Kermadec Petrel in Pennsylvania
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Behavior and Attendance Patterns of the Fork-Tailed Storm-Petrel
BEHAVIOR AND ATTENDANCE PATTERNS OF THE FORK-TAILED STORM-PETREL THEODORE R. SIMONS Wildlife Science Group, Collegeof Forest Resources, University of Washington, Seattle, Washington 98195 USA ABSTRACT.--Behavior and attendance patterns of breeding Fork-tailed Storm-Petrels (Ocea- nodromafurcata) were monitored over two nesting seasonson the Barren Islands, Alaska. The asynchrony of egg laying and hatching shown by these birds apparently reflects the influence of severalfactors, including snow conditionson the breedinggrounds, egg neglectduring incubation, and food availability. Communication between breeding birds was characterized by auditory and tactile signals.Two distinct vocalizationswere identified, one of which appearsto be a sex-specific call given by males during pair formation. Generally, both adults were present in the burrow on the night of egg laying, and the male took the first incubation shift. Incubation shiftsranged from 1 to 5 days, with 2- and 3-day shifts being the most common. Growth parameters of the chicks, reproductive success, and breeding chronology varied considerably between years; this pre- sumably relates to a difference in conditions affecting the availability of food. Adults apparently responded to changes in food availability during incubation by altering their attendance patterns. When conditionswere good, incubation shifts were shorter, egg neglectwas reduced, and chicks were brooded longer and were fed more frequently. Adults assistedthe chick in emerging from the shell. Chicks became active late in the nestling stage and began to venture from the burrow severaldays prior to fledging. Adults continuedto visit the chick during that time but may have reducedthe amountof fooddelivered. Chicks exhibiteda distinctprefledging weight loss.Received 18 September1979, accepted26 July 1980. -
HISTORICAL HURRICANES in SOUTH CAROLINA September 10-22, 1989 N Average, South Carolina Experiences a Land-Falling Hurricane Hurricane Hugo Every Seven Years
HISTORICAL HURRICANES IN SOUTH CAROLINA September 10-22, 1989 n average, South Carolina experiences a land-falling hurricane Hurricane Hugo every seven years. Between 1900 and 2000, 14 hurricanes Time of Landfall: 12 a.m., 9/22/1989 Saffir/Simpson Scale Category: Category 4 Omade landfall along the coast of South Carolina including three Location of Landfall: Sullivans Island, SC Estimated U.S. Damage Costs: $7 billion major hurricanes: Hurricane Hugo (1989), Hurricane Gracie (1959), Maximum Winds at Landfall: 140 mph Estimated U.S. Deaths: 49 and Hurricane Hazel (1954). These South Carolina hurricanes made the Minimum Pressure at Landfall: 27.58” (934 mb) Estimated Storm Surge: 18-20 feet Top 40 Most Intense Hurricanes in a study by scientists at the National Hurricane Center. Rankings were based on minimum central pressures SUMMARY at the time of landfall. Hugo ranked #11 on the list, followed by Hazel Hugo originated off the coast of western Africa near the Cape Verde Islands as a tropical disturbance on September 9th and quickly gained strength to a tropical storm on the 11th and hurricane on the 13th. Hugo reached maximum intensity at Category 5 on the 15th with winds estimated at 160 mph and a minimum pressure of 918 mb east of the Leeward Islands. at #13, and Gracie at #33. Although major hurricanes are rare for the The hurricane passed directly over the islands of Guadaloupe, St. Croix, and Puerto Rico over the next few days before heading northwestward toward the South Carolina coast. By 6 a.m. coastal sections of South Carolina, averaging one every 25 years, the EDT on September 21, 1989, hurricane warnings were issued for coastal South Carolina and more than 250,000 people evacuated the coast. -
Acoustic Attraction of Grey-Faced Petrels (Pterodroma Macroptera Gouldi) and Fluttering Shearwaters (Puffinus Gavia) to Young Nick’S Head, New Zealand
166 Notornis, 2010, Vol. 57: 166-168 0029-4470 © The Ornithological Society of New Zealand, Inc. SHORT NOTE Acoustic attraction of grey-faced petrels (Pterodroma macroptera gouldi) and fluttering shearwaters (Puffinus gavia) to Young Nick’s Head, New Zealand STEVE L. SAWYER* Ecoworks NZ Ltd, 369 Wharerata Road, RD1, Gisborne 4071, New Zealand SALLY R. FOGLE Ecoworks NZ Ltd, 369 Wharerata Road, RD1, Gisborne 4071, New Zealand Burrow-nesting and surface-nesting petrels colonies at sites following extirpation or at novel (Families Procellariidae, Hydrobatidae and nesting habitats, as the attraction of prospecting Oceanitidae) in New Zealand have been severely non-breeders to a novel site is unlikely and the affected by human colonisation, especially through probabilities of recolonisation further decrease the introduction of new predators (Taylor 2000). as the remaining populations diminish (Gummer Of the 41 extant species of petrel, shearwater 