Summer Is Here! Are You Weather Ready?
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Brooklyn College and Graduate School of the City University of NY, Brooklyn, NY 11210 and Northeastern Science Foundation Affiliated with Brooklyn College, CUNY, P.O
FLYSCH AND MOLASSE OF THE CLASSICAL TACONIC AND ACADIAN OROGENIES: MODELS FOR SUBSURFACE RESERVOIR SETTINGS GERALD M. FRIEDMAN Brooklyn College and Graduate School of the City University of NY, Brooklyn, NY 11210 and Northeastern Science Foundation affiliated with Brooklyn College, CUNY, P.O. Box 746, Troy, NY 12181 ABSTRACT This field trip will examine classical sections of the Appalachians including Cambro-Ordovician basin-margin and basin-slope facies (flysch) of the Taconics and braided and meandering stteam deposits (molasse) of the Catskills. The deep water settings are part of the Taconic sequence. These rocks include massive sandstones of excellent reservoir quality that serve as models for oil and gas exploration. With their feet, participants may straddle the classical Logan's (or Emmon 's) line thrust plane. The stream deposits are :Middle to Upper Devonian rocks of the Catskill Mountains which resulted from the Acadian Orogeny, where the world's oldest and largest freshwater clams can be found in the world's oldest back-swamp fluvial facies. These fluvial deposits make excellent models for comparable subsurface reservoir settings. INTRODUCTION This trip will be in two parts: (1) a field study of deep-water facies (flysch) of the Taconics, and (2) a field study of braided- and meandering-stream deposits (molasse) of the Catskills. The rocks of the Taconics have been debated for more than 150 years and need to be explained in detail before the field stops make sense to the uninitiated. Therefore several pages of background on these deposits precede the itinera.ry. The Catskills, however, do not need this kind of orientation, hence after the Taconics (flysch) itinerary, the field stops for the Catskills follow immediately without an insertion of background informa tion. -
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. -
CONGRESSIONAL RECORD— Extensions of Remarks E1745 HON
September 24, 2010 CONGRESSIONAL RECORD — Extensions of Remarks E1745 HONORING SUE PALKA It is important to recognize ways in which September 30, at the peak of hurricane sea- average investors of all ages and income lev- son. Madam Speaker, distinguished col- HON. CHRIS VAN HOLLEN els can access the same benefits as large real leagues, I ask you today to join me in passing OF MARYLAND estate investors. I stand with my colleague in this bill. However, we must dedicate ourselves IN THE HOUSE OF REPRESENTATIVES commending the 50th anniversary of Real Es- to finding a permanent solution for those tate Investment Trusts, and 50 years of pro- Americans adversely affected by flooding. The Friday, September 24, 2010 viding a broad range of investors an oppor- people of my district need a long-term exten- Mr. VAN HOLLEN. Madam Speaker, on tunity to achieve the investment goals of diver- sion of the flood insurance program—and they Monday, September 27, 2010, one of my con- sification, strong and reliable dividends, liquid- need to know that the flood insurance program stituents will be celebrating 25 years of out- ity, solid performance, and transparency. will always be there for them. While we are standing service to the Washington, DC met- f working to mitigate the damage caused by ropolitan region. floods, this program remains essential for NATIONAL FLOOD INSURANCE WTTG Fox 5 News weather forecaster Sue those tragic times when nature takes over. PROGRAM REEXTENSION ACT OF Palka has been bringing Washingtonians their With homes in my district and in every flood- 2010 weather reports for decades. -
Wetlands of Saratoga County New York
Acknowledgments THIS BOOKLET I S THE PRODUCT Of THE work of many individuals. Although it is based on the U.S. Fish and Wildlife Service's National Wetlands Inventory (NWI), tlus booklet would not have been produced without the support and cooperation of the U.S. Environmental Protection Agency (EPA). Patrick Pergola served as project coordinator for the wetlands inventory and Dan Montella was project coordinator for the preparation of this booklet. Ralph Tiner coordi nated the effort for the U.S. Fish and Wildlife Service (FWS). Data compiled from the NWI serve as the foun dation for much of this report. Information on the wetland status for this area is the result of hard work by photointerpreters, mainly Irene Huber (University of Massachusetts) with assistance from D avid Foulis and Todd Nuerminger. Glenn Smith (FWS) provided quality control of the interpreted aerial photographs and draft maps and collected field data on wetland communities. Tim Post (N.Y. State D epartment of Environmental Conservation), John Swords (FWS), James Schaberl and Chris Martin (National Park Ser vice) assisted in the field and the review of draft maps. Among other FWS staff contributing to this effort were Kurt Snider, Greg Pipkin, Kevin Bon, Becky Stanley, and Matt Starr. The booklet was reviewed by several people including Kathleen Drake (EPA), G eorge H odgson (Saratoga County Environmental Management Council), John Hamilton (Soil and W ater Conserva tion District), Dan Spada (Adirondack Park Agency), Pat Riexinger (N.Y. State Department of Environ mental Conservation), Susan Essig (FWS), and Jen nifer Brady-Connor (Association of State Wetland Nlanagers). -
