Lynn Donelson Wright C. Reid Nichols Editors Tomorrow’S Coasts: Complex and Impermanent Coastal Research Library
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The Perfect Storm
The Perfect Storm Weathering Climate Change By Building Better Communities A Presentation By R.W. Sandford Chair Canadian Partnership United Nations Water for Life Decade Director Western Watersheds Climate Research Collaborative The Perfect Storm Weathering Climate Change By Building Better Communities The purpose of the Canadian Partnership Initiative of the United Nations Water for Life Decade is to translate scientific research outcomes into language the average person can understand and that decision-makers can act upon in a timely manner to address water-related climate change impacts. While this has sometimes been difficult, the challenge has not distracted us from our urgent purpose. In our estimation, climate change has the potential to create a perfect environmental cum economic cum social cum political storm. It is a storm, however, that I think we can avoid. That is especially true here, where you live. The notion of a perfect storm emerged into popular culture in 1997 with the appearance of Sebastion Junger’s non- fiction work of the same name. The book is about the “Hallowe’en Nor’easter” as the locals called it – a storm that struck the east coast of North America in October of 1991. It should be noted that it wasn’t Sebastian Junger who first described the 1991 tempest as “the perfect storm”. It was the U.S. National Weather Service that gave it that name and created its legend. In the history of American weather observation, no had never seen anything quite like it. 2 The National Ocean and Atmospheric Administration in the United States still maintains a website explaining the nature and character of that remarkable storm. -
The Perfect Storm October 1991
Satellite Gallery / Extratropical Cyclones / Perfect Storm 1991 / The Perfect Storm October 1991 Enlarged Image Image Information Event Discussion Bizarre Ending An enormous extratropical low is creating havoc along the entire Eastern Atlantic Seaboard in this infrared image at 1200 UTC (0700 EST) on October 30, 1991. Labelled the "perfect storm" by the National Weather Service, the storm s ank the swordfishing boat Andrea Gail, whose story became the basis for the currently best-selling novel "The Perfect Storm" by Sebastian Junger. A little-known and bizarre ending came to this monster, which came to be known as the Halloween Storm. To tell this incredible story in its entirety, the Satellite's Eye Art Gallery spans two subject headings (Extratropical Cyclones and Hurricanes)! Image Information Satellite System Image Specifics Channel Satellite Name GOES 7 No. 4 (Infrared) Band October 30, Date Resolution 4-km 1991 Julian Date 303 Orbit No./Dir NA 1201 UTC Time Entity ID NA 0701 EST Instrument Western VAS: VISSR Area System Atlantic Data Type Sector The Perfect Storm Conditions at the Time of the Image The color-enhanced infrared image of 1200 UTC October 30, 1991 depicts a monster storm off the Eastern Sea board, which was described by the National Weather Service as the "perfect storm." In this image, the storm was at its peak intensity. The storm became subtropical thirty hours later, just before the inner core of the storm developed into a topical storm and later an unnamed hurricane. History of the Storm Late October and November are months with weather in rapid transition in the eastern U.S. -
Table of Contents
Commonwealth of Massachusetts 2013 State Hazard Mitigation Plan Section 13. Nor’easters .......................................................................................................................... 13-1 13.1 General Background .................................................................................................................. 13-1 13.1.1 Rating Scales ................................................................................................................ 13-2 13.1.2 Coastal Storm Frequency Caveats ................................................................................ 13-3 13.2 Hazard Profile ........................................................................................................................... 13-4 13.2.1 Location........................................................................................................................ 13-4 13.2.2 Previous Occurrences ................................................................................................... 13-4 13.2.3 Probability of Future Occurrences ............................................................................... 13-9 13.2.4 Severity ........................................................................................................................ 13-9 13.2.5 Warning Time .............................................................................................................. 13-9 13.3 Climate Change Impacts .......................................................................................................... -
