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Impacts of Global Warming on Hurricane-Related Flooding in Corpus Christi,Texas
Impacts of Global Warming on Hurricane-related Flooding in Corpus Christi, Texas Sea-level Rise and Flood Elevation A one-foot rise in flood elevation due to both sea-level rise and hurricane intensification leads to an inundation of 5000 –15,000 feet. Global Sea-level Rise Global warming causes sea level to rise through Limitations of the Analysis two major mechanisms. First, as water warms, it expands, taking up more space. Second, as ice This analysis looked only at damages due to flooding by storm on land melts (including mountain glaciers surge and sea-level rise. It is not a comprehensive analysis of the wide array of hurricane-related damages. Other simplifying around the world as well as the polar ice assumptions were made and there were limitations due to lack of sheets), this water flows to the oceans. data. For example, no data on historical flood damage to oil The thermal expansion of the oceans and the refineries was available to the researchers. melting of mountain glaciers are well understood. Increased melting and loss of ice on In addition, the study assumes that the barrier island retains its elevation and volume as sea level rises, though under high rates of parts of the polar ice sheets has recently been sea-level rise, the relative condition of the barrier island would be observed, especially on Greenland, although how expected to weaken, posing additional risk for erosion of the island much and how fast the ice sheets will increase and for flooding in the bay, both of which would increase economic sea-level rise is not well known, and this damages. -
Hurricane Info You Can Use- 2009
Since 1953, Atlantic tropical storms have been named from lists originated by the National Hurricane Center. They are now maintained and updated by an international committee of the World Meteorological Organization. The original name lists featured only women's names. In 1979, men's names were introduced and they alternate with the women's names. Six lists are used in rotation. Thus, the 2005 list will be used again in 2011. For more information about the history of naming hurricanes, log onto www.nhc.noaa.gov. The only time that there is a change in the list is if a storm is so deadly or costly that the future use of its name on a different storm would be inappropriate for reasons of sensitivity. If that occurs, then at an annual meeting by the WMO committee (called primarily to discuss many other issues) the name is stricken from the list and another name is selected to replace it. 2009 Names List Ana Bill Claudette Danny Erika Fred Grace Henri Ida Joaquin Kate Larry Mindy Nicholas Odette Peter Rose Sam Teresa Victor Wanda What is the National Hurricane Center? The National Hurricane Center (NHC) maintains a continuous watch on tropical cyclones over the Atlantic, Caribbean, Gulf of Mexico, and the Eastern Pacific from May 15th through November 30th. The Center prepares and distributes hurricane watches and warnings for the general public and also prepares and distributes marine and military advisories for other users. During the “off-season," NHC provides training for U.S. emergency managers and representatives from many other countries that are affected by tropical cyclones. -
45Th Anniversary of Hurricane Beulah
NWS Corpus Christi, TX Summer 2012 Edition 45th Anniversary of Hurricane Beulah Special points of John Metz — Warning Coordination Meteorologist interest: Severe Weather Season Beulah was the 2nd storm of the 2012 most active season in 1967 hurricane season in which there 25 years! were only 6 named storms. However Beulah left its mark on Texas history as All about the wildfire on the her slow storm motion produced record Padre Island National flooding and a prolific number of torna- Seashore does. Beulah was a long track storm, developing just east of the Leeward Is the Drought Improving? Islands in the Caribbean on Sept 5, 1967, intensifying rapidly into a hurricane the Find out how to become a Hurricane Beulah – September1967 next day. Beulah passed south of volunteer at the NWS WFO Hispaniola as a Category 4 hurricane with wind speeds of 150 mph. As she churned across Corpus Christi, TX the Caribbean, she weakened to a tropical storm while skirting south of Jamaica. But by the eleventh day she made her first direct impact, on the northern tip of the Yucatan Peninsula near Cozumel, as a Category 3 storm. She reemerged in the warm waters of the Gulf of Inside this issue: Mexico, becoming a powerful Category 5 storm, with sustained winds of 160 mph. Beulah finally moved ashore in Mexico, just south of Brownsville Texas on Sept 20, 1967. Maximum wind gusts were measured at 136 mph in Brownville producing a storm surge of Hurricane Beulah 1 18-20 feet north of where the center of the storm crossed the coast. -