Richmond, VA Hurricanes
Hurricanes Influencing the Richmond Area Why should residents of the Middle Atlantic states be concerned about hurricanes during the coming hurricane season, which officially begins on June 1 and ends November 30? After all, the big ones don't seem to affect the region anymore. Consider the following: The last Category 2 hurricane to make landfall along the U.S. East Coast, north of Florida, was Isabel in 2003. The last Category 3 was Fran in 1996, and the last Category 4 was Hugo in 1989. Meanwhile, ten Category 2 or stronger storms have made landfall along the Gulf Coast between 2004 and 2008. Hurricane history suggests that the Mid-Atlantic's seeming immunity will change as soon as 2009. Hurricane Alley shifts. Past active hurricane cycles, typically lasting 25 to 30 years, have brought many destructive storms to the region, particularly to shore areas. Never before have so many people and so much property been at risk. Extensive coastal development and a rising sea make for increased vulnerability. A storm like the Great Atlantic Hurricane of 1944, a powerful Category 3, would savage shorelines from North Carolina to New England. History suggests that such an event is due. Hurricane Hazel in 1954 came ashore in North Carolina as a Category 4 to directly slam the Mid-Atlantic region. It swirled hurricane-force winds along an interior track of 700 miles, through the Northeast and into Canada. More than 100 people died. Hazel-type wind events occur about every 50 years. Areas north of Florida are particularly susceptible to wind damage. -
Freshwater Fishing: a Driver for Ecotourism
New York FRESHWATER April 2019 FISHINGDigest Fishing: A Sport For Everyone NY Fishing 101 page 10 A Female's Guide to Fishing page 30 A summary of 2019–2020 regulations and useful information for New York anglers www.dec.ny.gov Message from the Governor Freshwater Fishing: A Driver for Ecotourism New York State is committed to increasing and supporting a wide array of ecotourism initiatives, including freshwater fishing. Our approach is simple—we are strengthening our commitment to protect New York State’s vast natural resources while seeking compelling ways for people to enjoy the great outdoors in a socially and environmentally responsible manner. The result is sustainable economic activity based on a sincere appreciation of our state’s natural resources and the values they provide. We invite New Yorkers and visitors alike to enjoy our high-quality water resources. New York is blessed with fisheries resources across the state. Every day, we manage and protect these fisheries with an eye to the future. To date, New York has made substantial investments in our fishing access sites to ensure that boaters and anglers have safe and well-maintained parking areas, access points, and boat launch sites. In addition, we are currently investing an additional $3.2 million in waterway access in 2019, including: • New or renovated boat launch sites on Cayuga, Oneida, and Otisco lakes • Upgrades to existing launch sites on Cranberry Lake, Delaware River, Lake Placid, Lake Champlain, Lake Ontario, Chautauqua Lake and Fourth Lake. New York continues to improve and modernize our fish hatcheries. As Governor, I have committed $17 million to hatchery improvements. -
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. -
The Atlantic Hurricane Season Summary – 2014
THE ATLANTIC HURRICANE SEASON SUMMARY – 2014 SPECIAL FOCUS ON ANTIGUA AND BARBUDA (PRELIMINARY) Dale C. S. Destin (follow @anumetservice) Antigua and Barbuda Meteorological Service Climate Section December 4, 2014 Satellite Image: Hurricane Gonzalo – Oct 13, 12:45 pm 2014 1 The Atlantic Hurricane Season Summary – 2014 Special Focus on Antigua and Barbuda Dale C. S. Destin (follow @anumetservice) Antigua and Barbuda Meteorological Service Climate Section December 3, 2014 The Season in Brief The 2014 Atlantic hurricane season was relatively quiet generally but relatively average for Antigua. It produced eight (8) named storms. Of the eight (8) storms, six (6) became hurricanes and two reached major hurricane status - category three (3) or higher on the Saffir-Simpson Hurricane Wind Scale. The strongest tropical cyclone for the season was Major Hurricane Gonzalo with peak winds of 145 mph and minimum pressure of 940 mb (see figure 2). Gonzalo impacted Antigua and Barbuda and most of the other northeast Caribbean islands causing loss of lives and 100s of millions of dollars in damage. Relative to Antigua and Barbuda Relative to Antigua and Barbuda, the rest of the Leeward Islands and the British Virgin Islands, two (2) tropical cyclones entered or formed in our defined monitored area (10N 40W – 10N 55W – 15N 70W – 20N 70W – 20N 55W – 15N 40W – 10N 40W) - Bertha and Gonzalo. Gonzalo impacted the northeast Caribbean with hurricane force winds, passing directly over Antigua, St. Martin and Anguilla. This is the first time since Jose in 1999, Antigua has had sustained hurricane force winds, ending our 14 year hurricane drought. In terms of number of named storms, it was not a quiet season for Antigua but rather an average one; however, with respect to hurricanes, we were a year over due since one affects us every three years on average. -
