Hurricanes and Tropical Storms in the Dutch Caribbean
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Observed Hurricane Wind Speed Asymmetries and Relationships to Motion and Environmental Shear
1290 MONTHLY WEATHER REVIEW VOLUME 142 Observed Hurricane Wind Speed Asymmetries and Relationships to Motion and Environmental Shear ERIC W. UHLHORN NOAA/AOML/Hurricane Research Division, Miami, Florida BRADLEY W. KLOTZ Cooperative Institute for Marine and Atmospheric Studies, Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida TOMISLAVA VUKICEVIC,PAUL D. REASOR, AND ROBERT F. ROGERS NOAA/AOML/Hurricane Research Division, Miami, Florida (Manuscript received 6 June 2013, in final form 19 November 2013) ABSTRACT Wavenumber-1 wind speed asymmetries in 35 hurricanes are quantified in terms of their amplitude and phase, based on aircraft observations from 128 individual flights between 1998 and 2011. The impacts of motion and 850–200-mb environmental vertical shear are examined separately to estimate the resulting asymmetric structures at the sea surface and standard 700-mb reconnaissance flight level. The surface asymmetry amplitude is on average around 50% smaller than found at flight level, and while the asymmetry amplitude grows in proportion to storm translation speed at the flight level, no significant growth at the surface is observed, contrary to conventional assumption. However, a significant upwind storm-motion- relative phase rotation is found at the surface as translation speed increases, while the flight-level phase remains fairly constant. After removing the estimated impact of storm motion on the asymmetry, a significant residual shear direction-relative asymmetry is found, particularly at the surface, and, on average, is located downshear to the left of shear. Furthermore, the shear-relative phase has a significant downwind rotation as shear magnitude increases, such that the maximum rotates from the downshear to left-of-shear azimuthal location. -
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. -
St. Eustatius (Statia)
St. Eustatius (Statia) Overview: Sint Eustatius, also known as Statia, is one of the islands which make up the Netherlands Antilles. Over its long history, it changed hands more than 20 times. The island has remained in Dutch hands since 1816. Vocanic in origin, and quite rugged along the coastal areas, it was once one of the busiest and most powerful commercial ports in the Caribbean. As a result of the British blockade during America's Revolutionary War, most goods destined for the new colonies flowed into St. Eustatius. It was not uncommon to see hundreds of supply ships off Oranjestad. When that war ended and mail and supplies were sent directly to the new United States, the economy of St. Eustatius changed dramatically. According to tradition, it was the first foreign port to salute (1776) the American flag. Tourism is the major industry today, and the island is a favorite destination for scuba diving aficionados and nature lovers. Territory: Highest point = Mt. Mazinga, 1,968 ft. (602m) St. Eustatius is hilly with a central flat plain. Sandy beaches are rare. Geographically, the island is saddle- shaped, with the 602 meter-high Mount Mazinga, colloquially called the Quill (a dormant volcano) to the southeast and the smaller pair Signal Hill/Little Mountain and Boven Mountain to the northwest. The bulk of the island's population lives in the "dip" between the two areas, which crosses the center of the island. The island is just 5 miles long and 2 miles wide; area: 21 sq. km. Location: It is in the northern, Leeward Islands portion of the West Indies, some distance southeast of the Virgin Islands. -
'Good Governance' in the Dutch Caribbean
Obstacles to ‘Good Governance’ in the Dutch Caribbean Colonial- and Postcolonial Development in Aruba and Sint Maarten Arxen A. Alders Master Thesis 2015 [email protected] Politics and Society in Historical Perspective Department of History Utrecht University University Supervisor: Dr. Auke Rijpma Internship (BZK/KR) Supervisor: Nol Hendriks Introduction .............................................................................................................................. 2 1. Background ............................................................................................................................ 9 1.1 From Colony to Autonomy ......................................................................................................... 9 1.2 Status Quaestionis .................................................................................................................... 11 Colonial history .............................................................................................................................. 12 Smallness ....................................................................................................................................... 16 2. Adapting Concepts to Context ................................................................................................. 19 2.1 Good Governance ..................................................................................................................... 19 Development in a Small Island Context ........................................................................................ -