Tornadoes Associated with Hurricane Beulah on September 19-23, 1967
July 1970 541 UDC 661.616.3:651.616.~~784)“1967.~.18-~”“BEOLAH” TORNADOES ASSOCIATED WITH HURRICANE BEULAH ON SEPTEMBER 19-23, 1967 ROBERT ORTON ESSA State Climatologist for Texas, Austin, Tex. ABSTRACT One hundred fifteen tornadoes are known to have occurred in association with humcane Beulah. The total was far greater than the number reported with any previous North Atlantic tropical cyclone in history. The spatial distribution of the tornadoes with reference to the hurricane center was examined, and it is shown that the best relationships on location of the hurricane-tornado within the parent cyclone are obtained with respect to true azimuth and are superior to those obtained using an orientation from a heading along the tropical cyclone track. With few exceptions, the tornadoes associated with hurricane Beulah occurred outside the area of known hurricane- force winds. The period of the day, the orientation of the Texas coastline in relation to the hurricane’s path, and the length of time Beulah lingered near the coast may have contributed to the record.numberof occurrences of hurricane- tornadoes. Unauthenticated | Downloaded 09/28/21 07:58 PM UTC 542 MONTHLY WEATHER REVIEW vel. 98, No. 7 hurricane Beulah for descriptive evidence of tornado occurrence. The daily September totals of tornadoes associated with hurricane Beulah are: the 19th, 5; 20th, 67; 21st, 21; 22d, 21; and 23d, 1. Of these, 79 occurred in the morning and 35 in the after- noon; for one tornado occurrence, the period of the day was not known. The location of each tornado, the time of occurrence when known, and other pertinent data concerning these storms are on file at the ESSA State Climatologist's of6ce. -
September Weather History for the 1St - 30Th
SEPTEMBER WEATHER HISTORY FOR THE 1ST - 30TH AccuWeather Site Address- http://forums.accuweather.com/index.php?showtopic=7074 West Henrico Co. - Glen Allen VA. Site Address- (Ref. AccWeather Weather History) -------------------------------------------------------------------------------------------------------- -------------------------------------------------------------------------------------------------------- AccuWeather.com Forums _ Your Weather Stories / Historical Storms _ Today in Weather History Posted by: BriSr Sep 1 2008, 11:37 AM September 1 MN History 1807 Earliest known comprehensive Minnesota weather record began near Pembina. The temperature at midday was 86 degrees and a "strong wind until sunset." 1894 The Great Hinckley Fire. Drought conditions started a massive fire that began near Mille Lacs and spread to the east. The firestorm destroyed Hinckley and Sandstone and burned a forest area the size of the Twin City Metropolitan Area. Smoke from the fires brought shipping on Lake Superior to a standstill. 1926 This was perhaps the most intense brief thunderstorm ever in downtown Minneapolis. 1.02 inches of rain fell in six minutes, starting at 2:59pm in the afternoon according to the Minneapolis Weather Bureau. The deluge, accompanied with winds of 42mph, caused visibility to be reduced to a few feet at times and stopped all streetcar and automobile traffic. At second and sixth street in downtown Minneapolis rushing water tore a manhole cover off and a geyser of water spouted 20 feet in the air. Hundreds of wooden paving blocks were uprooted and floated onto neighboring lawns much to the delight of barefooted children seen scampering among the blocks after the rain ended. U.S. History # 1897 - Hailstone drifts six feet deep were reported in Washington County, IA. -
Spatial and Temporal Variability of Tropical Storm and Hurricane Strikes
Louisiana State University LSU Digital Commons LSU Master's Theses Graduate School 2007 Spatial and temporal variability of tropical storm and hurricane strikes in the Bahamas, and the Greater and Lesser Antilles Alexa Jo Andrews Louisiana State University and Agricultural and Mechanical College, [email protected] Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_theses Part of the Social and Behavioral Sciences Commons Recommended Citation Andrews, Alexa Jo, "Spatial and temporal variability of tropical storm and hurricane strikes in the Bahamas, and the Greater and Lesser Antilles" (2007). LSU Master's Theses. 3558. https://digitalcommons.lsu.edu/gradschool_theses/3558 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]. SPATIAL AND TEMPORAL VARIABILITY OF TROPICAL STORM AND HURRICANE STRIKES IN THE BAHAMAS, AND THE GREATER AND LESSER ANTILLES 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 Alexa Jo Andrews B.S., Louisiana State University, 2004 December, 2007 Table of Contents List of Tables.........................................................................................................................iii -