Floods Caused by Tropical Systems: James River at Cartersville, VA
Floods Caused by Tropical Systems: James River at Cartersville, VA Latitude: 37.671 Period of Record: 1869-Present Longitude: -78.086 Flood Stage: 20 Last Flood: 2/25/2019 Number of Floods: 88 Date of Flood Crest (ft) Streamflow (cfs) Weather Summary 9/6/1935 27.8 134,000 The "Labor Day Hurricane" dumped heavy rain along the East Coast. A total of 16.62 inches of rain was reported in Easton and 12.1 inches of rain was reported in Salisbury, MD. 8/19/1955 24.48 104,000 Hurricane Diane made landfall 5 days after Hurricane Connie. Hurricane Diane produced several inches of rain with locally heavier amounts of 10 to 20 inches. 10/18/1932 21.54 75,400 Remnants of the eighth tropical storm of the season produced 2.00 inches of rainfall across most of the Mid- Atlantic region. 6/22/1972 37.87 362,000 Hurricane Agnes made landfall again over southeastern New York on June 22 and moved westward into Pennsylvania. Rainfall totals from June 20-25 range from 2-3 inches in the Upper Potomac to 18 inches near Shamokin, Pennsylvania. 8/12/1928 22.06 78,600 The remnants of an unnamed hurricane produced rainfall that caused flooding in the James and Appomattox basins. 8/18/1928 23.8 97,200 The weather summary is unavailable at this time. 10/16/1942 27.14 135,000 The remnants of the eighth tropical storm of the year produced torrential rains and caused the worst river flooding in the history of Virginia. 9/20/2003 22.89 89,825 Hurricane Isabel combined with another system and produced more than 3 inches of rain in VA with locally heavier amounts of 10 inches. -
Hurricanes of 1955 Gordon E
DECEMBEB1955 MONTHLY WEATHER REVIEW 315 HURRICANES OF 1955 GORDON E. DUNN, WALTER R. DAVIS, AND PAUL L. MOORE Weather Bureau Offrce, Miami, Fla. 1. GENERAL SUMMARY grouping i,n theirpaths. Thethree hurricanes entering the United States all crossed the North Carolina coast There were 13 tropical storms in 1955, (fig. 9), of which within a 6-week period and three more crossed the Mexican 10 attained hurricane force, a number known to have been coast within 150 miles of Tampico within a period of 25 exceeded only once before when 11 hurricanes were re- days. corded in 1950. This compares with a normal of about The hurricane season of 1955 was the most disastrous 9.2 tropical storms and 5 of hurricane intensity. In con- in history and for the second consecutive year broke all trast to 1954, no hurricanes crossed the coastline north of previous records for damage. Hurricane Diane was Cape Hatteras andno hurricane winds were reported north undoubtedly the greatest natural catastrophe in the his- of that point. No tropical storm of hurricane intensity tory of the United Statesand earned the unenviable affected any portion of the United States coastline along distinction of “the first billion dollar hurricane”. While the Gulf of Mexico or in Florida for the second consecutive the WeatherBureau has conservatively estimated the year. Only one hurricane has affected Florida since 1950 direct damage from Diane at between $700,000,000 and and it was of little consequence. However, similar hurri- $800,000,000, indirect losses of wages, business earnings, cane-free periods have occurred before. -
Invasive Species of the Adirondack Region
Invasive Species of the Adirondack Region Meghan Johnstone Aquatic Invasive Species Project Coordinator Adirondack Park Invasive Plant Program [email protected] (518)576-2082 x119 www.adkinvasives.com Presentation Outline • What are invasive species? • What is the Adirondack Park Invasive Plant Program? • What are the priority aquatic invasive species in the Adirondacks? • Black River Watershed • Which spread prevention tips should you use or recommend? Lythrum salicaria What’s the difference? Native Species • Species indigenous to a region at the time of European settlement Non-native Species (Exotic, Introduced, Alien) • Accidental or purposeful introduction of a species outside of its historic range Invasive Species (Noxious) • Non-native species that rapidly reproduces and displaces native species causing harm Nuisance Species (Weed) • Species that interferes with human activities Our Focus Species that… • Are not native to the ecosystem under consideration. • Can reproduce and support self-sustaining populations. • Can “jump” spatial gaps. • Cause ecological, economic, or societal harms. Benefits of Native Plants • Provide food • Stabilize sediments • Provide shelter and • Reduce turbidity spawning habitat • Produce oxygen • Transport nutrients • Protect shoreline • Support diversity The Horror Stories: What Can Happen If Invasives Are Allowed To Spread Eurasian watermilfoil, Eagle Lake Water chestnut, Lake Champlain Common reed grass, Long Lake Japanese knotweed, Saranac Lake Swallow-wort spp., St. Lawrence Why are some non-natives