New England Effects from the Hurricane Sandy Hybrid Storm
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Chapter 4: Cultural and Historic Resources
Ocean Special Area Management Plan Chapter 4: Cultural and Historic Resources Table of Contents 400 Introduction ......................................................................................................................3 410 Historic Contexts and Cultural Landscapes of the Ocean SAMP Area .......................4 410.1 Pre-Contact Geological History............................................................................5 410.2 Narragansett Tribal History.................................................................................6 410.3 European Exploration and Colonial Settlement Landscape Context .............16 410.4 Post-Colonial Cultural Landscape Context.......................................................18 410.5 Military Landscape Context ...............................................................................21 410.6 Fisheries Landscape Context ..............................................................................31 410.6.1 Rhode Island Fisheries.............................................................................31 410.6.2 Fishing and Subsistence on Block Island.................................................33 410.6.3 Historic Shipwrecks of Fishing Vessels ..................................................34 410.6.4 Historic Harbor Features..........................................................................35 410.7 Marine Transportation and Commercial Landscape Context........................35 410.8 Recreation and Tourism Landscape Context....................................................38 -
Block Island Sound Rhode Island Sound Inner Continental Shelf
Ecology of the Ocean Special Area Management Plan Area: Block Island Sound Rhode Island Sound Inner Continental Shelf Alan Desbonnet Carrie Byron with help from Elise Desbonnet, Barry Costa-Pierce, Meredith Haas and the PELL LIBRARY STAFF and MANY, MANY Researchers The Ecology of Rhode Island Sound, Block Island Sound and the Inner Continental Shelf GEOLOGY 2,500 km2 31 m average 60 m max 1,350 km2 40 m averageAcadian vs. Virginian 100 m maxecoregions The Ecology of Rhode Island Sound, Block Island Sound and the Inner Continental Shelf Boothroyd 2008 SLR 2.5-3.0 mm per year (1/10th inch) Glacial Origins--- a key element E. Uchupi, N.W. Driscoll, R.D. Ballard, and S.T. Bolmer, 2000 The Ecology of Rhode Island Sound, Block Island Sound and the Inner Continental Shelf Boothroyd 2009 Downwelling – Combined Flow Circulation/currents shaped by the geology Bottom habitats are dynamic/ever changing The Ecology of Rhode Island Sound, Block Island Sound and the Inner Continental Shelf Boothroyd 2008 Winter = NW (stronger) Summer = SW (milder) WINDS NOT a major driver of circulation Av.Big Wave implications height for stratification = 1-3 m Max = 7 m (9 m 100 yr. wave) The Ecology of Rhode Island Sound, Block Island Sound and the Inner Continental Shelf Spaulding 2007 Most recent Cat3 = Esther in 1961 Most recent = Bob (Cat2) in 1991 No named hurricane 18 years 17 RI hurricanes: 7 Category 1 8 Category 2 2 Category 3 The Ecology of Rhode Island Sound, Block Island Sound and the Inner Continental Shelf NOAA Hurricane Center online data 2010 Important -
Geological Survey
imiF.NT OF Tim BULLETIN UN ITKI) STATKS GEOLOGICAL SURVEY No. 115 A (lECKJKAPHIC DKTIOXARY OF KHODK ISLAM; WASHINGTON GOVKRNMKNT PRINTING OFF1OK 181)4 LIBRARY CATALOGUE SLIPS. i United States. Department of the interior. (U. S. geological survey). Department of the interior | | Bulletin | of the | United States | geological survey | no. 115 | [Seal of the department] | Washington | government printing office | 1894 Second title: United States geological survey | J. W. Powell, director | | A | geographic dictionary | of | Rhode Island | by | Henry Gannett | [Vignette] | Washington | government printing office 11894 8°. 31 pp. Gannett (Henry). United States geological survey | J. W. Powell, director | | A | geographic dictionary | of | Khode Island | hy | Henry Gannett | [Vignette] Washington | government printing office | 1894 8°. 31 pp. [UNITED STATES. Department of the interior. (U. S. geological survey). Bulletin 115]. 8 United States geological survey | J. W. Powell, director | | * A | geographic dictionary | of | Ehode Island | by | Henry -| Gannett | [Vignette] | . g Washington | government printing office | 1894 JS 8°. 31pp. a* [UNITED STATES. Department of the interior. (Z7. S. geological survey). ~ . Bulletin 115]. ADVERTISEMENT. [Bulletin No. 115.] The publications of the United States Geological Survey are issued in accordance with the statute approved March 3, 1879, which declares that "The publications of the Geological Survey shall consist of the annual report of operations, geological and economic maps illustrating the resources and classification of the lands, and reports upon general and economic geology and paleontology. The annual report of operations of the Geological Survey shall accompany the annual report of the Secretary of the Interior. All special memoirs and reports of said Survey shall be issued in uniform quarto series if deemed necessary by tlie Director, but other wise in ordinary octavos. -
