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Wind Speed-Damage Correlation in Hurricane Katrina
JP 1.36 WIND SPEED-DAMAGE CORRELATION IN HURRICANE KATRINA Timothy P. Marshall* Haag Engineering Co. Dallas, Texas 1. INTRODUCTION According to Knabb et al. (2006), Hurricane Katrina Mehta et al. (1983) and Kareem (1984) utilized the was the costliest hurricane disaster in the United States to concept of wind speed-damage correlation after date. The hurricane caused widespread devastation from Hurricanes Frederic and Alicia, respectively. In essence, Florida to Louisiana to Mississippi making a total of three each building acts like an anemometer that records the landfalls before dissipating over the Ohio River Valley. wind speed. A range of failure wind speeds can be The storm damaged or destroyed many properties, determined by analyzing building damage whereas especially near the coasts. undamaged buildings can provide upper bounds to the Since the hurricane, various agencies have conducted wind speeds. In 2006, WSEC developed a wind speed- building damage assessments to estimate the wind fields damage scale entitled the EF-scale, named after the late that occurred during the storm. The National Oceanic Dr. Ted Fujita. The author served on this committee. and Atmospheric Administration (NOAA, 2005a) Wind speed-damage correlation is useful especially conducted aerial and ground surveys and published a when few ground-based wind speed measurements are wind speed map. Likewise, the Federal Emergency available. Such was the case in Hurricane Katrina when Management Agency (FEMA, 2006) conducted a similar most of the automated stations failed before the eye study and produced another wind speed map. Both reached the coast. However, mobile towers were studies used a combination of wind speed-damage deployed by Texas Tech University (TTU) at Slidell, LA correlation, actual wind measurements, as well as and Bay St. -
San Jacinto Battleground and State Historical Park: a Historical Synthesis and Archaeological Management Plan
Volume 2002 Article 3 2002 San Jacinto Battleground and State Historical Park: A Historical Synthesis and Archaeological Management Plan I. Waynne Cox Steve A. Tomka Raba Kistner, [email protected] Follow this and additional works at: https://scholarworks.sfasu.edu/ita Part of the American Material Culture Commons, Archaeological Anthropology Commons, Environmental Studies Commons, Other American Studies Commons, Other Arts and Humanities Commons, Other History of Art, Architecture, and Archaeology Commons, and the United States History Commons Tell us how this article helped you. Cite this Record Cox, I. Waynne and Tomka, Steve A. (2002) "San Jacinto Battleground and State Historical Park: A Historical Synthesis and Archaeological Management Plan," Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State: Vol. 2002, Article 3. https://doi.org/10.21112/ita.2002.1.3 ISSN: 2475-9333 Available at: https://scholarworks.sfasu.edu/ita/vol2002/iss1/3 This Article is brought to you for free and open access by the Center for Regional Heritage Research at SFA ScholarWorks. It has been accepted for inclusion in Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State by an authorized editor of SFA ScholarWorks. For more information, please contact [email protected]. San Jacinto Battleground and State Historical Park: A Historical Synthesis and Archaeological Management Plan Creative Commons License This work is licensed under a Creative Commons Attribution-Noncommercial 4.0 License This article is available in Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State: https://scholarworks.sfasu.edu/ita/vol2002/iss1/3 San Jacinto Battleground State Historical Park A Historical Synthesis and Archaeological Management Plan by I. -
Texas Hurricane History
