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![Jeff Donnelly [Jdonnelly@Whoi.Edu] Sent: Friday, April 28, 2006 4:55 PM To: Foley@Mvcommission.Org Subject: Re: Martha's Vineyard and Hurricanes](https://docslib.b-cdn.net/cover/1959/jeff-donnelly-jdonnelly-whoi-edu-sent-friday-april-28-2006-4-55-pm-to-foley-mvcommission-org-subject-re-marthas-vineyard-and-hurricanes-61959.webp)
Jeff Donnelly [[email protected]] Sent: Friday, April 28, 2006 4:55 PM To: [email protected] Subject: Re: Martha's Vineyard and Hurricanes
From: Jeff Donnelly [[email protected]] Sent: Friday, April 28, 2006 4:55 PM To: [email protected] Subject: Re: Martha's Vineyard and Hurricanes Hi Paul... The current hospital location is relatively safe from hurricanes making landfall to the west of Martha's Vineyard. For example storm surge from the 1938 hurricane at that location was between 4 and 6 feet. The location is much more susceptible to nor'easters. You might get 6 feet of surge associated with an intense nor'easter potentially with some large waves on top of that. However, my biggest concern is if an intense hurricane were to slowly pass to the east of the island. This would result in strong north and northeast winds that could pile significant storm surge and waves into Vineyard Haven Harbor. The October 3, 1841 hurricane was just such a storm. One of the key factors is the forward motion of the storm. If the storm track is to the east of the island and it is moving rapidly the speed of forward motion would be subtracted from the rotary winds of the west side of the storm and the duration of strong winds would be less (a couple of hours or less). If the storm moves slowly the duration of onshore hurricane force winds could be more like 6 to 10 hours. In this scenario the hospital might be in peril. You could get between 10 and 15 feet of storm surge in Vineyard Haven Harbor during such an event. From my read of the topographic map it looks like the hospital is between 10 and 20 feet above sea level. -
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. -
Hurricane Skirts Shore, Rips New England Coast Cape Cod Damage in Line Here Is of Storm Minor
Distribufion Weatkei Today N ctonta by tt f M)BANK 17,475 MMtiyV toolfht ud Friday. Hl|fc today Jl; kw tw!|ht •«; twnorrair 75-». tee weather, I UOHBAV THMVCU /MD*Y-t8T. OH Dial SH I-0010 • M» •>« Kin et Iiiutd tally, ICooAiy uuoatfi Friday. Secocd CUM Fonts* RED BANK, N: J., THURSDAY, SEPTEMBER 21, 1961 7c PER COPY VOL. 84, NV). 61 puj it K«d Bank ml at Additional ltallliv Officu. PAGE ONE Dressing for Date—With Esther ¥&%' Hurricane Skirts Shore, Rips New England Coast Cape Cod Damage In Line Here Is Of Storm Minor BOSTON (AP) — Hurri- Gale winds, rain, and cane Esther's furious winds tides, two to. three feet aimed today at Cape Cod, above normal were Mon- site of the Summer White mouth County's experience . House at Hyannis Port. as Hurricane Esther's fly- Waterfront resident, and ^ packing wjnds up U{ ing skirts brushgtt-the area boat own.r, made mighty^ ^ . afl hour> hurf early today. preparation* yeiterday a. tnejcan). ^^ g drivjng rajn jn,0 shore are* was placed on|the southern New England The shore region was hurricane watch. William coastal area. Winds mounted pared the brunt of the ca- pricious storm when it hourly as the storm approached. eered slightly to the east from The center of the storm was its earlier northward bearing Bright, having already board- 65 miles south of Block Island, R. I., at 6 a.m. 'esterday. Mid-morning advi- sories indicated it .would slam Gusts as high as 90 miles an entrance to his property with hour were reported at Montauk Into the eastern New England sand bags in photo above. -
S Goddard Space F Light Center Earth Sciences Division: Atmospheres
Earth Sciences Division: Atmospheres Space Flight Goddard Center NASA’s Deputy Director for Atmospheres Dr. Steven Platnick [email protected] Associate Deputy Director for Atmospheres Dr. Emily Wilson [email protected] Mesoscale Atmospheric Processes Laboratory Chief: Dr. George Huffman [email protected] Climate and Radiation Laboratory Chief: Dr. Lazaros Oreopoulos [email protected] Atmospheric Chemistry and Dynamics Laboratory Chief: Dr. James Gleason [email protected] Earth Sciences Wallops Field Support Office Chief: David B. Wolff [email protected] National Aeronautics and Space Administration Aura D3R/ NPOL GPM GPS III Precipitation Accumulation Nitrogen Dioxide Change 2005 2016 Earth Sciences: Atmospheres Goddard Space Flight Center Sciences and Exploration Directorate Dr. Steven Platnick is the Deputy Director for Atmospheres at NASA’s Goddard Space Flight Center’s Earth