The Eastern Shore of Virginia, 1603-1964
For Reference Do Hot Take From the Library The laaB Eastern Shore l^UmUlllliUI IHitllUU^tSR Virginia 1603 - 1964 »« m • For Reference Not to be taken from this room V^€' T), v/ VIRGINIA BEACH PUBLIC LIBRARY CENTRAL LIBIJAR'Y 4100 VIRGiHlA BEACH BLVD. VIIJGINIA BtACH, VA= 23452 NOTE The following explanations are offered relative to inlonnation contained in this printing of The Eastern Shore of Virginia 1603-1964. Page Line 1 3 Reference is made to modern reckoning of longitude. 28 20 The wife of William Gotten was a sis- ter-in-law of William Stone. 43 3 The date should be July 28, 1643. 43 10 The date should be March 1643 N. S. 110 25 The General Assembly of 1732 provided for local sponsorship for licensing at- torneys rather than providing for the direct licensing of attorneys. 197 16 It was George R. Mapp who became the third superintendent and not John R. Mapp. 272 40 William T. Fitchett was Circuit Court Judge from March 1882 to March 1884 between two terms of Benjamin T. Gun- ter. 274 38 The reference to the Clerk of Court should be Robert H. Oldham rather than Robert H. Oldham, Jr. 274 49 In the list of Superintendent of Schools for Northampton County, the name should be D. W. Peterson rather than W. D. Peters, 280 1 John Andrews Upshur was graduated from the United States Naval Academy in the class of 1921. 280 44 Henry Alexander Wise was the son of Edward S. Wise rather than Edgar S. Wise as stated. -
U.S. Coast Guard Historian's Office
U.S. Coast Guard Historian’s Office Preserving Our History For Future Generations Historic Light Station Information VIRGINIA ASSATEAGUE LIGHT Lighthouse Name: Assateague Island Light Location: Southern end of Assateague Island Date Built: Established in 1833 with present tower built in 1867 Type of Structure: Conical brick tower with red and white stripes; Height: Tower is 145' with a 154' focal plane Characteristic: Originally a fixed white light, with a fixed red sector (added in 1907), changed to two white flashes every 5 seconds in 1961, visible for 19 miles. Lens: Original lens was an Argand lamp system with 11 lamps with 14 inch reflectors. The 1867 tower had a first order Fresnel lens with four wicks, now DCB 236. The Fresnel lens was made by Barbier & Fenestre, Paris 1866 Appropriation: $55,000 Automated: 1933 when changed to battery power Status: Open Easter through May, and October through Thanksgiving weekend every Friday through Sunday from 9 am to 3 pm; During June, July, August and September open Thursday through Monday from 9 AM to 3PM, last climb 2:30 PM call (757) 336- 3696 for information. Historical Information: The original light was built in 1833 was only 45 feet tall and was not sufficient for coastal needs so in 1859 Congress appropriated funds to build a higher, more effective tower. Work began in 1860 but was suspended during the Civil War. The current structure was completed and lit in 1867. The keeper's quarters built in 1867was a duplex. In 1892 it was remodeled with three large sections of six rooms each to house three families with each section including a pantry, kitchen, dining room, living room, three bedrooms, bathroom, and large closet. -
Geology Combination of Storms Precursors
Geology !Hurricanes: violent warm core tropical storm and min wind speed of 74 mph. Rotates counterclockwise spiraling around region of low pressure (eye/center) !June 1- November 30 !Saffir-Simpson Hurricane Scale (1-5) !4 Stages of Hurricane Growth: Tropical Jennifer Lougen Disturbance, Tropical Depression, Tropical Storm, Hurricane Natural Hazards & Disasters October 19, 2005 !Nor’easter: east moving cold air meets warm air from Eastern Atlantic Coast Combination of Storms region !snow, rain, freezing rain, and sleet !strong winds !significant coastal flooding !blizzard conditions !Hybrid Storm: special type of coastal storm that can produce major problems in the fall; combined char. Of tropical & extratropical/midlatitude storms October 28, 1991 Precursors !Subtropical storm E. Caribbean reaches hurricane status !Hurricane Bob, August 1991 (Hurricane Grace) !Extratropical storm !Hurricane Grace, October 28, 1991 off of New England October 29, 1991 !Strong Extratropical !Hurricane Grace Storm changed direction !Area of Low Pressure (ENE) !Extratropical storm absorbed Hurricane Grace 1 October 30, 1991 November 1, 1991 (4 pm) !Peak winds (~ 100 mph) ! 100 ft. waves (one of highest ever recorded) !10-30 ft. waves hitting coast !Extratropical Storm turned SW"S November 1, 1991 (6 pm) !Over Warm Gulf !Tropical Storm intensity Stream !Late, eye forming ! hit New England (almost hurricane status) Coast October 31, 1991 !November 2: !Makes counterclockwise loop !Winds ~ 100 mph !Hurricane Status !Cyclone weakened !Landfall near Halifax, Nova Scotia !Dissipated 10 hours later Preparation & Awareness After Effects ! Storm not thought !New England storms commonly from of as real threat to West land but more to ships !Perfect storm came from East ! Beach Erosion ! NWS, local meteorologists and (10’s m’s removed Hurricane Ctr. -