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. -
Assessing Interactions Between Estuary Water Quality and Terrestrial Land Cover in Hurricane Events with Multi-Sensor Remote Sensing
University of Central Florida STARS Electronic Theses and Dissertations, 2004-2019 2017 Assessing Interactions between Estuary Water Quality and Terrestrial Land Cover in Hurricane Events with Multi-sensor Remote Sensing Chandan Mostafiz University of Central Florida Part of the Environmental Engineering Commons, and the Water Resource Management Commons Find similar works at: https://stars.library.ucf.edu/etd University of Central Florida Libraries http://library.ucf.edu This Masters Thesis (Open Access) is brought to you for free and open access by STARS. It has been accepted for inclusion in Electronic Theses and Dissertations, 2004-2019 by an authorized administrator of STARS. For more information, please contact [email protected]. STARS Citation Mostafiz, Chandan, Assessing" Interactions between Estuary Water Quality and Terrestrial Land Cover in Hurricane Events with Multi-sensor Remote Sensing" (2017). Electronic Theses and Dissertations, 2004-2019. 5688. https://stars.library.ucf.edu/etd/5688 ASSESSING INTERACTIONS BETWEEN ESTUARY WATER QUALITY AND TERRESTRIAL LAND COVER IN HURRICANE EVENTS WITH MULTI-SENSOR REMOTE SENSING by CHANDAN MOSTAFIZ B.S. Bangladesh University of Engineering and Technology, 2014 A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in the Department of Civil, Environmental, and Construction Engineering in the College of Engineering and Computer Science at the University of Central Florida Orlando, Florida Fall Term 2017 Major Professor: Ni-Bin Chang © 2017 Chandan Mostafiz ii ABSTRACT Estuaries are environmentally, ecologically and environmentally important places as they act as a meeting place for land, freshwater and marine ecosystems. They are also called nurseries of the sea as they often provide nesting and feeding habitats for many aquatic plants and animals. -
Meeting Packet July 31, 2019
BLOCK ISLAND UTILITY DISTRICT Lineworkers Jim Stockman and Evan Carey performing hot line work; changing a failed fused cut out which caused the Corn Neck outage on the evening of July 4th. BOARD OF COMMISSIONERS MEETING JULY 31, 2019 Block Island Utility District Wednesday July 31, 2019 Town Hall, Old Town Road 4:00 p.m. 1. Commissioner’s Report 2. Public Input 3. Approve Minutes of June 25, 2019 4. Receive and Act on Treasurers Report a. Review June 2019 Financials b. Provide Feedback on New Financials Format 5. Receive and Act on Presidents Report 6. Review and Act on CFC Letter of Credit to be used for ISO-NE Financial Assurance 7. Review and Act on CFC Restatement of the Original $670,000 Line of Credit (LOC) – Mortgage Supplement to Secure LOC 8. Review and Act on Rate Case Filing 9. Discuss and Act on Annual Meeting Agenda a. Update on Election Schedule 10. Discuss and Act on NRECA Director Election 11. Discuss and Act on President’s Job Description, Performance Review and Salary 12. Discuss and Act on Litigation* *This item may be held in Closed Session pursuant to RIGL 42-46-5(2) (litigation: Sara McGinnes v. Town of New Shoreham & Howell Conant v. Block Island Power Company) Individuals requesting services for the deaf and hard of hearing must call (401) 466-5851 forty-eight hours in advance of the meeting date. TTY: 711 Posted: 7/25/19 Agenda Item 1 Commissioner’s Report (NOTE TAKING SECTION) Agenda Item 2 Public Input (NOTE TAKING SECTION) Page 2 of 32 Agenda Item 3 Approve Minutes of June 25, 2019 Page 3 of 32 Block Island Utility District Tuesday June 25, 2019 Town Hall 4:00 PM Present: Commissioners Mary Jane Balser, Barbara MacMullan, William Penn, Everett Shorey, Jeff Wright, President of BIPCo, Renee Meyers, Block Island Times, Bonnie Biocchi, Northeast Public Power Association. -
Massachusetts Tropical Cyclone Profile August 2021