Sciences Division (Code 610). He received B.S. and M.S. degrees in electrical engineering from Duke University and the University of California, Berkeley, respectively, and a Ph.D. in atmospheric sciences from the University of Arizona. Dr. Platnick’s research focuses on theoretical and experimental cloud remote sensing studies from satellite and aircraft observations. He has worked extensively on the development of NASA satellite cloud optical and microphysical data products, from the Moderate Resolution Imaging Spectroradiometer (MODIS), the Visible Infrared Imaging Radiometer Suite (VIIRS), and other imagers. Dear Readers: This brochure provides an overview of the portion of Earth atmospheric science activities at Goddard that comprise the Earth Sciences Division’s Atmospheres organization (Code 610AT). Inside you will find descriptions of our scope of work, our people and facilities, our place in NASA’s mission, and examples of recent accomplishments. -
A High-Resolution Paleoenvironmental and Paleoclimatic History of Extreme Events on the Laminated Sediment Record from Basin Pond, Fayette, Maine, U.S.A
University of Massachusetts Amherst ScholarWorks@UMass Amherst Masters Theses Dissertations and Theses November 2015 A High-Resolution Paleoenvironmental and Paleoclimatic History of Extreme Events on the Laminated Sediment Record from Basin Pond, Fayette, Maine, U.S.A. Daniel R. Miller University of Massachusetts Amherst Follow this and additional works at: https://scholarworks.umass.edu/masters_theses_2 Part of the Biogeochemistry Commons, Climate Commons, Geochemistry Commons, Other Environmental Sciences Commons, and the Sedimentology Commons Recommended Citation Miller, Daniel R., "A High-Resolution Paleoenvironmental and Paleoclimatic History of Extreme Events on the Laminated Sediment Record from Basin Pond, Fayette, Maine, U.S.A." (2015). Masters Theses. 286. https://doi.org/10.7275/7416079 https://scholarworks.umass.edu/masters_theses_2/286 This Open Access Thesis is brought to you for free and open access by the Dissertations and Theses at ScholarWorks@UMass Amherst. It has been accepted for inclusion in Masters Theses by an authorized administrator of ScholarWorks@UMass Amherst. For more information, please contact [email protected]. A HIGH-RESOLUTION PALEOENVIRONMENTAL AND PALEOCLIMATIC HISTORY OF EXTREME EVENTS ON THE LAMINATED SEDIMENT RECORD FROM BASIN POND, FAYETTE, MAINE, U.S.A. A Thesis Presented by DANIEL R. MILLER Submitted to the Graduate School of the University of Massachusetts Amherst in partial fulfillment of the requirements for the degree of MASTERS OF SCIENCE September 2015 Department of Geosciences © Copyright by Daniel R. Miller 2015 All Rights Reserved A HIGH-RESOLUTION PALEOENVIRONMENTAL AND PALEOCLIMATIC HISTORY OF EXTREME EVENTS ON THE LAMINATED SEDIMENT RECORD FROM BASIN POND, FAYETTE, MAINE, U.S.A. A Thesis Presented by DANIEL R. -
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. -
U.S. Coast Guard History Program Disasters Finding
U.S. Coast Guard History Program Disasters Finding Aid Box 1 A.W. Gill – 5 January 1980 A.W. Gill – 5 January 1980 – News Clippings A.W. Gill – 5 January 1980 – Photographs Aaron – 2 September 1971 AC33 Barge – 18 August 1976 AC33 Barge – 18 August 1976 – Photographs AC 38 – 1 August 1980 AC 38 – 1 August 1980 – Photographs Acapulco – 22 December 1961 Acapulco – 22 December 1961 – News Clippings Achille Lauro – 30 November 1994 – News Clippings Achilles – 9 January 1968 Aco 44 – 9 November 1975 Adlib II – 9 October 1971 Adlib II – 9 October 1971 – News Clippings Addiction – 19 April 1995 Admiral – 5 April 1998 Admiral – 5 April 1998 – News Clippings Adriana – 28 July 1977 Adriatic – 18 January 1999 Adriatic – 18 January 1999 – News Clippings Advance – 16 May 1985 Advent – 18 February 1913 – Photographs Adventurer – 16 April 1983 Adventurer – 16 April 1983 – Photographs Aegean Sea – 10 September 1977 – Photographs Aegis Duty – 4 December 1973 – News Clippings Aegis Duty – 4 December 1973 – Photographs Aeolus – 24 August 1974 Aeolus – 24 August 1974 – News Clippings Aeolus – 24 August 1974 – Photographs Afala – 24 January 1976 1 Afala – 24 January 1976 – News Clippings Affair – 4 November 1985 Afghanistan – 20 January 1979 Afghanistan – 20 January 1979 – News Clippings Agnes – 27 October 1985 Box 2 African Dawn – 5 January 1959 – News Clippings African Dawn – 5 January 1959 – Photographs African Neptune – 7 November 1972 African Queen – 30 December 1958 African Queen – 30 December 1958 – News Clippings African Queen – 30 December 1958 – Photographs African Star-Midwest Cities Collision – 16 March 1968 Agattu – 31 December 1979 Agattu – 31 December 1979 Box 3 Agda – 8 November 1956 – Photographs Ahad – n.d. -