Summer-Fall 2006 Newsletter.Pub
NOAA’S NATIONAL WEATHER SERVICE, NEWPORT/MOREHEAD CITY NC www.erh.noaa.gov/mhx - BOOKMARK IT! CAROLINA SKY WATCHER SUMMER 2006 EDITION Hurricane Season 2006 Outlook By John Cole, Warning Coordination Meteorologist 2006 is expected to be another active year for tropical cyclones in the Atlantic Hurricane Basin. NOAA expects 13-16 named storms, 8-10 hurri- canes (sustained winds greater than 74 mph), and 4-6 major hurricanes (sustained winds over 110 mph). Dr. William Gray and his research team at Colorado State University expect 17 named storms, 9 hurricanes, and 4 major hurricanes. Dur- ing an average hurricane season, which runs from June 1st through Nov. 30th, we have 11 named storms, 6 hurricanes, and 2 major hurricanes. Fac- tors which favor an active year are warmer than normal water temperatures, light mid and upper level winds, and lower pressure in the Atlantic Ocean, Caribbean Sea, and the Gulf of Mexico. The three primary months for hurricane activ- ity are August, September, and October. INSIDE THIS ISSUE: HURRICANE THREAT- 2 TORNADOES HURRICANE FRAN-10 YEARS 3-4 AGO HURRICANE QUIZ 5-6 SAFFIR WHO? SIMPSON WHO? 7 RIP CURRENT DANGER 8-9 PAGE 2 CAROLINA SKY WATCHER Hurricane threats: tornadoes! By Bob Frederick, Forecaster Hurricanes pose many threats to life and property when they impact eastern North Carolina. Across the United States approximately 10 percent of hurricane fatalities are a result of tornadoes. Some hurricanes and tropical storms produce little if any tornado activity, while other can produce numerous tornadoes. Almost all tornadoes associated with hurricanes occur on the right front quadrant of the storm (see Figure 1). -
Insights Into Barrier-Island Stability Derived from Transgressive/Regressive State Changes of Parramore Island, Virginia
Marine Geology 403 (2018) 1–19 Contents lists available at ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margo Insights into barrier-island stability derived from transgressive/regressive T state changes of Parramore Island, Virginia ⁎ Jessica L. Raffa, ,1, Justin L. Shawlerb, Daniel J. Ciarlettac, Emily A. Heinb, Jorge Lorenzo-Truebac, Christopher J. Heinb a Department of Geology, College of William & Mary, P.O. Box 8795, Williamsburg, VA 23187-8795, USA b Virginia Institute of Marine Science, College of William & Mary, P.O. Box 1346, Gloucester Point, VA 23062-1346, USA c Department of Earth and Environmental Studies, Montclair State University, 1 Normal Ave, Montclair, NJ 07043, USA ARTICLE INFO ABSTRACT Editor: E. Anthony Barrier islands and their associated backbarrier ecosystems front much of the U.S. Atlantic and Gulf coasts, yet Keywords: threshold conditions associated with their relative stability (i.e., state changes between progradation, erosion, Barrier island and landward migration) in the face of sea-level rise remain poorly understood. The barrier islands along Progradation Virginia's Eastern Shore are among the largest undeveloped barrier systems in the U.S., providing an ideal Antecedent geology natural laboratory to explore the sensitivity of barrier islands to environmental change. Details about the de- Foredune ridge velopmental history of Parramore Island, one of the longest (12 km) and widest (1.0–1.9 km) of these islands, Beach ridge provide insight into the timescales and processes of barrier-island formation and evolution along this mixed- Inlet energy coast. Synthesis of new stratigraphic (vibra-, auger, and direct-push cores), geospatial (historical maps, aerial imagery, t-sheets, LiDAR), and chronologic (optically stimulated luminescence, radiocarbon) analyses reveals that Parramore has alternated between periods of landward migration/erosion and seaward progradation during the past several thousand years. -
Hurricanes - General Information for Bermuda Prepared by the Bermuda Weather Service – Updated August 2021
Hurricanes - General Information for Bermuda Prepared by the Bermuda Weather Service – updated August 2021 Hurricanes and tropical storms have had an impact on Bermuda from its earliest times. The initial colonization of Bermuda was a direct result of a hurricane in 1609 in which an English ship the "Sea Venture" ran aground. A study of local records from 1609 to the present day, of storm damage through the years indicates a damaging storm once every 6 to 7 years until the 21st century. Since 2000, an uptick in Bermuda-relevant tropical cyclones (TCs) has been noted in the record, and highlighted in the academic literature. The long-term effects of climate change on the variability of Bermuda TCs are an area of active research. However, recent studies indicate that increasing upper ocean temperatures near Bermuda are contributing to increased trends in TC activity locally. Hurricane season in the Atlantic is June through November, however Bermuda has seen subtropical storm activity as early as April (e.g. 2003 Ana), and has occasionally experienced tropical cyclone activity through November. Bermuda is 54 square kilometres (21 sq. miles) in area, located approximately at 32.3°N 64.7°W. Despite being out of the main TC development region of the tropical Atlantic, as well as being a ‘small target’, Bermuda has received a number of notable TC impacts in the last 20 years. The peak months for tropical cyclone activity for Bermuda are September and October, with over 80% of all storms coming within ‘threat’ range (100nm/185km) of Bermuda occurring during these months. -
