2015 All-Hazards Mitigation Plan Update Kent County, Delaware
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Aids to Navigation Tended by USLHS/USCG Tender Lilac
Aids to Navigation Tended by USLHS/USCG Tender Lilac Note: For her entire operational career, the lighthouse/buoy tender Lilac was assigned to tend aids to navigation in the Delaware Bay and Delaware River as part of the old 4th District, and later 3rd District. Due to her navigational draft of 9.5ft., she likely tended aids that were at and below the Port of Philadelphia/Wilmington, while a smaller tender tended aids in the shallower waters upriver and along the shorelines. Lightships Overfalls Lighthouses Delaware Breakwater Delaware Breakwater West End Harbor of Refuge Harbor of Refuge North End Brandywine Shoal Fourteen-Foot Bank Miah Maull Shoal Elbow of Cross Ledge Ship John Shoal Ranges Liston Front Baker Front Reedy Island Front Cherry Island Front Marcus Hook Front Chester Front Minor Lights Reedy Island Jetty Hope Creek Jetty Old Reedy Island Fort Delaware Pea Patch Island Finns Point Jetty Block Island Broadkill Mispillion South Jetty Delaware City Aids to Navigation Tended by USLHS/USCG Tender Lilac (cont’d) Major Lighted Buoys 9x38 size lighted (acetylene gas or electric) buoys at McCrie Shoal, Hen and Chickens, Brown Shoal, and Ben Davis Point Shoal Aids to Navigation Tended by USLHS/USCG Tender Lilac (cont’d) Major Lighted Buoys 8x23 or 8x26 size lighted (acetylene gas or electric) buoys at Brandywine Lump, Joe Flogger Shoal, Hog Shoal, Liston Range Channel, Baker Range Channel, Reedy Island Range Channel, Finns Point Range Channel, New Castle Range Channel, Bulkhead Bar Range Channel, Deepwater Point Range Channel, Cherry Island Range Channel, Bellevue Range Channel, Marcus Hook Range Channel, Schooner Ledge Rock, Horseshoe Shoal, and Stony Point Aids to Navigation Tended by USLHS/USCG Tender Lilac (cont’d) Tender Lilac was based for many years at the U.S. -
Bridge Index
Co Br# Page Facility Carried Featured Intersedtion Co Br# Page Facility Carried Featured Intersedtion 1 001 12 2-G RISING SUN RD BRANDYWINE CREEK 1 087 9 10-C SNUFF MILL RD BURRIS RUN 1 001A 12 2-G RISING SUN RD BRANDYWINE CREEK 1 088 9 10-C SNUFF MILL RD TRIB OF RED CLAY CREEK 1 001B 12 2-F KENNETT PIKE WATERWAY & ABANDON RR 1 089 9 10-C SNUFF MILL RD. WATERWAY 1 002 9 12-G ROCKLAND RD BRANDYWINE CREEK 1 090 9 10-C SNUFF MILL RD. WATERWAY 1 003 9 11-G THOMPSON BRIDGE RD BRANDYWINE CREEK 1 091 9 10-C SNUFF MILL RD. WATERWAY 1 004P 13 3-B PEDESTRIAN NORTHEAST BLVD 1 092 9 11-E KENNET PIKE (DE 52) 1 006P 12 4-G PEDESTRIAN UNION STREET 1 093 9 10-D SNUFF MILL RD WATERWAY 1 007P 11 8-H PEDESTRIAN OGLETOWN STANTON RD 1 096 9 11-D OLD KENNETT ROAD WATERWAY 1 008 9 9-G BEAVER VALLEY RD. BEAVER VALLEY CREEK 1 097 9 11-C OLD KENNETT ROAD WATERWAY 1 009 9 9-G SMITHS BRIDGE RD BRANDYWINE CREEK 1 098 9 11-C OLD KENNETT ROAD WATERWAY 1 010P 10 12-F PEDESTRIAN I 495 NB 1 099 9 11-C OLD KENNETT RD WATERWAY 1 011N 12 1-H SR 141NB RD 232, ROCKLAND ROAD 1 100 9 10-C OLD KENNETT RD. WATERWAY 1 011S 12 1-H SR 141SB RD 232, ROCKLAND ROAD 1 105 9 12-C GRAVES MILL RD TRIB OF RED CLAY CREEK 1 012 9 10-H WOODLAWN RD. -
2014 North Atlantic Hurricane Season Review
2014 North Atlantic Hurricane Season Review WHITEPAPER Executive Summary The 2014 Atlantic hurricane season was a quiet season, closing with eight 2014 marks the named storms, six hurricanes, and two major hurricanes (Category 3 or longest period on stronger). record – nine Forecast groups predicted that the formation of El Niño and below consecutive years average sea surface temperatures (SSTs) in the Atlantic Main – that no major Development Region (MDR)1 through the season would inhibit hurricanes made development in 2014, leading to a below average season. While 2014 landfall over the was indeed quiet, these predictions didn’t materialize. U.S. The scientific community has attributed the low activity in 2014 to a number of oceanic and atmospheric conditions, predominantly anomalously low Atlantic