Texas Hurricane History David Roth National Weather Service Camp Springs, MD Table of Contents Preface 3 Climatology of Texas Tropical Cyclones 4 List of Texas Hurricanes 8 Tropical Cyclone Records in Texas 11 Hurricanes of the Sixteenth and Seventeenth Centuries 12 Hurricanes of the Eighteenth and Early Nineteenth Centuries 13 Hurricanes of the Late Nineteenth Century 16 The First Indianola Hurricane - 1875 21 Last Indianola Hurricane (1886)- The Storm That Doomed Texas’ Major Port 24 The Great Galveston Hurricane (1900) 29 Hurricanes of the Early Twentieth Century 31 Corpus Christi’s Devastating Hurricane (1919) 38 San Antonio’s Great Flood – 1921 39 Hurricanes of the Late Twentieth Century 48 Hurricanes of the Early Twenty-First Century 68 Acknowledgments 74 Bibliography 75 Preface Every year, about one hundred tropical disturbances roam the open Atlantic Ocean, Caribbean Sea, and Gulf of Mexico. About fifteen of these become tropical depressions, areas of low pressure with closed wind patterns. Of the fifteen, ten become tropical storms, and six become hurricanes. Every five years, one of the hurricanes will become reach category five status, normally in the western Atlantic or western Caribbean. About every fifty years, one of these extremely intense hurricanes will strike the United States, with disastrous consequences. Texas has seen its share of hurricane activity over the many years it has been inhabited. Nearly five hundred years ago, unlucky Spanish explorers learned firsthand what storms along the coast of the Lone Star State were capable of. Despite these setbacks, Spaniards set down roots across Mexico and Texas and started colonies. Galleons filled with gold and other treasures sank to the bottom of the Gulf, off such locations as Padre and Galveston Islands. -
Washburn Tunnel Wastewater Treatment
Washburn Tunnel Wastewater Treatment Facility WASHBURN TUNNEL & Vince Bayou Receiving Station WASTEWATER TREATMENT Location: Pasadena, TX, on the Houston FACILITY & VINCE BAYOU Ship Channel RECEIVING STATION Process: Activated sludge with atmospheric and pure oxygen infusion (Washburn Tunnel) Capacity: 48 million gallons/day (Washburn Tunnel) 1.4 million gallons/month (Vince Bayou) Acquired in 1973 from Champion Paper Co. and immediately modified and improved, Washburn Tunnel was the first facility to be operated by GCA, providing an early demonstration of the effectiveness and viability of wastewater treatment on a regional scale. Washburn Tunnel serves refineries, petrochemical plants, bulk storage facilities and other local industries located along the Houston Ship Channel. The facility also treats approximately a million gallons per day of municipal waste- water from the City of Pasadena as well as volumes from GCA’s nearby Vince Bayou Receiving Station. The facility receives most of its wastewater via pipeline; one customer, a small specialty fuels refinery, delivers its waste by barge. Wastewater containing high concentra- tions of organic material goes through a two-step activated sludge treatment process involving oxygenation and aeration. The facility’s incoming low-strength streams are mixed with higher-content organic waste streams before the second step of aeration. The final stage of the process utilizes conventional secondary clarifiers to remove much of the remaining solids before the effluent is discharged into the Houston Ship Channel. Gulf Coast Waste Disposal Authority Gulf Coast Waste The diverse, complex nature of wastewater treated at 910 Bay Area Blvd. • Houston, Texas 77058 Disposal Authority Washburn Tunnel has helped produce a robust mixture Phone: 281.488.4115 www.gcwda.com of contaminant-consuming microorganisms. -
GCHC NEWSLETTER FEBRUARY 2017.Pdf
Issue 2 Volume 3 Grimes County Historical Commission February 2017 Meetings of the Grimes County Historical Commission are held on the Second Monday of the Month at 7:00 pm in the Courthouse Annex in Anderson, Texas Contact Information Joe King Fultz [email protected] Visit us on Facebook https://www.facebook.com/Grim esCountyHistoricalCommission Grimes County Historical Commission Executive Board Photo of the Month Chairman Joe King Fultz Vice Chairman Vacant Secretary Vanessa Burzynski Treasurer Joe King Fultz COMMITTEES Historical Markers Denise Upchurch Historic Preservation Sarah Nash Newsletter & Publicity Vanessa Burzynski W. W. Meachum Law Office Anderson, Texas GRIMES COUNTY HISTORICAL COMMISSION NEWSLETTER FEBRUARY 2017 PAGE 2 History of the Town of Richards Richards is located on the Allen Vince one-half league RICHARDS, TEXAS. Richards is on Farm roads 1486 survey which the Mexican government granted him and 149 and the Burlington-Rock Island line in east on May 30, 1831. Vince, with his