Tropical Cyclone Report for Hurricane Ivan
Tropical Cyclone Report Hurricane Ivan 2-24 September 2004 Stacy R. Stewart National Hurricane Center 16 December 2004 Updated 27 May 2005 to revise damage estimate Updated 11 August 2011 to revise damage estimate Ivan was a classical, long-lived Cape Verde hurricane that reached Category 5 strength three times on the Saffir-Simpson Hurricane Scale (SSHS). It was also the strongest hurricane on record that far south east of the Lesser Antilles. Ivan caused considerable damage and loss of life as it passed through the Caribbean Sea. a. Synoptic History Ivan developed from a large tropical wave that moved off the west coast of Africa on 31 August. Although the wave was accompanied by a surface pressure system and an impressive upper-level outflow pattern, associated convection was limited and not well organized. However, by early on 1 September, convective banding began to develop around the low-level center and Dvorak satellite classifications were initiated later that day. Favorable upper-level outflow and low shear environment was conducive for the formation of vigorous deep convection to develop and persist near the center, and it is estimated that a tropical depression formed around 1800 UTC 2 September. Figure 1 depicts the “best track” of the tropical cyclone’s path. The wind and pressure histories are shown in Figs. 2a and 3a, respectively. Table 1 is a listing of the best track positions and intensities. Despite a relatively low latitude (9.7o N), development continued and it is estimated that the cyclone became Tropical Storm Ivan just 12 h later at 0600 UTC 3 September. -
2014 North Atlantic Hurricane Season Review
2014 North Atlantic Hurricane Season Review WHITEPAPER Executive Summary The 2014 Atlantic hurricane season was a quiet season, closing with eight 2014 marks the named storms, six hurricanes, and two major hurricanes (Category 3 or longest period on stronger). record – nine Forecast groups predicted that the formation of El Niño and below consecutive years average sea surface temperatures (SSTs) in the Atlantic Main – that no major Development Region (MDR)1 through the season would inhibit hurricanes made development in 2014, leading to a below average season. While 2014 landfall over the was indeed quiet, these predictions didn’t materialize. U.S. The scientific community has attributed the low activity in 2014 to a number of oceanic and atmospheric conditions, predominantly anomalously low Atlantic mid-level moisture, anomalously high tropical Atlantic subsidence (sinking air) in the Main Development Region (MDR), and strong wind shear across the Caribbean. Tropical cyclone activity in the North Atlantic basin was also influenced by below average activity in the 2014 West African monsoon season, which suppressed the development of African easterly winds. The year 2014 marks the longest period on record – nine consecutive years since Hurricane Wilma in 2005 – that no major hurricanes made landfall over the U.S., and also the ninth consecutive year that no hurricane made landfall over the coastline of Florida. The U.S. experienced only one landfalling hurricane in 2014, Hurricane Arthur. Arthur made landfall over the Outer Banks of North Carolina as a Category 2 hurricane on July 4, causing minor damage. While Mexico and Central America were impacted by two landfalling storms and the Caribbean by three, Bermuda suffered the most substantial damage due to landfalling storms in 2014.Hurricane Fay and Major Hurricane Gonzalo made landfall on the island within a week of each other, on October 12 and October 18, respectively. -
Hurricane and Tropical Storm