mid-level moisture, anomalously high tropical Atlantic subsidence (sinking air) in the Main Development Region (MDR), and strong wind shear across the Caribbean. Tropical cyclone activity in the North Atlantic basin was also influenced by below average activity in the 2014 West African monsoon season, which suppressed the development of African easterly winds. The year 2014 marks the longest period on record – nine consecutive years since Hurricane Wilma in 2005 – that no major hurricanes made landfall over the U.S., and also the ninth consecutive year that no hurricane made landfall over the coastline of Florida. The U.S. experienced only one landfalling hurricane in 2014, Hurricane Arthur. Arthur made landfall over the Outer Banks of North Carolina as a Category 2 hurricane on July 4, causing minor damage. While Mexico and Central America were impacted by two landfalling storms and the Caribbean by three, Bermuda suffered the most substantial damage due to landfalling storms in 2014.Hurricane Fay and Major Hurricane Gonzalo made landfall on the island within a week of each other, on October 12 and October 18, respectively. -
Hurricane and Tropical Storm
State of New Jersey 2014 Hazard Mitigation Plan Section 5. Risk Assessment 5.8 Hurricane and Tropical Storm 2014 Plan Update Changes The 2014 Plan Update includes tropical storms, hurricanes and storm surge in this hazard profile. In the 2011 HMP, storm surge was included in the flood hazard. The hazard profile has been significantly enhanced to include a detailed hazard description, location, extent, previous occurrences, probability of future occurrence, severity, warning time and secondary impacts. New and updated data and figures from ONJSC are incorporated. New and updated figures from other federal and state agencies are incorporated. Potential change in climate and its impacts on the flood hazard are discussed. The vulnerability assessment now directly follows the hazard profile. An exposure analysis of the population, general building stock, State-owned and leased buildings, critical facilities and infrastructure was conducted using best available SLOSH and storm surge data. Environmental impacts is a new subsection. 5.8.1 Profile 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 (National Oceanic and Atmospheric Administration [NOAA] 2013a). 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. -
Town of Little Creek, Delaware Comprehensive Plan
TownTown ofof LittleLittle Creek,Creek, DelawareDelaware ComprehensiveComprehensive PlanPlan July 2006 Prepared by The Town of Little Creek Planning Commission With assistance from the Delaware Office of State Planning Coordination Little Creek, Delaware Comprehensive Plan Adopted by the Little Creek Planning Commission In December 2005; and by the Little Creek Town Council July 2006 Prepared by: The Town of Little Creek Planning Commission With assistance from the: Delaware Office of State Planning Coordination August 28, 2006 The Honorable Harry E. Marvel, Sr. Mayor, Town of Little Creek P.O. Box 298 Little Creek, DE 19961 RE: Certification of the Town of Little Creek Comprehensive Plan Dear Mayor Marvel: I am pleased to inform the Town that as of August 7, 2006 per the recommendation of the Office of State Planning Coordination, the comprehensive plan for the Town of Little Creek is hereby certified provided no major changes are enacted. The certification signifies that the comprehensive plan is currently in compliance with State Strategies. I would like to take this opportunity to thank the Town of Little Creek for working with the State to incorporate our recommendations into the plan before adoption. My staff and I look forward to working with the Town to accomplish the goals set forth in your plan. Congratulations on your certification! Sincerely, Constance C. Holland Director Town of Little Creek Comprehensive Plan TABLE OF CONTENTS TOWN, COUNTY, AND STATE OFFICIALS.................................................................................... -
Hurricane Strike!
