The 2005 Atlantic Hurricane Season Is the Most Active on Record
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Town of East Haven Hazard Mitigation Plan Update 2012
TOWN OF EAST HAVEN HAZARD MITIGATION PLAN UPDATE 2012 ADOPTED MAY 1, 2012 MMI #2731-02-1 Prepared for: TOWN OF EAST HAVEN Town Hall 200 Main Street East Haven, Connecticut 06512 (203)468–3840 http://www.townofeasthavenct.org/ Prepared by: MILONE & MACBROOM, INC. 99 Realty Drive Cheshire, Connecticut 06410 (203) 271-1773 www.miloneandmacbroom.com TABLE OF CONTENTS Section Page CONTACT INFORMATION ....................................................................................................ES-1 EXECUTIVE SUMMARY .......................................................................................................ES-2 1.0 INTRODUCTION 1.1 Background and Purpose ................................................................................................. 1-1 1.2 Hazard Mitigation Goals .................................................................................................. 1-4 1.3 Identification of Hazards and Document Overview ........................................................ 1-5 1.4 Discussion of STAPLEE Ranking Method.................................................................... 1-10 1.5 Discussion of Benefit-Cost Ratio................................................................................... 1-12 1.6 Documentation of the Planning Process ........................................................................ 1-12 1.7 Coordination with Neighboring Communities ............................................................... 1-12 2.0 COMMUNITY PROFILE 2.1 Physical Setting ............................................................................................................... -
Climatology, Variability, and Return Periods of Tropical Cyclone Strikes in the Northeastern and Central Pacific Ab Sins Nicholas S
Louisiana State University LSU Digital Commons LSU Master's Theses Graduate School March 2019 Climatology, Variability, and Return Periods of Tropical Cyclone Strikes in the Northeastern and Central Pacific aB sins Nicholas S. Grondin Louisiana State University, [email protected] Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_theses Part of the Climate Commons, Meteorology Commons, and the Physical and Environmental Geography Commons Recommended Citation Grondin, Nicholas S., "Climatology, Variability, and Return Periods of Tropical Cyclone Strikes in the Northeastern and Central Pacific asinB s" (2019). LSU Master's Theses. 4864. https://digitalcommons.lsu.edu/gradschool_theses/4864 This Thesis 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 Master's Theses by an authorized graduate school editor of LSU Digital Commons. For more information, please contact [email protected]. CLIMATOLOGY, VARIABILITY, AND RETURN PERIODS OF TROPICAL CYCLONE STRIKES IN THE NORTHEASTERN AND CENTRAL PACIFIC BASINS A Thesis 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 Master of Science in The Department of Geography and Anthropology by Nicholas S. Grondin B.S. Meteorology, University of South Alabama, 2016 May 2019 Dedication This thesis is dedicated to my family, especially mom, Mim and Pop, for their love and encouragement every step of the way. This thesis is dedicated to my friends and fraternity brothers, especially Dillon, Sarah, Clay, and Courtney, for their friendship and support. This thesis is dedicated to all of my teachers and college professors, especially Mrs. -
CENTRAL AMERICA: Disaster Management Is Key Challenge
http://search.proquest.com.libproxy.nps.edu/printviewfile?accountid=12702 Back to previous page document 1 of 1 CENTRAL AMERICA: Disaster management is key challenge OxResearch Daily Brief Service. (Dec 31, 2014). Find a copy http://sfxhosted.exlibrisgroup.com/nps?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:book& genre=unknown&sid=ProQ:OxResearch&atitle=& title=CENTRAL+AMERICA%3A+Disaster+management+is+key+challenge&issn=&date=2014-12-31&volume=& issue=&spage=1&au=&isbn=&jtitle=& btitle=CENTRAL+AMERICA%3A+Disaster+management+is+key+challenge&rft_id=info:eric/&rft_id=info:doi/ Abstract Disaster preparedness in Central America. In recent months, Central American countries have been boosting regional cooperation for the enhancement of security strategies in response to the increase in child migration through the region en route to the United States. Less high-profile regional efforts are also being made in the area of emergency preparedness in this disaster-prone region. Full Text SUBJECT:Disaster preparedness in Central America. SIGNIFICANCE:In recent months, Central American countries have been boosting regional cooperation for the enhancement of security strategies in response to the increase in child migration through the region en route to the United States. Less high-profile regional efforts are also being made in the area of emergency preparedness in this disaster-prone region. ANALYSIS: Impacts. The United States will continue to support training exercises, as natural disasters increase regional vulnerability, thus driving migration. 1 of 6 12/13/2015 4:07 PM http://search.proquest.com.libproxy.nps.edu/printviewfile?accountid=12702 Long-term urban planning will remain a key factor in the reduction of the impact of natural disasters in the region. -