2003). and storm petrels in New Zealand, 35 species are Both active (translocation) and passive (social categorised as ‘threatened’ or ‘at risk’ with 3 species attraction) methods have been used in attempts to listed as nationally critical (Miskelly et al. 2008). establish or restore petrel colonies (e.g. Miskelly In conjunction with habitat protection, habitat & Taylor 2004; Podolsky & Kress 1992). Methods enhancement and predator control, the restoration for the translocation of petrel chicks to new colony of historic colonies or the attraction of petrels to sites are now fairly well established, with fledging new sites is recognised as important for achieving rates of 100% achievable, however, the return of conservation and species recovery objectives translocated chicks to release sites is still awaiting (Aikman et al. -
Understanding Our Coastal Environment
Preface The South Carolina Beachfront Management Act In the Beginning The Coastal Zone Management Act of 1977 was enacted to protect our coastal resources from unwise development. This legislation served the beaches well during its first decade, but as South Carolina became a more popular tourist destination, it became apparent that the portion of the Act that dealt with beaches was inadequate. As development crept seaward, seawalls and rock revetments proliferated, damaging the public’s beach. In many areas there was no beach left at high tide. In some areas, there was no beach at low tide, either. In 1988 and again in 1990, South Carolina’s legislators took action and amended and strengthened the Coastal Zone Management Act. The resulting Beachfront Management Act protects South Carolina’s sandy shores by increasing the state’s jurisdiction and encouraging development to move landward. South Carolina’s Beachfront Jurisdiction To find the boundaries of this jurisdiction, staff from the Office of Ocean and Coastal Resource Management must first locate the baseline, which is the crest of the primary oceanfront sand dune. Where there are no dunes, the agency uses scientific methods to determine where the natural dune would lie if natural or man-made occurrences had not interfered with nature’s dune building process. The setback line is the most landward boundary and is measured from the baseline. To find the depth of the setback line, the beach’s average annual erosion rate for the past forty years is calculated and multiplied by forty. For example, if the erosion rate is one foot per year, the results will be a setback line that stretches forty feet from the baseline. -
Geographic Variation in Leach's Storm-Petrel
GEOGRAPHIC VARIATION IN LEACH'S STORM-PETREL DAVID G. AINLEY Point Reyes Bird Observatory, 4990 State Route 1, Stinson Beach, California 94970 USA ABSTRACT.-•A total of 678 specimens of Leach's Storm-Petrels (Oceanodroma leucorhoa) from known nestinglocalities was examined, and 514 were measured. Rump color, classifiedon a scale of 1-11 by comparison with a seriesof reference specimens,varied geographicallybut was found to be a poor character on which to base taxonomic definitions. Significant differences in five size charactersindicated that the presentlyaccepted, but rather confusing,taxonomy should be altered: (1) O. l. beali, O. l. willetti, and O. l. chapmani should be merged into O. l. leucorhoa;(2) O. l. socorroensisshould refer only to the summer breeding population on Guadalupe Island; and (3) the winter breeding Guadalupe population should be recognizedas a "new" subspecies,based on physiological,morphological, and vocal characters,with the proposedname O. l. cheimomnestes. The clinal and continuoussize variation in this speciesis related to oceanographicclimate, length of migration, mobility during the nesting season,and distancesbetween nesting islands. Why oceanitidsfrequenting nearshore waters during nestingare darker rumped than thoseoffshore remains an unanswered question, as does the more basic question of why rump color varies geographicallyin this species.Received 15 November 1979, accepted5 July 1980. DURING field studies of Leach's Storm-Petrels (Oceanodroma leucorhoa) nesting on Southeast Farallon Island, California in 1972 and 1973 (see Ainley et al. 1974, Ainley et al. 1976), several birds were captured that had dark or almost completely dark rumps. The subspecificidentity of the Farallon population, which at that time was O. -
The Rise and Fall of Bulwer's Petrel