Your Name(s): ____________________________ Hurricane Strike! Goto The Hurricane Strike Learning Module at http://www.meted.ucar.edu/hurrican/strike/index.htm Here’s a youtube introduction to the Hurricane Strike Environment. (5 minutes) (note: the video and this document assume that you are using the multimedia version of this activity. Some students prefer the text version. ) Science Worksheet 1 (select Sunday) Watch the Weather Channel News Flash (on the Castillos’ TV) and look in Storm Track (on the Castillos’ laptop computer) to answer questions 1–3: 1. Where was Tropical Storm Erin at 8:00 PM on Sunday, July 30th? (Fill in the blanks with latitude and longitude numbers and identify N, S, E, or W for each. If you have a tracking chart, plot the location.) Latitude: __ __ . __ N S E W Longitude: __ __ . __ N S E W 2. Which place was closest to the center of Tropical Storm Erin? (identify one) Cuba Florida Mexico The Turks & Caicos 3. Tropical Storm Erin’s winds are gusting to 60 mph. How many kilometers per hour (kph) is that, if 1 mph equals 1.61 kph? _______ kph Look in Hurricanes and tropical Cyclones to answer questions 4–11: 4. Tropical storms that begin in the Atlantic Ocean north of the equator form near the … (identify one) Tropic of Cancer Tropic of Capricorn 5. Hurricanes can’t strike places in the northern part of the U.S., like New York. (identify one) TRUE FALSE 6. If you lived in Japan, what would you call hurricanes? (Fill in the blank.) _______________________________ 7. -
! 1! NASA's Hurricane and Severe Storm Sentinel (HS3) Investigation
https://ntrs.nasa.gov/search.jsp?R=20170005486 2019-08-31T16:22:19+00:00Z 1! NASA’s Hurricane and Severe Storm Sentinel (HS3) Investigation 2! 3! Scott A. Braun, Paul A. Newman, Gerald M. Heymsfield 4! NASA Goddard Space Flight Center, Greenbelt, Maryland 5! 6! Submitted to Bulletin of the American Meteor. Society 7! October 14, 2015 8! 9! 10! 11! Corresponding author: Scott A. Braun, NASA Goddard Space Flight Center, Code 612, 12! Greenbelt, MD 20771 13! Email: [email protected] 14! ! 1! 15! Abstract 16! The National Aeronautics and Space Administrations’s (NASA) Hurricane and Severe Storm 17! Sentinel (HS3) investigation was a multi-year field campaign designed to improve understanding 18! of the physical processes that control hurricane formation and intensity change, specifically the 19! relative roles of environmental and inner-core processes. Funded as part of NASA’s Earth 20! Venture program, HS3 conducted five-week campaigns during the hurricane seasons of 2012-14 21! using the NASA Global Hawk aircraft, along with a second Global Hawk in 2013 and a WB-57f 22! aircraft in 2014. Flying from a base at Wallops Island, Virginia, the Global Hawk could be on 23! station over storms for up to 18 hours off the East Coast of the U.S. to about 6 hours off the 24! western coast of Africa. Over the three years, HS3 flew 21 missions over 9 named storms, along 25! with flights over two non-developing systems and several Saharan Air Layer (SAL) outbreaks. 26! This article summarizes the HS3 experiment, the missions flown, and some preliminary findings 27! related to the rapid intensification and outflow structure of Hurricane Edouard (2014) and the 28! interaction of Hurricane Nadine (2012) with the SAL. -
Cultural Contexts
3.0 CULTURAL CONTEXTS 3.0 CULTURAL CONTEXTS 3.1 PRE-COLONIAL PERIOD OVERVIEW The following brief, general discussion provides an outline of the prehistoric cultural record of the Delmarva Peninsula as it is currently understood (e.g., Custer 1984a, 1986a, 1987, 1989, 1994; Thomas et al. 1975). The prehistoric archeological record of the Delmarva Peninsula can be divided into five major periods: • the Paleoindian Period (circa 14,000 - 8,500 yrs. BP); • the Archaic Period (8,500 - 5,000 yrs. BP); • the Woodland I Period (5,000 - 1,000 yrs. BP); • the Woodland IT Period (1,000 - 350 yrs. BP; and • the Contact Period (A.D. 1650 - A.D. 1700). 