Long-Term Development in Post-Disaster Intentional Communities in Honduras
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Part 1-B Cause & Impact of Landfalling Tropical Cyclone
Part 1-b Cause & Impact of Landfalling Tropical Cyclone Rainfall & River Flooding • In addition to high winds & storm surge, all tropical storms can produce torrential rains causing massive flooding & trigger landslides and debris floods • Catastrophic flash flooding may occur as a result of intense rainfall over a relatively short duration. Longer duration storms, say a few days, can be equally devastating. 2 River flooding associated with heavy rainfall from tropical cyclones Flood stages & inundation maps • Rain-triggered flooding is not confined to coastal areas. The reach of a large tropical storm can cause flooding well inland, especially along the estuaries. • Beneficial contributions of tropical cyclones: rainfall for needed water supply in the region; and maintenance of global heat balance 5 Cases of landfalling of catastrophic tropical cyclones • Hurricane Andrew , August 24, 1993- Florida • Hurricane Allison , June 5-9, 2001- Houston and TX and LA coasts • Hurricane Katrina , Aug 29, 2005- New Orleans & LA and TX coasts • Hurricane Mitch , Oct 26- Nov 5, Honduras, Salvador, Nicaragua, and Guatemala • Typhoon Morakot , August 3-10, 2009, Taiwan • Typhoon Ketsana , Sept 23-30, 2009, Manila, Philippine , Vietnam & Cambodia 6 Hurricane Andrew (Aug24,1993) 7 Hurricane Andrew (Aug24,1993) Source: Report on Hurricane Andrew Storm Summary & Impacts on Florida Beaches, by USACE & Florida DNR, May 1993 Pressure zones, wind zones and storm surge contour 9 Surge at landfall & waves height Storm surges Wave Heights 10 Impact of gusts on homes 11 Impacts on beaches of Florida 12 Erosion and accretion of beach profiles 13 Hurricane Allison, June 5-9, 2001 * Hurricane Allison’s swath of rainfall – 25-50 cm or more rainfall in coastal TX & LA for nearly 6 days. -
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. -
NOAA Technical Memorandum NWS HYDR0-20 STORM TIDE
NOAA Technical Memorandum NWS HYDR0-20 STORM TIDE FREQUENCY ANALYSIS FOR THE GULF COAST OF FLORIDA FROM CAPE SAN BLAS TO ST. PETERSBURG BEACH Francis P. Ho and Robert J. Tracey Office of Hydrology Silver Spring, Md. April 1975 UNITED STATES /NATIONAL OCEANIC AND / National Weather DEPARTMENT OF COMMERCE ATMOSPHERIC ADMINISTRATION Service Frederick B. Dent, Secretar1 Robert M. White, Administrator George P, Cressman, Director CONTENTS 1. Introduction. • • • • • • • 1 1.1 Objective and scope •• 1 1.2 Authorization •• 1 1.3 Study method •• 2 2. Summary of historical hurricanes •• 2 2.1 Hurricane tracks 2 2.2 Historical notes 3 3. Climatology of hurricane characteristics. 8 3.1 Frequency of hurricane tracks •••. 8 3.2 Probability distribution of hurricane intensity. 8 3.3 Probability distribution of radius of maximum winds. 9 3.4 Probability distribution of speed and direction of forward motion • . • • • • • • • • 9 4. Hurricane surge • • • • 9 4.1 Surge model ••• 9 4.2 Shoaling factor •• 10 5. Tide frequency analysis by joint probability method • 10 5.1 The joint probability method • 10 5.2 Astronomical tides •••••• 11 5.2.1 Reference datum •.•••• 11 Table 1. Tropical storm parameters - Clearwater, Fla 12 Table 2. Tropical storm parameters - Bayport, Fla •• 13 Table 3. Tropical storm parameters - Cedar Key, Fla. 14 Table 4. Tropical storm parameters- Rock ·Islands, Fla .. 15 Table 5. Tropical storm parameters - Carrabelle, Fla • 16 Table 6. Tropical storm parameters - Apalachicola, Fla 17 5.2.2 Astronomical tide • • • •.• 19 5.3 Prestorm water level ••••••. 19 5.4 Tide frequencies • • • • . • ••• 19 5.5 Adjustment along coast ••••••.•••.•••. 19 5.6 Comparison of frequency curves with observed tides and high-water marks • • • • • • • • • • • . -
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 -
Letter from the Government of Honduras on Actions Taken