A paper from the British Ornithologists’ Union Records Committee The rise and fall of Bulwer’s Petrel Andrew H. J. Harrop ABSTRACT This short paper examines two recent reviews of records of Bulwer’s Petrel Bulweria bulwerii in Britain by BOURC. Four records were assessed, including three specimen records from the nineteenth and early twentieth centuries and a modern-day sighting from Cumbria. None was found acceptable, and the reasons are discussed here. ulwer’s Petrel Bulweria bulwerii was By the time The Handbook was published, seven named after Rev. James Bulwer, an records were listed for Britain, all in England Bamateur Norfolk collector, naturalist and (Witherby et al. 1940), and these were repeated conchologist, who first collected it in Madeira, in Bannerman’s The Birds of the British Isles probably in 1825 during a short expedition to (1959). Of these seven, four (all from Sussex, Deserta Grande (Mearns & Mearns 1988). It between 1904 and 1914) were subsequently was first described by Sir William Jardine and rejected as ‘Hastings Rarities’ (Nicholson & Fer- Prideaux John Selby, in Illustrations of guson-Lees 1962; see plate 380) and a fifth, said Ornithology in 1828 (Jardine & Selby 1828). The to have been picked up at Beachy Head, Sussex, species has had a turbulent history as a British by an unnamed person on 3rd February 1903, bird. This paper provides a brief summary of escaped this fate only because it occurred records in the British ornithological literature, outside the area used to define ‘Hastings’ presents the results of two BOURC reviews, and records (Bourne 1967). -
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. -
Management Plan for Antarctic Specially Protected Area No
Measure 2 (2005) Annex E Management Plan for Antarctic Specially Protected Area No. 120 POINTE-GÉOLOGIE ARCHIPELAGO, TERRE ADÉLIE Jean Rostand, Le Mauguen (former Alexis Carrel), Lamarck and Claude Bernard Islands, The Good Doctor’s Nunatak and breeding site of Emperor Penguins 1. Description of Values to be Protected In 1995, four islands, a nunatak and a breeding ground for emperor penguins were classified as an Antarctic Specially Protected Area (Measure 3 (1995), XIX ATCM, Seoul) because they were a representative example of terrestrial Antarctic ecosystems from a biological, geological and aesthetics perspective. A species of marine mammal, the Weddell seal (Leptonychotes weddelli) and various species of birds breed in the area: emperor penguin (Aptenodytes forsteri); Antarctic skua (Catharacta maccormicki); Adélie penguins (Pygoscelis adeliae); Wilson’s petrel (Oceanites oceanicus); giant petrel (Macronectes giganteus); snow petrel (Pagodrama nivea), cape petrel (Daption capense). Well-marked hills display asymmetrical transverse profiles with gently dipping northern slopes compared to the steeper southern ones. The terrain is affected by numerous cracks and fractures leading to very rough surfaces. The basement rocks consist mainly of sillimanite, cordierite and garnet-rich gneisses which are intruded by abundant dikes of pink anatexites. The lowest parts of the islands are covered by morainic boulders with a heterogenous granulometry (from a few cm to more than a m across). Long-term research and monitoring programs of birds and marine mammals have been going on for a long time already (since 1952 or 1964 according to the species). A database implemented in 1981 is directed by the Centre d'Etudes Biologiques de Chize (CEBC-CNRS). -
Dear Investors As You May Might Have Heard from Different Media Outlets
Dear investors As you may might have heard from different media outlets, the east coast of the U.S. is facing a potential threat of landfall of the major hurricane named Florence in the coming days. The storm is currently about 385 miles/620 KM southwest of BERMUDA and about 625 miles/1005 KM southeast of Cape Fear North CAROLINA, moving to the direction of North and South Carolina. The intensity is currently Cat 4, with maximum sustained wind speed very close to 140 mph. As the storm moves to the coast, the wind will intensify to Cat 5 and maximum sustained winds can reach 155 mph. Timing is more difficult to predict now as many meteorologists suggest Florence will slow on approach to the coast, with a possible stalling that could exacerbate the impacts for the area it nears the shore. Catastrophe risk modeller RMS said, “Florence will be the strongest hurricane to make landfall over North Carolina since Hazel in 1954 – this would be a major event for the insurance industry. As with all hurricanes of this intensity, Florence poses significant impacts due to damaging hurricane-force winds and coastal storm surge, but inland flooding is becoming an increasing threat. Forecasts include the possibility of Florence slowing down after landfall and causing as much as 20 inches of rain in the Carolinas. While very significant, this remains much lower than the amount of rainfall observed last year during Hurricane Harvey.” Wind Florence is expected to make landfall as a hurricane between Cat 3 and Cat 4. The wind speed can reach 110-130 mph and central pressure is estimated 962mb. -
The Hurricane-Tornado