3.1.1 PALEOINDlAN PERIOD Native Americans first inhabited Delaware sometime after 14,000 yrs. BP, based on dates from Paleoindian period sites in the eastern United States (Custer 1989:81-86). It is believed that small family groups of Paleoindians lived a wandering existence, hunting in the shifting woodland and grassland mosaic of the time. Game animals may have included musk ox, caribou, moose, and the extinct mastodon; however, modem game animals, such as white-tailed deer, were also present in the region (Custer 1989:95-98). Skeletal evidence of extinct megafauna (mastodon, mammoth) and large northern mammals (e.g., moose, caribou) has been recovered from the drowned continental shelves of the Middle Atlantic region (Emory 1966; Emory and Edwards 1966; Edwards and Merrill 1977). The Paleoindian stone tool kit was designed for hunting and processing animals. Wild plant foods supplemented the diet. Distinctive "fluted" points, characteristic of the early Paleoindian period, show a preference for high quality stone (Custer 1984b). -
Summary Report to the City of Milford
MilfordSummary_cover_Layout 1 12/13/12 12:24 PM Page 1 Planning for Complete Communities in Delaware Summary Report to the City of Milford aHractive, inclusive, efficient, healthy & resilient places December 2012 written by Marcia Scott and Natasha Nau with contributions by Christopher Anderson project co-managed by Marcia Scott and Theodore Patterson Institute for Public Administration School of Public Policy & Administration College of Arts & Sciences University of Delaware www.ipa.udel.edu serving the public good, shaping tomorrow’s leaders in collaboration with the Delaware Office of State Planning Coordination and funded by the Delaware Department of Transportation Planning for Complete Communities in Delaware: Summary Report to the City of Milford December 2012 written by Marcia Scott, Associate Policy Scientist Natasha Nau, Public Administration Fellow with contributions from Christopher Anderson, Public Administration Fellow project co-managed by Marcia Scott, Associate Policy Scientist Theodore Patterson, Limited-Term Researcher published by Institute for Public Administration School of Public Policy and Administration College of Arts and Sciences University of Delaware www.ipa.udel.edu serving the public good, shaping tomorrow’s leaders in collaboration with Delaware Office of State Planning Coordination and funded by the Delaware Department of Transportation This work was sponsored and funded by the Delaware Department of Transportation (DelDOT). The contents of this report reflect the views of the authors, who are responsible for the facts and accuracy of research. The contents do not necessarily reflect the official view of DelDOT. Planning for Complete Communities in Delaware: Summary Report to the City of Milford Preface Delaware, like the rest of the nation, continues to be challenged by shifts in the housing market, changing demographics, and an uneven economy. -
Observations and Analyses of Upper Ocean Responses to Tropical Storms and Hurricanes in the Vicinity of Bermuda W
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113, C08009, doi:10.1029/2007JC004358, 2008 Click Here for Full Article Observations and analyses of upper ocean responses to tropical storms and hurricanes in the vicinity of Bermuda W. J. Black1 and T. D. Dickey1 Received 6 June 2007; revised 10 December 2007; accepted 11 February 2008; published 6 August 2008. [1] A circular region within a radius of 400 km of Bermuda has been struck by 188 tropical storms or hurricanes from 1851 through 2005 and by 20 since 1995. Here we describe new direct and remote sensing observations and analyses of recent events near the Bermuda Testbed Mooring including Hurricane Fabian (2003), Tropical Storm Harvey (2005) and Hurricane Nate (2005). The most impressive upper ocean response of the recent events was produced by Hurricane Fabian when SST cooling exceeded 3.5°C, vertical mixing occurred to a depth of greater than 130 m, and upper ocean currents reached 100 cm sÀ1. Fabian also triggered an ocean color event visible in SeaWiFS satellite images. Related implications include improved estimates of the roles of tropical cyclones in driving meridional overturning circulation (MOC) and testing of hypotheses concerning warming of the tropical oceans which could cause more intense tropical storms and hurricanes. Citation: Black, W. J., and T. D. Dickey (2008), Observations and analyses of upper ocean responses to tropical storms and hurricanes in the vicinity of Bermuda, J. Geophys. Res., 113, C08009, doi:10.1029/2007JC004358. 1. Introduction infer wind speed, sea surface temperature, sea surface and wave height, and ocean color is proving to be extremely [2] Recent hurricane events such as those observed dur- valuable, but there are serious limitations such as restriction ing the 2005 Atlantic hurricane season, and in particular to surface expressions, cloudiness, and measurement reso- Hurricane Katrina, have focused the attention of both the lution [e.g., Babin et al., 2004; Scharroo et al., 2005; Son et scientific community and society in general on the connec- al., 2006]. -