three brothers, central Grimes County. It was founded in 1907, when came to Texas in 1822 and settled on Sims Bayou in the residents of several communities in the vicinity present Harris County. His brothers settled along of Lake Creek moved to a newly constructed line of Vince’s Bayou and it was formerly thought the bridge the Trinity and Brazos Valley Railway where it across the Bayou was the one Sam Houston ordered crossed the road between Fairview (or Dolph) and destroyed before the Battle of San Jacinto, but today Longstreet. The area had been settled by Anglo- it has been proved to be the bridge over Sim’s Bayou American immigrants in the early 1830s, but no that had been built by Allen Vince. -
Urbanization Exacerbated the Rainfall and Flooding Caused by Hurricane Harvey and Tropical Storm Allison
Urbanization exacerbated the rainfall and flooding caused by hurricane Harvey and tropical storm Allison Wei Zhang IIHR-Hydroscience & Engineering, University of Iowa, Iowa City Hurricanes are formed in the warm ocean and make landfall over coastal regions occasionally. NASA 2 Hurricanes are warm-core low-pressure systems with destructive winds and torrential rainfall. Harvey in 2017 Katrina in 2005 100+ casualties 1,800+ casualties $125+ billion in damage $160+ billion in damage National Weather Service 3 Harvey stayed in Texas for several days. The reason for its stalling movement is still under investigation. 4 Record-breaking hurricane Harvey poured more than 1 meter rainfall over some parts of Houston. 休斯顿 Houston Stage IV Radar Products 5 Extreme precipitation and flash flooding caused by hurricane Harvey have led to major damages to Houston and surrounding areas. Associated Press CNN 6 Research on Harvey Rainfall (Impacts of anthropogenic forcing) • Assessing the present and future probability of Hurricane Harvey's rainfall (Emanuel 2018) • Quantitative attribution of climate effects on Hurricane Harvey's extreme rainfall in Texas (Wang et al. 2018) • Attribution of extreme rainfall from Hurricane Harvey, August 2017 (Van Oldenborgh et al. 2018) • Hurricane Harvey links to ocean heat content and climate change adaptation (Trenberth et al. 2018) 7 Climate change increased the probability of Harvey rainfall events. (Van Oldenborgh et al. 2018) 8 Again, climate change increased the probability of Harvey rainfall events. Emanuel, 2017, PNAS But, I examined Harvey rainfall from a different perspective … 9 What was the role played by buildings in Houston in changing the rainfall associated with hurricane Harvey? Before Hurricane Harvey After Hurricane Harvey 10 Oke et al. -
Stormwater Management Program 2013-2018 Appendix A
Appendix A 2012 Texas Integrated Report - Texas 303(d) List (Category 5) 2012 Texas Integrated Report - Texas 303(d) List (Category 5) As required under Sections 303(d) and 304(a) of the federal Clean Water Act, this list identifies the water bodies in or bordering Texas for which effluent limitations are not stringent enough to implement water quality standards, and for which the associated pollutants are suitable for measurement by maximum daily load. In addition, the TCEQ also develops a schedule identifying Total Maximum Daily Loads (TMDLs) that will be initiated in the next two years for priority impaired waters. Issuance of permits to discharge into 303(d)-listed water bodies is described in the TCEQ regulatory guidance document Procedures to Implement the Texas Surface Water Quality Standards (January 2003, RG-194). Impairments are limited to the geographic area described by the Assessment Unit and identified with a six or seven-digit AU_ID. A TMDL for each impaired parameter will be developed to allocate pollutant loads from contributing sources that affect the parameter of concern in each Assessment Unit. The TMDL will be identified and counted using a six or seven-digit AU_ID. Water Quality permits that are issued before a TMDL is approved will not increase pollutant loading that would contribute to the impairment identified for the Assessment Unit. Explanation of Column Headings SegID and Name: The unique identifier (SegID), segment name, and location of the water body. The SegID may be one of two types of numbers. The first type is a classified segment number (4 digits, e.g., 0218), as defined in Appendix A of the Texas Surface Water Quality Standards (TSWQS). -