July 1965 John S. Smith 453 THEHURRICANE-TORNADO JOHN S. SMITH Weather Bureau Forecast Center, Chicago, 111. ABSTRACT Climatological data in recent years have become sufficient for the further study of tornadoes which occur in hurricane systems. Several characteristics of the hurricane tornado are determined from data for an 8-yr. period by plotting the center positions of each hurricane and its associated tornadoes. The data show: (1) a comparison betweenhurricane and non-hurricane tornadoes; (2) a “Significant Sector” fortornado-genesis; (3) a “Preferred Quadrant” of the hurricane for tornado-genesis; (4) the mostfavorable time of dayfor tornado occurrence; (5) tornado frequencies with,respect to various speeds and distances of the hurricane on and off shore; (6) a tenative hurricane model. 1. INTRODUCTION the “Preferred Quadrant.” Other significant patterns are established from the relationship of the tornado to the Although considerable research has been done on the hurricane. forecasting problemspresented byboth tornadoes and hurricanes, relatively little investigation has been made 2. GENERALCLIMATOLOGY intothe forecasting problems of tornadoesassociated with hurricanes. In this study of the hurricane-tornado Of 15 hurricanes that entered the United States from problem,a climatological analysishas been made by the Gulf of Mexico andthrough the Atlantic Coastal plottingthe center position of eachhurricane and its States, 11 produced tornadoes. Atotal of 98 tornadoes associated tornadoes. was produced during the period from hurricane Connie in August 1955, to hurricane Carla in September 1961. Of Recognition of hurricane tornadoes prior to 1955 was the hurricanes producing tornadoes, the average number apparently limited-unless therehas beensuddena of tornadoes per hurricane is 9, although hurricanes Audrey rash of hurricane-tornadoesin recent years, for since and Carla spawned more than 20 tornadoes each. -
Albatross and Giant-Petrel Distribution Across the World's Tuna And
The Third Joint Tuna RFMOs meeting; La Jolla, July 11-15, 2011 s e l l e c s a L B - s e s s o r t b l a g n i y l F ; F T A / n e r o G M - e n li g n o l n o s s o r t a b l a Albatross and giant-petrel distribution across the world’s tuna and swordfish fisheries R. Alderman1, D. Anderson2, J. Arata3, P. Catry4, R. Cuthbert5, L. Deppe6, G. Elliot7, R. Gales1, J. Gonzales Solis9, J.P. Granadeiro10, M. Hester11, N. Huin12, D. Hyrenbach13, K. Layton14, D. Nicholls15, K. Ozak16, S. Peterson17, R.A. Phillips18, F. Quintana19, G. R. Balogh20, C. Robertson21, G. Robertson14, P. Sagar22, F. Sato16, S. Shaffer23, C. Small5, J. Stahl24, R. Suryan25, P. Taylor26, D. Thompson22, K. Walker7, R. Wanless27, S. Waugh24, H. Weimerskirch28 Summary More than 90% of albatross and giant Albatrosses are vulnerable to bycatch in tuna and swordfish longline fisheries. petrel global distribution overlaps Remote tracking data provide a key tool to identifying priority areas for with the areas managed by the tuna seabird bycatch mitigation. This paper presents an updated analysis of the global distribution of albatrosses and giant-petrels using data from the Global commissions Procellariiform Tracking Database. Overall, 91% of global albatross and giant- petrel distribution during the breeding season and 92% of global albatross and giant-petrel distribution during the non-breeding season, overlaps with the areas Results emphasise the importance of managed by the tuna commissions. -
Herald Petrel New to the West Indies
EXTRALIMITAL RECORD Herald Petrel new to the West Indies Michael Gochfeld,Joanna Burger, Jorge Saliva, and Deborah Gochfeld (Pterodroma)are bestrepresented SinA southGROUP temperate THEGADFLY and subantarc-PETRELS tic waterswith a few speciesbreeding on tropicalislands in the Central Pacific, Atlantic, and Indian Oceans.In the West Indies,the only member of this genusis the Black-cappedPetrel (P hasitata), which breeds in the Greater Antilles and perhaps still in the Lesser Antilles. A dose relative,the endangeredBermuda (P..cahow) breeds in Bermuda. On July 12, 1986, while studyingthe breeding Laughing Gulls (Larus atri- cilia), Royal Terns,and SandwichTerns (Sterna maxima and S. sandvicensis)on Cayo Lobito, in the Culebra National Wildlife Refuge, about 40 kilometers eastof Fajardo,Puerto Rico, we flushed an all-dark petrel from a scrapeamong the nestingterns. As soon as the bird wheeled around we realized that it was a petrel, and not the familiar Sooty Shearwater(Puj•nus griseus),a species Figure 1. Dark-phasePterodroma landing among Laughing Gulls on Cayo Lobito. Culebra, which would itselfbe extremelyunusual PuertoRico. Note the ashygray undersurface of theprimary.feathers, ending in longnarrow at Culebra. Compared to a shearwater, "digital" extensionsthat are the pale areas of the inner websof theprimaries. The greater the petrelappeared to havea largerhead underwingcoverts are pale with a narrowdark tip that showsas thefaint wavybar at the base of theprimaries. The Iongishtail and shortishbill are apparent. and a longerand slightlywedge-shaped tail. It did not showthe conspicuouspale wing linings of the Sooty Shearwater (Fig. 1). The bird circled rapidly, first low over the water and then wheeling high overthe rocky islet,before return- ing to its scrapeamong the gulls and terns.