Wetlands of Delaware
SE M3ER 985 U.s. - artm nt of h - n erior S ate of D lawa FiSh and Wildlife Service Department of Natural Resourc and Enviro mental Con ra I WETLANDS OF DELAWARE by Ralph W. Tiner, Jr. Regional Wetland Coordinator Habitat Resources U.S. Fish and Wildlife Service Region 5 Newton Corner, MA 02158 SEPTEMBER 1985 Project Officer David L. Hardin Department of Natural Resources and Environmental Control Wetlands Section State of Delaware 89 Kings Highway Dover, DE 19903 Cooperative Publication U.S. Fish and Wildlife Service Delaware Department of Natural Region 5 Resources and Environmental Habitat Resources Control One Gateway Center Division of Environmental Control Newton Corner, MA 02158 89 Kings Highway Dover, DE 19903 This report should be cited as follows: Tiner, R.W., Jr. 1985. Wetlands of Delaware. U.S. Fish and Wildlife Service, National Wetlands Inventory, Newton Corner, MA and Delaware Department of Natural Resources and Environmental Control, Wetlands Section, Dover, DE. Cooperative Publication. 77 pp. Acknowledgements Many individuals have contributed to the successful completion of the wetlands inventory in Delaware and to the preparation of this report. The Delaware Department of Natural Resources and Environmental Control, Wetlands Section contributed funds for wetland mapping and database construction and printed this report. David Hardin served as project officer for this work and offered invaluable assistance throughout the project, especially in coor dinating technical review of the draft report and during field investigations. The U.S. Army Corps of Engineers, Philadelphia District also provided funds for map production. William Zinni and Anthony Davis performed wetland photo interpretation and quality control of draft maps, and reviewed portions of this report. -
Lang Impoundment, 2017
Historical Documentation and National Register of Historic Places Evaluation Lang Impoundment Dike Restoration and Rehabilitation Project Port Penn, New Castle County, Delaware prepared for Delaware Department of Natural Resources and Environmental Control 152 S. State Street Dover, Delaware 19901 Prepared by Wade P. Catts, RPA Commonwealth Heritage Group, Inc. 535 N. Church Street West Chester, Pennsylvania 19380 FINAL January 2017 LANG IMPOUNDMENT HISTORICAL DOCUMENTATION AND NATIONAL REGISTER EVALUATION ABSTRACT The Lang Impoundment project area contains an earthen and stone embankment with a steel and concrete sluice. The configuration of this human-built landscape element dates to circa 1920. The impoundment area has a long history of diking and embanking. It was originally called Doctors Swamp in the late seventeenth century, and by 1787 was the common property of the Little St. Georges Marsh Company, an entity that was still extant in 1917. An earlier dike configuration, dating to at least the late 1840s, shows a different shape to the configuration present at the Lang Impoundment today, indicating that considerable rebuilding and reconfiguration have taken place over time. Later work on the dike has included new sluice wing walls and gates, the addition of gravel and soil to the embankment, and the addition of stone riprap to the exterior, riverside of the dike. While the Lang Impoundment has sufficient age and retains some of the aspects or qualities of integrity that would make it eligible for listing to the National Register of Historic Places, Commonwealth does not recommend the resource as National Register eligible. It is not an outstanding example of a dike from the early twentieth century since many of the dikes along the Delaware River were rebuilt and replaced at that time.