State of New Jersey 2014 Hazard Mitigation Plan Section 5. Risk Assessment 5.8 Hurricane and Tropical Storm 2014 Plan Update Changes The 2014 Plan Update includes tropical storms, hurricanes and storm surge in this hazard profile. In the 2011 HMP, storm surge was included in the flood hazard. The hazard profile has been significantly enhanced to include a detailed hazard description, location, extent, previous occurrences, probability of future occurrence, severity, warning time and secondary impacts. New and updated data and figures from ONJSC are incorporated. New and updated figures from other federal and state agencies are incorporated. Potential change in climate and its impacts on the flood hazard are discussed. The vulnerability assessment now directly follows the hazard profile. An exposure analysis of the population, general building stock, State-owned and leased buildings, critical facilities and infrastructure was conducted using best available SLOSH and storm surge data. Environmental impacts is a new subsection. 5.8.1 Profile 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 (National Oceanic and Atmospheric Administration [NOAA] 2013a). 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. -
Caribbean Hurricanes
YEMEN - COMPLEX EMERGENCY FACT SHEET #7, FISCAL YEAR (FY) 2016 JANUARY 1, 2016 CARIBBEAN – HURRICANES FACT SHEET #2, FISCAL YEAR (FY) 2017 SEPTEMBER 8, 2017 NUMBERS AT HIGHLIGHTS HUMANITARIAN FUNDING A GLANCE FOR THE HURRICANE IRMA RESPONSE Hurricane Irma remains a significant IN FY 2017 threat to The Bahamas, while Hurricane USAID/OFDA1 $200,000 155 mph Jose may exacerbate the situation on the island of Barbuda, which sustained Sustained Wind Speed of widespread damage from the passage of Hurricane Irma $200,000 NHC – September 8, 2017 Hurricane Irma USAID/OFDA is providing $200,000 to address hurricane-related needs in Up to 20 Antigua and Barbuda and The Bahamas feet Assessments of hurricane-affected areas of Hispaniola have commenced, with Potential Storm Surge in The Bahamas from initial reports suggesting less damage Hurricane Irma than expected NHC – September 8, 2017 Up to 20 KEY DEVELOPMENTS The National Hurricane Center (NHC) anticipates that Hurricane Irma will affect The inches Bahamas through September 9 as the storm continues tracking northwestward across the Anticipated Rainfall in northern Caribbean. The storm is bringing sustained winds of nearly 160 miles per hour Isolated Areas of (mph), storm surge of up to 20 feet, and 10–15 inches of rain to The Bahamas, according The Bahamas from Hurricane Irma to NHC forecasts. NHC – September 8, 2017 Hurricane Irma had passed north of Hispaniola as of September 8, and initial reports indicate some localized flooding along the northern coast of Haiti, although overall damage appears less than expected given the intensity of the hurricane. The Government 150 mph of Haiti and humanitarian organizations have commenced damage assessments of Sustained Wind Speed of storm-affected areas. -
10R.3 the Tornado Outbreak Across the North Florida Panhandle in Association with Hurricane Ivan
10R.3 The Tornado Outbreak across the North Florida Panhandle in association with Hurricane Ivan Andrew I. Watson* Michael A. Jamski T.J. Turnage NOAA/National Weather Service Tallahassee, Florida Joshua R.Bowen Meteorology Department Florida State University Tallahassee, Florida Jason C. Kelley WJHG-TV Panama City, Florida 1. INTRODUCTION their mobile homes were destroyed near Blountstown, Florida. Hurricane Ivan made landfall early on the morning of 16 September 2004, just west of Overall, there were 24 tornadoes reported Gulf Shores, Alabama as a category 3 across the National Weather Service (NWS) hurricane on the Saffir-Simpson Hurricane Tallahassee forecast area. The office issued Scale. Approximately 117 tornadoes were 130 tornado warnings from the afternoon of 15 reported associated with Ivan across the September until just after daybreak on 16 southeast United States. Eight people were September. killed and 17 were injured by tornadoes (Storm Data 2004; Stewart 2004). The most The paper examines the convective cells significant tornadoes occurred as hurricane within the rain bands of hurricane Ivan, which Ivan approached the Florida Gulf coast on the produced these tornadoes across the Florida afternoon and evening of 15 September. Panhandle, Big Bend, and southwest Georgia. The structure of the tornadic and non-tornadic The intense outer rain bands of Ivan supercells is examined for clues on how to produced numerous supercells over portions better warn for these types of storms. This of the Florida Panhandle, Big Bend, southwest study will focus on the short-term predictability Georgia, and Gulf coastal waters. In turn, of these dangerous storms, and will these supercells spawned dozens of investigate the problem of how to reduce the tornadoes. -
And Hurricane Michael (2018)