Pilotthe Cameron Parish 35¢ June 21, 2007 Vol
PilotThe Cameron Parish 35¢ June 21, 2007 Vol. 50--No. 37 Cameron, La. 70631 THIS HISTORIC photo was taken from the second or third floor of the Cameron Courthouse on June 27, 1957, the day that Hurricane Audrey devastated Cameron Parish. Several hundred persons in the courthouse survived but about 500 others else- where in the parish perished. This photo was taken by the late Hadley Fontenot, who was Cameron’s county agent at the time. Audrey’s 50th anniversary will be observed Wednesday, June 27 in ceremonies at the courthouse. Audrey’s 50th anniversary to be observed here June 27th By CYNDI SELLERS Hurricane Audrey book; Cameron Parish Library - his- Even as Cameron Parish torical photos; Cameron Pilot struggles to recover from the - archival materials including effects of Hurricane Rita, the the first issue after the storm; tragic and devastating impact KPLC-TV - documentaries of Hurricane Audrey in 1957 and film clips; and the has not been forgotten. On National Hurricane Museum Wednesday, June 27, the and Science Center. parish will commemorate the Corporate sponsors of the 50th anniversary of the dead- commemoration are Cheniere ly storm, which claimed over LNG, Sempra Energy, and 400 lives. Cameron Communications. The ceremony will take place at 10 a.m. on the steps of the Cameron Court House, Oak Grove which sheltered hundreds from the fury of the storm. A speaker told light lunch will be served Brigadier General after the program, and dis- plays of hurricane informa- Robert J. LeBlanc Rev. John Reynolds will be tion, books, and memorabilia guest speaker at Oak Grove will be available for viewing. -
Downloaded 10/01/21 04:51 PM UTC JULY 2003 ANNUAL SUMMARY 1455
1454 MONTHLY WEATHER REVIEW VOLUME 131 ANNUAL SUMMARY Atlantic Hurricane Season of 2001 JOHN L. BEVEN II, STACY R. STEWART,MILES B. LAWRENCE,LIXION A. AVILA,JAMES L. FRANKLIN, AND RICHARD J. PASCH NOAA/NWS/Tropical Prediction Center/National Hurricane Center, Miami, Florida (Manuscript received 19 July 2002, in ®nal form 9 December 2002) ABSTRACT Activity during the 2001 hurricane season was similar to that of the 2000 season. Fifteen tropical storms developed, with nine becoming hurricanes and four major hurricanes. Two tropical depressions failed to become tropical storms. Similarities to the 2000 season include overall activity much above climatological levels and most of the cyclones occurring over the open Atlantic north of 258N. The overall ``lateness'' of the season was notable, with 11 named storms, including all the hurricanes, forming after 1 September. There were no hurricane landfalls in the United States for the second year in a row. However, the season's tropical cyclones were responsible for 93 deaths, including 41 from Tropical Storm Allison in the United States, and 48 from Hurricanes Iris and Michelle in the Caribbean. 1. Overview of the 2001 season cycleÐsimultaneously exhibiting characteristics of both tropical and extratropical cyclones (Hebert 1973). The National Hurricane Center (NHC) tracked 15 No hurricanes struck the United States during 2001. tropical cyclones (TCs) that achieved tropical storm or The season thus joins the 2000, 1990, and 1951 seasons hurricane strength in the Atlantic basin during 2001 as years in which eight or more hurricanes occurred (Table 1). Nine of these became hurricanes and four without a U.S. -
Hurricane Andrew in Florida: Dynamics of a Disaster ^
Hurricane Andrew in Florida: Dynamics of a Disaster ^ H. E. Willoughby and P. G. Black Hurricane Research Division, AOML/NOAA, Miami, Florida ABSTRACT Four meteorological factors aggravated the devastation when Hurricane Andrew struck South Florida: completed replacement of the original eyewall by an outer, concentric eyewall while Andrew was still at sea; storm translation so fast that the eye crossed the populated coastline before the influence of land could weaken it appreciably; extreme wind speed, 82 m s_1 winds measured by aircraft flying at 2.5 km; and formation of an intense, but nontornadic, convective vortex in the eyewall at the time of landfall. Although Andrew weakened for 12 h during the eyewall replacement, it contained vigorous convection and was reintensifying rapidly as it passed onshore. The Gulf Stream just offshore was warm enough to support a sea level pressure 20-30 hPa lower than the 922 hPa attained, but Andrew hit land before it could reach this potential. The difficult-to-predict mesoscale and vortex-scale phenomena determined the course of events on that windy morning, not a long-term trend toward worse hurricanes. 