Appendix 13 – Letter from the Government of Honduras on actions taken OFFICIAL LETTER No.1077-DGPE/DSM-10 Tegucigalpa, June 4, 2010 Excellency, It is my honor to present my compliments and to say that the purpose of this letter in follow- up to the two notes sent to the international community in April 2010 is to express our desire for genuine understanding of the situation in our country and that the international community be suitably and correctly informed of the efforts of the Government of Honduras to implement a real process of national unity and reconciliation. I should begin by drawing attention to the fact that our president, Mr. Porfirio Lobo Sosa, has set about the task of leading the country with the strength afforded him by the legitimacy of a transparent election extensively observed by the international community, in which the majority of the people of Honduras clearly, lawfully, and unmistakably expressed their will in the search for peace, stability, and restored unity. This electoral process, called by the Supreme Electoral Tribunal under the administration of former President Zelaya Rosales, was preceded by the primary elections in which all legally registered political parties chose their candidates to the National Congress, Municipalities, and the Presidency of the Republic, a process monitored by international observers—including those from the Organization of American States (OAS)—who noted the transparency and success thereof. I am at pains to draw your attention to the fact that Article 51 of the Constitution of Honduras defines the Supreme Electoral Tribunal as an autonomous and independent entity responsible for the convocation, organization, direction, and supervision of electoral processes. -
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. -
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 -
Tropical Cyclone Effects on California
/ i' NOAA Technical Memorandum NWS WR-~ 1s-? TROPICAL CYCLONE EFFECTS ON CALIFORNIA Salt Lake City, Utah October 1980 u.s. DEPARTMENT OF I National Oceanic and National Weather COMMERCE Atmospheric Administration I Service NOAA TECHNICAL ME~RANOA National Weather Service, Western R@(Jfon Suhseries The National Weather Service (NWS~ Western Rl!qion (WR) Sub5eries provide! an informal medium for the documentation and nUlck disseminuion of l"'eSUlts not appr-opriate. or nnt yet readY. for formal publication. The series is used to report an work in pronf"'!ss. to rie-tJ:cribe tl!1:hnical procedures and oractice'S, or to relate proqre5 s to a Hmitfd audience. The~J:e Technical ~ranc1i!l will report on investiqations rit'vot~ or'imaroi ly to rl!nionaJ and local orablems of interest mainly to personnel, "'"d • f,. nence wUl not hi! 'l!lidely distributed. Pacer<; I to Z5 are in the fanner series, ESSA Technical Hetooranda, Western Reqion Technical ~-··•nda (WRTMI· naoors 24 tn 59 are i·n the fanner series, ESSA Technical ~-rando, W.othel" Bureou Technical ~-randa (WSTMI. aeqinniM with "n. the oaoers are oa"t of the series. ltOAA Technical >4emoranda NWS. Out·of·print .....,rond1 are not listed. PanfiM ( tn 22, except for 5 {revised erlitinn), ar'l! availabll! froM tt'lt Nationm1 Weattuu• Service Wesurn Ret1inn. )cientific ~•,.,irr• Division, P.O. Box lllAA, Federal RuildiM, 125 South State Street, Salt La~• City, Utah R4147. Pacer 5 (revised •rlitinnl. and all nthei"S beqinninq ~ith 25 are available from the National rechnical Information Sel'"lice. II.S. -
Plh Partido Liberal De Honduras
Partis Politiques PLH PARTIDO LIBERAL DE HONDURAS Données clés Date de création : 5 février 1891. Positionnement idéologique actuel : Libéral, de centre-droit à centre-gauche. Le manque de cohésion idéologique et la forte fragmentation interne rendent le positionnement flou. Affiliations internationales : Membre de l’Internationale libérale et de la COPPPAL (Conférence Permanente des Partis Politiques d’Amérique Latine et des Caraïbes). Implantations territoriales : Mobilisation des zones urbaines principalement. Le parti compte 31 bastions, situés dans l’ouest du pays et a l’avantage dans environ 61 autres municipalités plus au centre, à tendance abstentionniste. Principaux dirigeants : Roberto Michelleti Bain (Président du parti), Ernesto