Mariners Weather Log Vol
Mariners Weather Log Vol. 44, No. 2 August 2000 The Jay Gould sank on June 17, 1918, near Southeast Shoal, Lake Erie, while towing the barge Commodore. All on board the two ships were rescued by passing steamboats. (See article on page 13.) Photo: Milwaukee Public Library. Mariners Weather Log Mariners Weather Log From the Editorial Supervisor This issue features an article on storm surge, which is the term used to describe the rise in still-water sea level that accompanies the landfall of a tropical storm or hurricane. Recognized as the single most destructive aspect of a hurricane, the coastal storm surge can cause much damage and loss of life (nine out of ten hurricane U.S. Department of Commerce deaths result from drowning in storm surge). The low Norman Y. Mineta, Secretary pressure in the eye literally sucks the ocean surface upward, like liquid through a straw, and vast tracts of National Oceanic and low-lying coastal terrain can be inundated with water as Atmospheric Administration the eye of the hurricane makes landfall. In the northern Dr. D. James Baker, Administrator hemisphere, the area just to the right of the storm track experiences the greatest rise in water level due to the added effect of the wind pushing the water. During the National Weather Service John J. Kelly, Jr., infamous hurricane Camille in 1969, a 25-foot storm Assistant Administrator for Weather Services surge inundated Pass Christian, Mississippi. Lesser heights are more usual, but still extremely dangerous. Editorial Supervisor Directly linked to a tropical storm’s central barometric Martin S. -
Seed Groups Process
Exploring the Scriptures June 24, 2012 Mark 4:35-41 Storms and Calm by Blair Odney In his book, “The Perfect Storm,” Sebastian Junger recounts the story of a natural disaster off the coast of Massachusetts in the fall of 1991. In 2000, the book became a movie starring George Clooney. The death toll was 13 and damage was estimated at $200 million, most which occurred when waves up to 10 meters struck the coastline from Canada to Florida and down to Puerto Rico. A buoy off the coast of Nova Scotia reported a wave height of 30 meters, the highest ever recorded in the province's offshore waters...basically the height of ten story building. Imagine meeting a wall of water 100 feet high.. So what made this storm so “perfect”? Junger got the phrase “perfect storm” from a retired meteorologist who said the storm’s intensity was caused by a perfect alignment of several factors; such a convergence of weather conditions occurs only once every 50 to 100 years. This perfect storm began on October 26, with the formation of a hurricane, a Category 2 tropical storm south of Bermuda. This hurricane moved up the East Coast of the United States, losing power along the way, but on October 29, it collided with a cyclone moving down the coast from Nova Scotia. The cyclone, formed by a low-pressure front moving in from the Midwestern United States met a high-pressure front moving down from Northern Canada, which together absorbed the power of the first hurricane, increasing in intensity. -
Perfect Storm
THE PERFECT STORM DEVELOPS 0. THE PERFECT STORM DEVELOPS - Story Preface 1. THE ANDREA GAIL 2. LONG-LINING for SWORDFISH 3. PREDICTING BAD WEATHER 4. PREDICTING DANGEROUS STORMS 5. THE PERFECT STORM DEVELOPS 6. DEATH ON THE HIGH SEAS 7. ANOTHER MAELSTROM 8. RESCUE EFFORTS AT SEA 9. THE UNNAMED HURRICANE 10. NEIGHBORS IN DEATH Three different weather systems collided between the 28th of October and the 2nd of November - in 1991 - to produce what meteorologists called a "perfect storm." Graphic online, courtesy AccuWeather. On October 23, 1991, Billy Tyne and his crew (Michael "Bugsy" Moran, Dale "Murph" Murphy, Alfred Pierre, David Sullivan and Bobby Shatford) set their longline for what they hoped would be the best catch of the trip. (The links take you on board the Andrea Gail the year before she was lost. The fish hold is empty in the picture.) It was the last full moon of the fishing season, and the men would soon be steaming home to Gloucester. As the Andrea Gail headed home, most of the other boats in the fleet were hundreds of miles east - still fishing. When Billy radioed the Canadian Coast Guard the afternoon of October 27th, to let them know his boat was inside Canada's territorial waters, he didn't know a huge storm was brewing south of him. (The link takes you inside the pilot house of the Andrea Gail.) He didn't know until he received the first fax, later that night. What Billy didn't know was that Hurricane Grace, forming off Bermuda on the 27th of October, had turned northeast.