This work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law. Access to this work was provided by the University of Maryland, Baltimore County (UMBC) ScholarWorks@UMBC digital repository on the Maryland Shared Open Access (MD-SOAR) platform. Please provide feedback Please support the ScholarWorks@UMBC repository by emailing [email protected] and telling us what having access to this work means to you and why it’s important to you. Thank you. atmosphere Article Understanding the Role of Mean and Eddy Momentum Transport in the Rapid Intensification of Hurricane Irma (2017) and Hurricane Michael (2018) Alrick Green 1, Sundararaman G. Gopalakrishnan 2, Ghassan J. Alaka, Jr. 2 and Sen Chiao 3,* 1 Atmospheric Physics, University of Maryland, Baltimore County, Baltimore, MD 21250, USA; [email protected] 2 Hurricane Research Division, NOAA/AOML, Miami, FL 33149, USA; [email protected] (S.G.G.); [email protected] (G.J.A.) 3 Department of Meteorology and Climate Science, San Jose State University, San Jose, CA 95192, USA * Correspondence: [email protected]; Tel.: +1-408-924-5204 Abstract: The prediction of rapid intensification (RI) in tropical cyclones (TCs) is a challenging problem. In this study, the RI process and factors contributing to it are compared for two TCs: an axis-symmetric case (Hurricane Irma, 2017) and an asymmetric case (Hurricane Michael, 2018). -
Hurricane Irma-ENG-20170910.Pdf
The Caribbean: Hurricane Irma Situation Report No. 4 (as of 10 September 2017) This report is produced by OCHA ROLAC in collaboration with humanitarian partners. It covers the first period from 06 to 10 September, 2017. The next report will be issued on or around 12 September 2017. Highlights • Irma hit Cuba as the first category 5 hurricane to make landfall in the country since 1924, causing massive destruction and widespread flooding along its northern coast. • Irma upgraded to a category 4 hurricane as it pummeled Florida state in US on 10 September has left three people dead. • Most of the Caribbean islands battered by Irma were spared by Hurricane Jose. • People of Turks and Caicos are in urgent need of emergency relief. • Livelihoods, housing and infrastructure in Anguilla, Barbuda, the British Virgin Islands, St. Martin/St. Maartin, the US Virgin Islands, and Turks and Caicos are severely affected. • Reports of extensive damage to agriculture are coming in from Haiti and Cuba. • The number of dead and missing is expected to rise as communications and access are gradually restored across the Caribbean. • Several organizations and Governments are deploying pre-positioned teams and supplies and Evacuations in Barbuda on 08 September / UN Assessment team in Antigua assessments have begun in some areas. and Barbuda 25 34,000 17,000 1.2 million people reported dead people displaced in the people in need of people affected by damage across affected territories. Dominican Republic and immediate shelter across to water infrastructure in Haiti the affected eastern the affected areas of the Caribbean islands Dominican Republic Situation Overview Most of the smaller Caribbean islands which faced the onslaught of Irma were spared by Hurricane Jose. -
Fishing Pier Design Guidance Part 1
Fishing Pier Design Guidance Part 1: Historical Pier Damage in Florida Ralph R. Clark Florida Department of Environmental Protection Bureau of Beaches and Coastal Systems May 2010 Table of Contents Foreword............................................................................................................................. i Table of Contents ............................................................................................................... ii Chapter 1 – Introduction................................................................................................... 1 Chapter 2 – Ocean and Gulf Pier Damages in Florida................................................... 4 Chapter 3 – Three Major Hurricanes of the Late 1970’s............................................... 6 September 23, 1975 – Hurricane Eloise ...................................................................... 6 September 3, 1979 – Hurricane David ........................................................................ 6 September 13, 1979 – Hurricane Frederic.................................................................. 7 Chapter 4 – Two Hurricanes and Four Storms of the 1980’s........................................ 8 June 18, 1982 – No Name Storm.................................................................................. 8 November 21-24, 1984 – Thanksgiving Storm............................................................ 8 August 30-September 1, 1985 – Hurricane Elena ...................................................... 9 October 31,