Elvin Santos Lozano (Vice- président), Bill O’Neill Santos Brito (Secrétaire Général), Eduardo Antonio Bueso (Secrétaire des Finances). Mode de désignation des dirigeants : Le Président du Conseil National Exécutif, son Vice-président et les secrétaires sont choisis lors des élections primaires par un vote direct, secret et selon le principe de proportionnalité. Mode de désignation des candidats : Les candidats à la Présidence et la Vice-présidence sont choisis lors d’élections internes ouvertes. Périodes au gouvernement : 1957-1963, 1982-1986, 1986-1990, 1994-1998, 1998-2002, 2006-2010. ________________________________________________________ Résultats électoraux (29 novembre 2009) Elections présidentielles Elections législatives Candidats Nombre de Parti politique Votes % Parti politique présidentiels -
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. -
The Case Against Roberto Micheletti Baín
Parents of Assassinated Activist sue Honduran Coup Leader: The Case against Roberto Micheletti Baín HONDURAS AND THE COUP aftermath have not been called to account for their actions. On June 28, 2009, the Honduran military kidnapped and forcibly exiled President Zelaya in a coup d’etat. The MURILLO V. MICHELETTI BAÍN coup against President Zelaya was universally condemned by the United Nations, the European On June 23, 2011, Union, the Organization of American States, the Inter- the Center for American Commission on Human Rights, and Constitutional numerous governments around the world, including Rights (CCR) filed that of the United States. a complaint in the Houston Division COUP OPPOSITION & THE KILLING OF ISIS of the Southern MURILLO District of Texas, on behalf of On July 5, 2009, President Zelaya attempted to return David Murillo and to Honduras and restore the democratically-elected Silvia Mencías, the government. Zelaya intended to return by airplane and parents of Isis land at Toncontin International Airport in the capital Obed Murillo. Silvia Mencías, the mother of Isis Obed of Tegucigalpa, although the self-declared interim Murillo, holds a photograph of her son. The defendant is government under de facto President Roberto Roberto Micheletti Baín, former president of the Micheletti Bain said it would not allow him to return. Honduran National Congress who assumed the role of Nineteen-year-old Isis Obed Murillo and his family head of the de facto government immediately joined thousands of other coup opponents at the following the coup d’etat ousting President Zelaya, and airport for a non-violent, peaceful gathering to acted as such until January 27, 2010. -
The Geography of Fishing in British Honduras and Adjacent Coastal Areas
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1966 The Geography of Fishing in British Honduras and Adjacent Coastal Areas. Alan Knowlton Craig Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Craig, Alan Knowlton, "The Geography of Fishing in British Honduras and Adjacent Coastal Areas." (1966). LSU Historical Dissertations and Theses. 1117. https://digitalcommons.lsu.edu/gradschool_disstheses/1117 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. This dissertation has been „ . „ i i>i j ■ m 66—6437 microfilmed exactly as received CRAIG, Alan Knowlton, 1930— THE GEOGRAPHY OF FISHING IN BRITISH HONDURAS AND ADJACENT COASTAL AREAS. Louisiana State University, Ph.D., 1966 G eo g rap h y University Microfilms, Inc., Ann Arbor, Michigan THE GEOGRAPHY OP FISHING IN BRITISH HONDURAS AND ADJACENT COASTAL AREAS A Dissertation Submitted to the Graduate Faculty of the Louisiana State university and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Geography and Anthropology by Alan Knowlton Craig B.S., Louisiana State university, 1958 January, 1966 PLEASE NOTE* Map pages and Plate pages are not original copy. They tend to "curl". Filmed in the best way possible. University Microfilms, Inc. AC KNQWLEDGMENTS The extent to which the objectives of this study have been acomplished is due in large part to the faithful work of Tiburcio Badillo, fisherman and carpenter of Cay Caulker Village, British Honduras.