Commonwealth of Massachusetts Tropical Cyclone Profile August 2021 Commonwealth of Massachusetts Tropical Cyclone Profile Description Tropical cyclones, a general term for tropical storms and hurricanes, are low pressure systems that usually form over the tropics. These storms are referred to as “cyclones” due to their rotation. Tropical cyclones are among the most powerful and destructive meteorological systems on earth. Their destructive phenomena include storm surge, high winds, heavy rain, tornadoes, and rip currents. As tropical storms move inland, they can cause severe flooding, downed trees and power lines, and structural damage. Once a tropical cyclone no longer has tropical characteristics, it is then classified as a post-tropical system. The National Hurricane Center (NHC) has classified four stages of tropical cyclones: • Tropical Depression: A tropical cyclone with maximum sustained winds of 38 mph (33 knots) or less. • Tropical Storm: A tropical cyclone with maximum sustained winds of 39 to 73 mph (34 to 63 knots). • Hurricane: A tropical cyclone with maximum sustained winds of 74 mph (64 knots) or higher. • Major Hurricane: A tropical cyclone with maximum sustained winds of 111 mph (96 knots) or higher, corresponding to a Category 3, 4 or 5 on the Saffir-Simpson Hurricane Wind Scale. Primary Hazards Storm Surge and Storm Tide Storm surge is an abnormal rise of water generated by a storm, over and above the predicted astronomical tide. Storm surge and large waves produced by hurricanes pose the greatest threat to life and property along the coast. They also pose a significant risk for drowning. Storm tide is the total water level rise during a storm due to the combination of storm surge and the astronomical tide. -
National Assessment of Hurricane-Induced Coastal Erosion Hazards: Northeast Atlantic Coast
National Assessment of Hurricane-Induced Coastal Erosion Hazards: Northeast Atlantic Coast By Justin J. Birchler, Hilary F. Stockdon, Kara S. Doran, and David M. Thompson Open-File Report 2014–1243 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2014 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1-888-ASK-USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Suggested citation: Birchler, J.J., Stockdon, H.F., Doran, K.S., and Thompson, D.M., 2014, National assessment of hurricane-induced coastal erosion hazards—Northeast Atlantic Coast: U.S. Geological Survey Open-File Report 2014–1243, 34 p., http://dx.doi.org/10.3133/ofr20141243. ISSN 2331-1258 (online) ii Contents 1. Introduction ............................................................................................................................................................. 1 1.1 Impacts of Hurricanes on Coastal Communities ............................................................................................... 1 1.2 Prediction of Hurricane-Induced Coastal Erosion.............................................................................................. 4 1.3 Storm-Impact Scaling Model ............................................................................................................................. 4 2. -
Historical Perspective
kZ _!% L , Ti Historical Perspective 2.1 Introduction CROSS REFERENCE Through the years, FEMA, other Federal agencies, State and For resources that augment local agencies, and other private groups have documented and the guidance and other evaluated the effects of coastal flood and wind events and the information in this Manual, performance of buildings located in coastal areas during those see the Residential Coastal Construction Web site events. These evaluations provide a historical perspective on the siting, design, and construction of buildings along the Atlantic, Pacific, Gulf of Mexico, and Great Lakes coasts. These studies provide a baseline against which the effects of later coastal flood events can be measured. Within this context, certain hurricanes, coastal storms, and other coastal flood events stand out as being especially important, either Hurricane categories reported because of the nature and extent of the damage they caused or in this Manual should be because of particular flaws they exposed in hazard identification, interpreted cautiously. Storm siting, design, construction, or maintenance practices. Many of categorization based on wind speed may differ from that these events—particularly those occurring since 1979—have been based on barometric pressure documented by FEMA in Flood Damage Assessment Reports, or storm surge. Also, storm Building Performance Assessment Team (BPAT) reports, and effects vary geographically— Mitigation Assessment Team (MAT) reports. These reports only the area near the point of summarize investigations that FEMA conducts shortly after landfall will experience effects associated with the reported major disasters. Drawing on the combined resources of a Federal, storm category. State, local, and private sector partnership, a team of investigators COASTAL CONSTRUCTION MANUAL 2-1 2 HISTORICAL PERSPECTIVE is tasked with evaluating the performance of buildings and related infrastructure in response to the effects of natural and man-made hazards. -
A Pictoral History of the Boston Music Hall and the Great Organ