Climatology of Tropical Cyclones in New England and Their Impact at the Blue Hill Observatory, 1851-2012
Climatology of Tropical Cyclones in New England and Their Impact at the Blue Hill Observatory, 1851-2012 Michael J. Iacono Blue Hill Meteorological Observatory Updated September 2013 Introduction Over the past four centuries, extreme hurricanes have occurred in New England at intervals of roughly 150 years, as evidenced by the three powerful storms of 1635, 1815, and 1938. Histories and personal accounts of these infamous hurricanes make for fascinating reading (Ludlum, 1963; Minsinger, 1988), and they serve as an important reminder of the devastating impact that tropical cyclones can have in the Northeast. Most tropical systems in New England are less damaging, but they can still disrupt our daily lives with strong winds, heavy rain, and flooding. This article, which updates an earlier report in the Blue Hill Observatory Bulletin (Iacono, 2001), will describe the climatology of all 250 tropical cyclones that have affected New England since the mid-19th century and will summarize their intensity, frequency, and specific meteorological impact at the Blue Hill Observatory. A hurricane is a self-sustaining atmospheric process in which sunlight, water, and wind combine to transfer energy from the tropics to higher latitudes. The uneven distribution of solar heating at the Earth’s surface ultimately drives much of our weather as the atmosphere continually circulates to equalize the tropical warmth and the polar cold. In the tropics, this process is normally tranquil and slow, brought about through the life cycles of individual thunderstorms, the prevailing winds, and ocean currents. However, under the right conditions very warm air and water in the tropics trigger the formation of the most efficient heat transfer mechanism available to the atmosphere: a hurricane. -
DOCUMENT RESUME ED 088 518 IR 000 359 TITLE Film Catalog of The
DOCUMENT RESUME ED 088 518 IR 000 359 TITLE Film Catalog of the New York State Library. 1973 Supplement. INSTITUTION New York State Education Dept., Albany. Div. of Library Development. PUB DATE 73 NOTE 228p. EDRS PRICE MF-$0.75 HC-$11.40 DESCRIPTORS *Catalogs; Community Organizations; *Film Libraries; *Films; *Library Collections; Public Libraries; *State Libraries; State Programs IDENTIFIERS New York State; New York State Division of Library Development; *New York State Library ABSTRACT Several hundred films contained in the New York State Division of Library Development's collection are listed in this reference work. The majority of these have only become available since the issuance of the 1970 edition of the "Catalog," although a few are older. The collection covers a wide spectrum of subjects and is intended for nonschcol use by local community groups; distribution is accomplished through local public libraries. Both alphabetical and subject listings are provided and each"citation includes information about the film's running time, whether it is in color, its source, and its date. Brief annotations are also given which describe the content of the film and the type of audience for which it is appropriate. A directory of sources is appended. (PB) em. I/ I dal 411 114 i MI1 SUPPLEMENT gilL""-iTiF "Ii" Alm k I I II 11111_M11IN mu CO r-i Le, co co FILM CATALOG ca OF THE '1-1-1 NEW YORK STATE LIBRARY 1973 SUPPLEMENT THE UNIVERSITY OF THE STATE OF NEW YORK THE STATE EDUCATION DEPARTMENT ALBANY, 1973 THE UNIVERSITY OF THE STATE OF NEW YORK Regents of the University ( with years when terms expire) 1984 JOSEPH W. -
P3.4 the Distribution of Precipitation Over the Northeast Accompanying Landfalling and Transitioning Tropical Cyclones
20th Conf. on Weather Analysis and Forecasting Seattle, WA, 11–15 January 2004 P3.4 The Distribution of Precipitation over the Northeast Accompanying Landfalling and Transitioning Tropical Cyclones David P. DeLuca*, Lance F. Bosart, Daniel Keyser University at Albany, State University of New York, Albany, New York and David R. Vallee National Weather Service Forecast Office, Taunton, Massachusetts 1. INTRODUCTION United States. Approximately 3500 surface stations were analyzed for each storm period (currently: 1950– Landfalling and transitioning tropical cyclones 1991) by Ron Horwood of NWS WFO Taunton, MA. pose a significant heavy precipitation forecast challenge Obvious erroneous data were removed to obtain the most over the northeastern United States. The forecast accurate analyses possible. challenge is heightened because the heavy rainfall distribution