-September 6, 2019. -
Learning from Hurricane Hugo: Implications for Public Policy
LEARNING FROM HURRICANE HUGO: IMPLICATIONS FOR PUBLIC POLICY prepared for the FEDERAL INSURANCE ADMINISTRATION FEDERAL EMERGENCY MANAGEMENT AGENCY 500 C Street, S.W. Washington, D.C. 20472 under contract no. EMW-90-G-3304,A001 June 1992 CONTENTS INTRODUCTION ............................... 1.............I PHYSICAL CHARACTERISTICS OF THE STORM . 3 Wind Speeds .3 IMPACTS ON NATURAL SYSTEMS 5 ................................ Biological Systems ....... .................................5 Dunes and Beaches ....... .5............................... Beach Nourishment . .................................7 IMPACTS ON HUMANS AND HUMAN SYSTEMS ............................ 9 Deaths and Injuries ............................ 9 Housing ............................ 9 Utilities ................... 10 Transportation Systems .1................... 10 The Economy ................... 11 Psychological Effects ................... 11 INSURANCE .......................... 13 COASTAL DEVELOPMENT .......................... 14 Setbacks ........................... 15 Coastal Protection Structures .......................... 16 PERFORMANCE OF STRUCTURES ..... .... 18 Effects of Wind and/or Water ...... .... 18 Effects of Water, Waves, or Erosion . .. .18 Effects of Wind .............. .... 19 Foundations .................. .... 21 Slabs ................ .... 22 Piers and Columns ....... .... 22 Pilings............... .... 22 Elevation .................. .... 23 Lower Area Enclosures .... .... 23 Connections ................. ....24 Manufactured Housing .......... .... 24