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. -
Eastern North Pacific Hurricane Season of 1995
1152 MONTHLY WEATHER REVIEW VOLUME 126 Eastern North Paci®c Hurricane Season of 1995 EDWARD N. RAPPAPORT,LIXION A. AVILA,MILES B. LAWRENCE,MAX MAYFIELD, AND RICHARD J. PASCH National Hurricane Center, Tropical Prediction Center, NWS/NOAA, Miami, Florida (Manuscript received 3 September 1996, in ®nal form 28 January 1997) ABSTRACT The 1995 eastern North Paci®c hurricane season is reviewed. The activity comprised 11 tropical cyclones, consisting of seven hurricanes, three tropical storms, and one tropical depression. Hurricane Ismael caused a large loss of life in the southern Gulf of California. 1. Introduction gion. This pattern is also consistent with fewer than normal storms forming in the Paci®c and enhanced ac- The western hemisphere was a scene of stark contrasts tivity over the western Caribbean region (cf. Lawrence in tropical cyclone activity during 1995. More tropical et al. 1998). cyclones formed in the Atlantic hurricane basin than in In contrast to these atmospheric features, anomalies the eastern North Paci®c Ocean for the ®rst time in 26 of sea surface temperature (not shown) were small and years (cf. Lawrence et al. 1998). In fact, while the At- thought to be insigni®cant. In fact, when atmospheric lantic produced 19 tropical storms, its second largest conditions were conducive for development, the warm total during the past 125 years, the total of 10 tropical eastern Paci®c waters allowed three of the 10 tropical storms in the eastern North Paci®c Ocean ranks as the storms to strengthen to category 4 status on the Saf®r± second fewest in the 30-yr period of routine satellite Simpson hurricane scale (1-min wind speeds exceeding surveillance (1977 had 8 storms) and is 6 fewer than about 58 m s21). -
1989 Hurricane Hugo - September 1989
1989 Hurricane Hugo - September 1989. Category 4 hurricane devastates SC and NC with ~ 20 foot storm surge and severe wind damage after hitting PR and the U.S. Virgin Islands; over $9.0 (13.9) billion (about $7.1 (10.9) billion in Carolinas); 86 deaths (57--U.S. mainland, 29--U.S. Islands). Hurricane Hugo was a powerful Cape Verde hurricane that caused widespread damage and loss of life in Guadeloupe, Saint Croix, Puerto Rico, and the Southeast United States. It formed over the eastern Atlantic near the Cape Verde Islands on September 9, 1989. Hugo moved thousands of miles across the Atlantic, rapidly strengthening to briefly attain category 5 hurricane strength on its journey. It later crossed over Guadeloupe and St. Croix on September 17 and 18 as a category 4 hurricane. Weakening slightly more, it passed over Puerto Rico as a strong category 3 hurricane. Further weakening occurred several hours after re-emerging into the Atlantic, becoming downgraded to a category 2 hurricane. However, it re-strengthened into a category 4 hurricane before making landfall just slightly north of Charleston, on Isle of Palms on September 22 with 140 mph sustained winds (gusts to more than 160 mph). It had devolved to a remnant low near Lake Erie by the next day. As of 2016, Hurricane Hugo is the most intense tropical cyclone to strike the East Coast north of Florida since 1898. Hurricane Hugo caused 34 fatalities (most by electrocution or drowning) in the Caribbean and 27 in South Carolina, left nearly 100,000 homeless, and resulted in $9.47 billion (1989 USD) in damage overall, making it the most damaging hurricane ever recorded at the time. -
NCAR Annual Scientific Report Fiscal Year 1985 - Link Page Next PART0002