Role of Climate Change on Recent Weather Disasters
Acta Scientific Agriculture Volume 2 Issue 4 April 2018 Research Article Role of Climate Change on Recent Weather Disasters S Jeevananda Reddy* Formerly Chief Technical Advisor – WMO/UN and Expert – FAO/UN and Fellow, Telangana Academy Sciences and Convenor, Forum for a Sustainable Environment, Hyderabad, Telangana, India *Corresponding Author: S Jeevananda Reddy, Formerly Chief Technical Advisor – WMO/UN and Expert – FAO/UN and Fellow, Telangana Academy Sciences and Convenor, Forum for a Sustainable Environment, Hyderabad, Telangana, India. Received: January 22, 2018; Published: March 21, 2018 Abstract damage to property and as well to nature that includes agriculture and water resources. The quantum of such loss or damage de- Natural disasters such as earthquakes, volcanoes, landslides, tsunamis, blizzards, floods, droughts, etc. can cause loss of life and pends on several factors. In the case of weather disasters, humans play vital destructive role. For the past one decade world over witnessed extreme weather events such as urban floods in India, hurricanes in southern USA, bomb cyclones in northeastern USA- events to climate change, which is used as de-fact global warming. The historical pattern on the occurrence of such extreme weather Canada. All these received wide media coverage; and rulers of the nations and so-called scientific community started attributing such events dispels this type of notion. Many a time they try to look at short period information and come up with sensational conclusions, which have serious repercussions’ on long-term planning for agriculture, water resources, etc. There is well-established data about these matters. However, there is a limitation on such historically data in both space and time as the recording started around 1850s; and prior to that written descriptions and as folklores of the events and consequent disasters are only available. -
Hurricane Beulah: Then and Now Is the Rio Grande Valley Ready, 50 Years Later?
Hurricane Beulah: Then and Now Is the Rio Grande Valley Ready, 50 Years Later? Barry Goldsmith Warning Coordination Meteorologist NWS Brownsville/Rio Grande Valley September 20: Catastrophic Hurricane, 160 mph 67 miles south of Brownsville/Port Isabel/SPI! Beulah’s September 15: Track Major Hurricane, 115 mph Southwest of Cayman Islands September 13: Tropical Storm, 60 mph South of Jamaica September 6: Depression, 35 mph September 18: Near Barbados Major Hurricane, 115 mph East of Tampico September 9: Major Hurricane, 140 mph South of Puerto Rico Beulah: Tale of the Tape • Landfall: September 20, just after midnight. Wind SSHWS Rating most likely high Cat 3/Low Cat 4. Minimum central pressure ~945 mb. • Inland inundation was the “Memory of Record” – Rainfall of 15-25” (or more) region wide – “Lake” South Texas – Floodways failed in at least two places • Wind damage widespread in Lower Valley – 136 mph gust in ship channel entrance; eight hours of hurricane force winds at Brownsville – 100 mph gusts as far west as Weslaco and McAllen • Peak storm tides 8 to 14 feet – Coastal inundation of South Padre Island, Port Mansfield, and parts of Port Isabel • 115 (to 141) tornadoes in south and central Texas, a single-storm U.S. record that stood until Ivan (2004) Beulah: Tale of the Tape • Damage Totals (1967 4.5 Impact Ranking Dollars): $170 million 4 statewide; $100 for the Rio 3.5 Grande Valley. Total 3 estimated damage was >$1 2.5 2 billion, second on record at 1.5 time 1 • Death toll still “fuzzy”; 0.5 reports vary from 11 to as 0 more than 15 persons. -
Tornado Basics