A PICTORIAL HISTORY OF THE BOSTON MUSIC HALL AND THE GREAT ORGAN by Ed Sampson, President, Methuen Memorial Music Hall, Inc. 2018 Few instruments in the history of pipe organs in America have had as long, or as distinguished, a career as the Boston Music Hall Organ. The first concert organ in the country, it remains today one of the outstanding organs in America. The need for a large and centrally-located concert hall for Boston was discussed at the annual meeting of the Harvard Musical Association, founded in 1837 (Henry White Pickering (1811-1898), President) on January 31, 1851. A "Music Hall Committee", comprised of members Robert East Apthorp (1812-1882), George Derby (1819-1874), John Sullivan Dwight (1813-1893), Charles Callahan Perkins (1822-1886), and Dr. Jabez Baxter Upham (1820- 1902), was appointed to address the matter. The Boston Music Hall was built in 1852 by the Boston Music-Hall Association, founded in 1851 (Jabez Baxter Upham, President) and by the Harvard Musical Association, that contributed $100,000 towards its construction. It stood in the center of a block that sloped downward from Tremont Street to Washington Street; and was between Winter Street on the south and Bromfield Street on the north. Almost entirely surrounded by other buildings, only glimpses of the hall's massive granite block foundation and plain brick walls could be seen. There were two entrances to the Music Hall: the Bumstead Place entrance, (named after Thomas Bumstead (1740-1828) a Boston coachmaker), off Tremont Street (later Hamilton Place) opposite the Park Street Church; 1 and the Central Place or Winter Place (later Music Hall Place) entrance off Winter Street. -
The Perfect Storm
The Perfect Storm A True Story of Men Against the Sea by Sebastian Junger Contents FOREWORD GEORGES BANK, 1896 GLOUCESTER, MASS., 1991 GOD’S COUNTRY THE FLEMISH CAP THE BARREL OF THE GUN GRAVEYARD OF THE ATLANTIC THE ZERO-MOMENT POINT THE WORLD OF THE LIVING INTO THE ABYSS THE DREAMS OF THE DEAD AFTERWORD ACKNOWLEDGMENTS THIS BOOK IS DEDICATED TO MY FATHER, WHO FIRST INTRODUCED ME TO THE SEA. FOREWORD Recreating the last days of six men who disappeared at sea presented some obvious problems for me. On the one hand, I wanted to write a completely factual book that would stand on its own as a piece of journalism. On the other hand, I didn’t want the narrative to asphyxiate under a mass of technical detail and conjecture. I toyed with the idea of fictionalizing minor parts of the story—conversations, personal thoughts, day-to-day routines—to make it more readable, but that risked diminishing the value of whatever facts I was able to determine. In the end I wound up sticking strictly to the facts, but in as wide-ranging a way as possible. If I didn’t know exactly what happened aboard the doomed boat, for example, I would interview people who had been through similar situations, and survived. Their experiences, I felt, would provide a fairly good description of what the six men on the Andrea Gail had gone through, and said, and perhaps even felt. As a result, there are varying kinds of information in the book. Anything in direct quotes was recorded by me in a formal interview, either in person or on the telephone, and was altered as little as possible for grammar and clarity. -
Impact of Parameterized Boundary Layer Structure on Tropical Cyclone Rapid Intensification Forecasts in HWRF
APRIL 2017 Z H A N G E T A L . 1413 Impact of Parameterized Boundary Layer Structure on Tropical Cyclone Rapid Intensification Forecasts in HWRF JUN A. ZHANG NOAA/Atlantic Oceanographic and Meteorological Laboratory/Hurricane Research Division, and Cooperative Institute for Marine and Atmospheric Studies, University of Miami, Miami, Florida ROBERT F. ROGERS NOAA/Atlantic Oceanographic and Meteorological Laboratory/Hurricane Research Division, Miami, Florida VIJAY TALLAPRAGADA NOAA/NWS/NCEP/Environmental Modeling Center, College Park, Maryland (Manuscript received 5 April 2016, in final form 27 October 2016) ABSTRACT This study evaluates the impact of the modification of the vertical eddy diffusivity (Km) in the boundary layer parameterization of the Hurricane Weather Research and Forecasting (HWRF) Model on forecasts of tropical cyclone (TC) rapid intensification (RI). Composites of HWRF forecasts of Hurricanes Earl (2010) and Karl (2010) were compared for two versions of the planetary boundary layer (PBL) scheme in HWRF. The results show that using a smaller value of Km, in better agreement with observations, improves RI forecasts. The composite-mean, inner-core structures for the two sets of runs at the time of RI onset are compared with observational, theoretical, and modeling studies of RI to determine why the runs with reduced Km are more likely to undergo RI. It is found that the forecasts with reduced Km at the RI onset have a shallower boundary layer with stronger inflow, more unstable near-surface air outside the eyewall, stronger and deeper updrafts in regions farther inward from the radius of maximum wind (RMW), and stronger boundary layer convergence closer to the storm center, although the mean storm intensity (as measured by the 10-m winds) is similar for the two groups.