National Center for Atmospheric Research Annual Scientific Report Fiscal Year 1985 Submitted to National Science Foundation by University Corporation for Atmospheric Research March 1986 iii CONTENTS INTRODUCTION ............... ............................................. v ATMOSPHERIC ANALYSIS AND PREDICTION DIVISION ............... 1 Significant Accomplishments........................ 1 AAP Division Office................................................ 4 Mesoscale Research Section . ........................................ 8 Climate Section........................................ 15 Large-Scale Dynamics Section....................................... 22 Oceanography Section. .......................... 28 ATMOSPHERIC CHEMISTRY DIVISION................................. .. 37 Significant Accompl i shments........................................ 38 Precipitation Chemistry, Reactive Gases, and Aerosols Section. ..................................39 Atmospheric Gas Measurements Section............................... 46 Global Observations, Modeling, and Optical Techniques Section.............................. 52 Support Section.................................................... 57 Di rector' s Office. * . ...... .......... .. .. ** 58 HIGH ALTITUDE OBSERVATORYY .. .................. ............... 63 Significant Accomplishments .......... .............................. 63 Coronal/Interplanetary Physics Section ....................... 64 Solar Variability and Terrestrial Interactions Section........................................... 72 Solar -
BARBARA (EP022019) 30 June – 5 July 2019
NATIONAL HURRICANE CENTER TROPICAL CYCLONE REPORT HURRICANE BARBARA (EP022019) 30 June – 5 July 2019 John P. Cangialosi National Hurricane Center 25 August 2019 VISIBLE SATELLITE MODIS IMAGE OF HURRICANE BARBARA AROUND THE TIME OF ITS PEAK INTENSITY. IMAGE COURTSEY OF NASA. Barbara was a category 4 hurricane (on the Saffir-Simpson Hurricane Wind Scale) that rapidly intensified and remained out at sea. The hurricane then rapidly weakened and became a post-tropical cyclone just east of the central North Pacific basin. Hurricane Barbara 2 Hurricane Barbara 30 JUNE – 5 JULY 2019 SYNOPTIC HISTORY The genesis of Barbara appears to be associated with a tropical wave that moved off the west coast of Africa on 18 June. This disturbance produced disorganized deep convection while it was travelling across the Atlantic Ocean, especially when it interacted with an upper-level trough near the Lesser Antilles on 22 and 23 June. Showers and thunderstorms remained disorganized near the wave axis as it entered the far eastern North Pacific basin on 26 June, but the convective activity gradually increased during the next couple of days while the disturbance passed well south of Mexico. Environmental low-level southwesterly flow helped the wave establish a broad circulation on 29 June. Deep convection continued to increase later that day, and the system developed a well-defined center by 0600 UTC 30 June, marking the formation of a tropical cyclone about 550 n mi south-southwest of Manzanillo, Mexico. Since scatterometer data indicated that winds were already near 35 kt, tropical storm status is shown at the time of genesis. -
Trabing Commons Library Res
Analysis of Hurricanes Using Long-Range Lightning Detection Networks BENJAMIN TRABING University of Oklahoma/NSSL, Norman, OK JOHN A. KNAFF NOAA Center for Satellite Applications and Research, Fort Collins, CO ANDREA SCHUMACHER AND KATE MUSGRAVE CIRA/ Colorado State University, Fort Collins, CO MARK DEMARIA NWS/National Hurricane Center, Miami, FL * Corresponding Author: Benjamin Trabing, University of Oklahoma/NSSL, 120 David L. Boren Blvd., Suite 5900, Norman, OK 73072, [email protected] Abstract The new GOES-R satellite will be equipped with the Geostationary Lightning Mapper (GLM) that will provide unprecedented total lightning data with the potential to improve hurricane intensity forecasts. Past studies have provided conflicting interpretations of the role that lightning plays in forecasting tropical cyclone (TC) intensity changes. With the goal of improving the usefulness of total lightning, detailed case studies were conducted of five TCs that underwent rapid intensification (RI) within the domains of two unique ground-based long-range lightning detection networks, the World Wide Lightning Location Network (WWLLN) and Earth Networks Total Lightning Network (ENTLN). This analysis will provide greater details of the distribution of lightning within predefined storm features to highlight specific phenomena that large statistical studies cannot resolve. Both WWLLN and ENTLN datasets showed similar spatial and temporal patterns in lightning that validates the independent use of either network for analysis. For the cases examined, a maxima in eyewall lightning was located downshear and in the front-right quadrants relative to storm motion. Results show that RI follows a burst of lightning in the eyewall when coinciding with a period of little environmental vertical shear. -
United Nations Environment Program Terminal Evaluation Of