1. Introduction might have been a harbinger of more devastating hur- ricanes on a warmer globe (e.g., Fisher 1994). Here When Hurricane Andrew smashed into South we interpret Andrew's progress to show that the ori- Florida on 24 August 1992, it was the third most in- gins of the disaster were too complicated to be ex- tense hurricane to cross the United States coastline in plained by thermodynamics alone. the 125-year quantitative climatology. -
Hurricane Audrey Storm Tide
QC9¥f 0 7^-2 3 39 NAL HURRICANE RESEARCH PROJECT ATSL REPORT NO. 23 Hurricane Audrey Storm Tide *•*'• U. S. DEPARTMENT OF COMMERCE Sinclair Weeks, Secretary WEATHER BUREAU F. W. Reichelderfer, Chief NATIONAL HURRICANE RESEARCH PROJECT REPORT NO. 23 Hurricane Audrey Storm Tide by D. Lee Harris U. S. Weather Bureau, Washington, D. C. Washington, D. C. October 1958 UlfiMOl 0b0b32^ NATIONAL HURRICANE RESEARCH PROJECT REPORTS Reports by Weather Bureau units, contractors, and coopera- tors working on the hurricane problem are pre-printed in this series to facilitate immediate distribution of the information among the workers and other interested units. As this limited < reproduction and distribution in this form do not constitute formal scientific publication, reference to a paper in the . series should identify it as a pre-printed report. 1. Objectives and basic desigu of the National Hurricane Research Pro- ? No. ject. March 1956. ^ T , inR^ I P Numerical weather prediction of hurricane motion. July 195©. No. SementTError analysis of prognostic 500-mb. maps made for numer ical weather prediction of hurricane motion. March 195 (> 3. Rainfall associated with hurricanes. July 195&. i] No. I. %m problems involved in the study of storm surges. December 1956. is No. 5. Survey of meteorological factors pertinent to reduction of loss of life and property in hurricane situations. March 1957. ; No 6. A mean atmosphere for the West Indies area. May 1957. j No. 7. An index of tide gages and tide gage records for the Atlantic and Gulf coasts of the United States. May 1957- \ Nmo ft PartE£ Ili. ^exchangeHurricanes andoftheenergysea betweensurface temperaturethe sea and thefield.atmosphere ?j in relation to hurricane behavior. -
Hurricanes Are a Regular Threat to the SCIPP Gulf Coast and Average Amount of Time That Passes Between Hurricane Events at Should Be Planned for Each Season
SCIPP HURRICANE CLIMATOLOGY: The NHC defines the Atlantic hurricane season as the period from part of the hurricane season, landfall occurrences shift from the June 1 to November 30. Tropical cyclones occur with greatest Gulf Coast to the U.S. east coast. frequency during that time period, which is when the sea surface temperatures are warmest, but can still occur outside of the The relative return frequency of hurricane landfalls can give us a official season. statistical idea of just how often we can expect a hurricane at a specific spot along the Gulf Coast. A return period represents the Hurricanes are a regular threat to the SCIPP Gulf Coast and average amount of time that passes between hurricane events at should be planned for each season. Of the top 10 deadliest and any one location based on the historical record. Figure 3 depicts top 10 costliest (adjusted for inflation, 2006) tropical cyclones to the return frequency for some notable beaches in the SCIPP make U.S. landfall, five in each list have occurred along the domain, from 1900-2005 records. For all of the beaches analyzed SCIPP coast. From 1851-2006 128 hurricanes have affected the in the study, a tropical cyclone can by expected every 3-5 years Texas, Louisiana, or Mississippi coastline, 58 of them have been and a hurricane every 7-15 years. Major hurricanes are much major hurricanes of Category 3 or greater. more rare and, based on past storm events, have a return period of 26 or 52 years for most of the beaches.