TORNADO BASICS NOAA/National Weather Service Tornado FAQ What is a tornado? According to the Glossary of Meteorology (AMS 2000), a tornado is "a violently rotating column of air, pendant from a cumuliform cloud or underneath a cumuliform cloud, and often (but not always) visible as a funnel cloud." Literally, in order for a vortex to be classified as a tornado, it must be in contact with the ground and the cloud base. Weather scientists haven't found it so simple in practice, however, to classify and define tornadoes. For example, the difference is unclear between an strong mesocyclone (parent thunderstorm circulation) on the ground, and a large, weak tornado. There is also disagreement as to whether separate touchdowns of the same funnel constitute separate tornadoes. It is well- known that a tornado may not have a visible funnel. Also, at what wind speed of the cloud-to-ground vortex does a tornado begin? How close must two or more different tornadic circulations become to qualify as a one multiple-vortex tornado, instead of separate tornadoes? There are no firm answers. BACK UP TO THE TOP How do tornadoes form? The classic answer -- "warm moist Gulf air meets cold Canadian air and dry air from the Rockies" -- is a gross oversimplification. Many thunderstorms form under those conditions (near warm fronts, cold fronts and drylines respectively), which never even come close to producing tornadoes. Even when the large-scale environment is extremely favorable for tornadic thunderstorms, as in an SPC "High Risk" outlook, not every thunderstorm spawns a tornado. The truth is that we don't fully understand. -
PREPARE SURVIVE BE SAFE ASSISTANCE EVACUATION ROUTES May 31, 2020
May 31, 2020 The Valley’s Guide to SURVIVING A STORM • 1 CAMERON COUNTY GUIDE THE VALLEY’S GUIDE TO SURVIVING A STORM PREPARE SURVIVE BE SAFE ASSISTANCE EVACUATION ROUTES May 31, 2020 EVACUATION HURRICANE TRACKING MAP ROUTES PULLOUT MAP PGS 10 & 11 PG. 17 2• The Valley’s Guide to SURVIVING A STORM May 31, 2020 TABLE OF CONTENTS 4 How to prepare for a hurricane. INTRODUCTION 6 Safety plan is key before the storm. A hurricane can cause widespread devastation during and after it occurs. 7 Stay safe when caught outdoors. This guide is designed to help you properly prepare for a hurricane and know how to protect yourself during and after one. ‘Assume’ you’re going to be hit. 8 Planning and preparing can make a big difference in safety and resiliency in the wake of a hurricane. The ability to quickly recover following a hurricane 9 Protect your property. requires a focus on preparedness, advance planning, and knowing what to do in the event of a hurricane. 10 Hurricane tracking map. 12 Preparation starts at home. 13 Stay Informed. 14 Insurance tips for hurricane preparation. 15 Residents should know flood risks. 16 How to build a pet hurricane kit. 17 Survive a hurricane. 18 What to put in your hurricane kit. 19 Secure your medicine. Cars travel through flooded streets in Weslaco after Hurricane Beulah in September 1967. Photos courtesy of Bob Retorik/USDA May 31, 2020 The Valley’s Guide to SURVIVING A STORM • 3 Taste the Difference Avant Quality Makes Locations Valleywide 10 lbs of Ice Only $1.00 Alamo Edinburg (cont.) Lyford El Gato Road and South Tower Road* 2202 W. -
I Hurrk R Leaves Close' Ricane B( I^Es Wak( E to $50 Beulah J Ike of Dl
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Characteristics of Tornadoes Associated with Land-Falling Gulf
CHARACTERISTICS OF TORNADOES ASSOCIATED WITH LAND-FALLING GULF COAST TROPICAL CYCLONES by CORY L. RHODES DR. JASON SENKBEIL, COMMITTEE CHAIR DR. DAVID BROMMER DR. P. GRADY DIXON A THESIS Submitted in partial fulfillment of the requirements for the degree of Master of Science in the Department of Geography in the Graduate School of The University of Alabama TUSCALOOSA, ALABAMA 2012 Copyright Cory L. Rhodes 2012 ALL RIGHTS RESERVED ABSTRACT Tropical cyclone tornadoes are brief and often unpredictable events that can produce fatalities and create considerable economic loss. Given these uncertainties, it is important to understand the characteristics and factors that contribute to tornado formation within tropical cyclones. This thesis analyzes this hazardous phenomenon, examining the relationships among tropical cyclone intensity, size, and tornado output. Furthermore, the influences of synoptic and dynamic parameters on tornado output near the time of tornado formation were assessed among two phases of a tropical cyclone’s life cycle; those among hurricanes and tropical storms, termed tropical cyclone tornadoes (TCT), and those among tropical depressions and remnant lows, termed tropical low tornadoes (TLT). Results show that tornado output is affected by tropical cyclone intensity, and to a lesser extent size, with those classified as large in size and ‘major’ in intensity producing a greater amount of tornadoes. Increased values of storm relative helicity are dominant for the TCT environment while CAPE remains the driving force for TLT storms. ii ACKNOWLEDGMENTS I would like to thank my advisor and committee chair, Dr. Jason Senkbeil, and fellow committee members Dr. David Brommer and Dr. P. Grady Dixon for their encouragement, guidance and tremendous support throughout the entire thesis process.