United Nations Environment Program Terminal Evaluation of Mainstreaming the conservation of ecosystem services and biodiversity at the sub-watershed scale in Chiapas, Mexico By Robert Hofstede Evaluation Office November 2014 TABLE OF CONTENTS EXECUTIVE SUMMARY .......................................................................................................... 1 ABBREVIATIONS ...................................................................................................................... 5 I. INTRODUCTION .................................................................................................................... 6 II. THE EVALUATION .............................................................................................................. 6 III. THE PROJECT ..................................................................................................................... 7 A. PROJECT CONTEXT ..................................................................................................... 7 B. OBJECTIVES AND COMPONENTS.............................................................................. 8 C. TARGET AREAS/GROUPS ............................................................................................ 9 D. MILESTONES/KEY DATES IN PROJECT DESIGN AND IMPLEMENTATION..... 9 E. IMPLEMENTATION ARRANGEMENTS ....................................................................10 F. PROJECT FINANCING ..................................................................................................10 G. PROJECT -
BARBARA (EP022013) 28 – 30 May 2013
NATIONAL HURRICANE CENTER TROPICAL CYCLONE REPORT HURRICANE BARBARA (EP022013) 28 – 30 May 2013 Daniel P. Brown National Hurricane Center 1 19 August 2013 GOES 14 SATELLITE IMAGE OF HURRICANE BARBARA AT 1815 UTC 29 MAY, NEAR THE TIME OF LANDFALL IN SOUTHERN MEXICO. IMAGE COURTESY OF THE NOAA ENVIRONMENTAL VISUALIZATION LABORATORY. Barbara was an early season category 1 hurricane (on the Saffir-Simpson Hurricane Wind Scale) that made landfall along the Pacific coast of southeastern Mexico. Barbara’s landfall location is the easternmost recorded landfall point for an eastern North Pacific hurricane. Barbara’s landfall date of 29 May marks the second-earliest hurricane landfall date in the basin since records began in 1949. 1 Original report date 6 August 2013. Corrected for tropical cyclone status in Table 1 and Figure 1. Hurricane Barbara 2 Hurricane Barbara 28 – 30 MAY 2013 SYNOPTIC HISTORY Barbara appears to have formed from the interaction of a tropical wave with an eastward-moving atmospheric Kelvin wave during an active period of the Madden-Julian Oscillation (Fig.1 ). Satellite data suggest that the low-amplitude tropical wave departed the west coast of Africa on 16 May and crossed Central America on 24 May. The wave moved over the far eastern Pacific Ocean shortly thereafter, and a broad low pressure area formed southwest of the coast of Nicaragua on 25 May after the atmospheric Kelvin wave passed the longitude of the disturbance (Fig. 1). The broad low moved west-northwestward during the next few days while the associated shower and thunderstorm activity gradually increased. Early on 28 May, the circulation became better defined, which resulted in the formation of a tropical depression by 1200 UTC, about 110 n mi south-southeast of Puerto Angel, Mexico. -
Natural Catastrophes and Man-Made Disasters in 2013
No 1/2014 Natural catastrophes and 01 Executive summary 02 Catastrophes in 2013 – man-made disasters in 2013: global overview large losses from floods and 07 Regional overview 15 Fostering climate hail; Haiyan hits the Philippines change resilience 25 Tables for reporting year 2013 45 Terms and selection criteria Executive summary Almost 26 000 people died in disasters In 2013, there were 308 disaster events, of which 150 were natural catastrophes in 2013. and 158 man-made. Almost 26 000 people lost their lives or went missing in the disasters. Typhoon Haiyan was the biggest Typhoon Haiyan struck the Philippines in November 2013, one of the strongest humanitarian catastrophe of the year. typhoons ever recorded worldwide. It killed around 7 500 people and left more than 4 million homeless. Haiyan was the largest humanitarian catastrophe of 2013. Next most extreme in terms of human cost was the June flooding in the Himalayan state of Uttarakhand in India, in which around 6 000 died. Economic losses from catastrophes The total economic losses from natural catastrophes and man-made disasters were worldwide were USD 140 billion in around USD 140 billion last year. That was down from USD 196 billion in 2012 2013. Asia had the highest losses. and well below the inflation-adjusted 10-year average of USD 190 billion. Asia was hardest hit, with the cyclones in the Pacific generating most economic losses. Weather events in North America and Europe caused most of the remainder. Insured losses amounted to USD 45 Insured losses were roughly USD 45 billion, down from USD 81 billion in 2012 and billion, driven by flooding and other below the inflation-adjusted average of USD 61 billion for the previous 10 years, weather-related events.