associated with these tropical cyclones can A subset of eight storms (Fig. 1) where the be modulated significantly when the poleward-moving precipitation distribution is possibly influenced by storms interact with mobile midlatitude upper-level coastal frontogenesis was chosen from well–documented troughs and coastal fronts over regions of complex or famous cases. Detailed analyses were conducted terrain. The purpose of this paper is to document the using the four times daily (0000, 0600, 1200 and 1800 large spatial and temporal variability of heavy UTC) NCEP/NCAR reanalysis dataset (Kalnay et al. precipitation that accompanies landfalling and 1996; Kistler et al. 2001) and archived DIFAX surface transitioning tropical cyclones, and to determine the charts in an attempt to elucidate both synoptic and physical basis for the observed rainfall distribution. mesoscale processes. 2. METHODOLOGY 3. RESULTS A 38-storm dataset (Fig. -
Aspects of Hurricane Structure: New Model
MONTHLY - REVIEW VOLUME 92, NUMBER 2 FEBRUARY 4 964 BECBS OF WURRl STRUCUURE: NE SUGGESTED BY AND SWOJECU ERCUWY OBSERVATIO ROBERT W. FETT’ Air Weather Service Member, National Weather Satellite Center, U.S. Weather Bureau, Washington, D.C. ABSTRACT Satellite photographs of hurricanes reveal the complete storm in relationship to its environmcnt. In many instances “outer convective bands” or “pre-hurricane squall lnes” appear to partially “ring” the storm. These bands are usually separated from the rim of thc high cloud shield by a relatively clear channel, visible and distinct for long distances along the circumference. This channel may be formed through the action of a major subsiding branch of the hurricane’s circulation. Many photographs also reveal extensive areas of convective, cirrus-producing cloudiness in the wake of the storm. This cloudiness appears to be intimately associated with that of the hurricane, and strongly influenced by outflow effects. Time cross.section analyses of hurricanes Carla and Anna suggest peripheral subsidence. The area of possible subsidence, in both instances, occurred under an upper shear line, where air diverging in the outflow layer from the hurricane converged with air emanating from the subtropical High. A jet stream, in the case of hurricane Carla, appeared in the region of the subsident annular zone, at the edge of the high cloud shield. This high speed current curved anticyclonically along the northern quadrants of the storm-then, on being directed southward, split into two main branches. The eastern branch curved cyclonically into a trailing vortex, apparent as a cold Low at 200 mb. The western branch continued southward, in alignment with the curvature of cloud streaks forming the cirrus “tail” of hurricane Carla. -
Survivors' Recount Fiery Last Moments of KA
JJNIV1:KS1l'I' OF HAWAll UBRJUl arianas %rietYr;~ Micronesia's Leading Newspaper Since 1972 ~ ews Boria.. slams Gov.· Tenorio's status overtures: oto public' By Zaldy Dandan that happening. dependent Northern Marianas. make it clear to Congress that his "But we're adults, and we Variety News Staff Most of the local residents "It's his personal opinion, and "request" for an independent or a should sit down, negotiate and try ONLY the people of the CNMI would prefer that the CNMI re it should stay that way-it is not freely associated state status is his to arrive at a compromise." can ask the United States to grant main in political union with the the opinion of a majority of the (Tenorio) opinion alone. In a media conference Wednes independence to the Northern Unites States, Borja said, react people," Borja, who is running Borja, at the same, reiterated day, Tenorio said if the Clinton Marianas, and Lt. Gov. Jesus C. ing to Gov. Froilan C. Tenorio's against Tenorio, said. that CNMI should pursue nego administration continues to insist Borja yesterday said he can't see statement Wednesday on an in- The governor, he added, shou Id tiations with the Clinton adminis on the federalization of the tration through the Covenant Sec CNMI's immigration and mini tion 902 talks. mum wage policies, he would ask "We should state our position Congress to grant independence in a reasonable and cogent man or a "freely associated state" sta ner," he said. tus to the Northern Marianas. Tenorio' s "attitude," Borja said, He said the CNMI will survive "is, 'If you make me angry I'll being independent, but not with take the marbles and go home.' Continued on page 54 Survivors' recount fiery last moments of KA 801 By JU-YEON KIM it went down in a heavy rain , AGANA, Guam (AP) - A Ko storm on approach to the air rean Air jetliner shook viole!1tly port.