AUTUMN MIGRATION of the BLACKPOLL WARBLER: EVIDENCE for LONG FLIGHT PROVIDED by REGIONAL SURVEY* by IA• C
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Review and Herald for 1955
GENERAL CHURCH PAPER OF THE SEVENTH-DAY ADVENTISTS flurticanes tixt 'Citial Waves im Mexico By E. C. CHRISTIE Treasurer, Mexican Union TIASTOR LEON AND CAR- TUMAL BEING EVACUATED. ing the "flooding of Tampico and r REON TRAPPED BY HUR- LEON AND CARREON SAFE. neighboring territory," "causing mil- RICANE IN CHETUMAL. MANY CHURCH MEMBERS lions of dollars' worth of damage." MANY PERSONS KILLED AND DEAD. CHURCH BUILDING Heavy rains in the mountains were BURIED. ALL ATTEMPTS TO SWEPT AWAY BY TIDAL WAVES." forcing rivers out of their regular LOCATE THESE TWO WORKERS It is a most unpleasant task to place channels, and farms and villages HAVE FAILED." before our people information along the valleys were being invaded This was the message delivered by gleaned from the recent disasters that by the muddy torrents. the telegram boy on Sabbath morning, have been punishing Mexico from The city of Tampico, along with October 1, 1955. Brother LeOn is the one end to the other; even a vicious smaller towns here and there, was president of our Southeast Mission fighter does not hit a man when he's completely isolated from other parts and Brother Carre6n works with him down and out, but the hurricanes of the republic. Highways, railways, as treasurer. They had gone to Chetu- Gladys, Hilda, and Janet have been no and airports were under water. Food, mal to hold a baptismal service on this respecters of persons or cities. They water, and other items ordinarily in- very Sabbath, but the plans were not hit the hardest before the people were dispensable for existence were not carried through this time. -
Revista 224.Indd
U CARIBBEAn TROPICAL STORMS Ecological Implications for Pre-Hispanic and Contemporary Maya Subsistence on the Yucatan Peninsula Herman W. Konrad ABSTRACT The ecological stress factor of hurricanes is examined as a dimension of pre-Hispanic Maya adaptation to a tropical forest habitat in the Yucatan peninsula. Pre-Hispanic, colonial and contemporary texts as well as climatic data from the Caribbean region support the thesis that the hurricane was an integral feature of the pre-Hispanic Maya cosmology and ecological paradigm. The author argues that destruction of forests by tropical storms and subsequent succession cycles mimic not only swidden —"slash- and-burn"— agriculture, but also slower, natural succession cycles. With varying degrees of success, flora and fauna adapt to periodic, radical ecosystem disruption in the most frequently hard-hit areas. While not ignoring more widely-discussed issues surrounding the longevity and decline of pre-Hispanic Maya civilization, such as political development, settlement patterns, migration, demographic stability, warfare and trade, the author suggests that effective adaptation to the ecological effects of tropical storms helped determine the success of pre-Hispanic Herman W. Konrad. university Maya subsistence strategies. of Calgary. Email: [email protected] gary.ca NÚMERO 224 • PRIMER TRIMESTRE DE 2003 • 99 Herman W. Konrad RESuMEn Los efectos ecológicos causados por los huracanes se analizan en el contexto de la adaptación de los mayas prehispánicos a la selva de la península de Yucatán. Textos prehispánicos, coloniales y contemporáneos, así como información climática sobre el Caribe en general, apoyan la hipótesis de que el huracán era un elemento central en la cosmovisión y el paradigma ecológico prehispánico. -
Florida Hurricanes and Tropical Storms
FLORIDA HURRICANES AND TROPICAL STORMS 1871-1995: An Historical Survey Fred Doehring, Iver W. Duedall, and John M. Williams '+wcCopy~~ I~BN 0-912747-08-0 Florida SeaGrant College is supported by award of the Office of Sea Grant, NationalOceanic and Atmospheric Administration, U.S. Department of Commerce,grant number NA 36RG-0070, under provisions of the NationalSea Grant College and Programs Act of 1966. This information is published by the Sea Grant Extension Program which functionsas a coinponentof the Florida Cooperative Extension Service, John T. Woeste, Dean, in conducting Cooperative Extensionwork in Agriculture, Home Economics, and Marine Sciences,State of Florida, U.S. Departmentof Agriculture, U.S. Departmentof Commerce, and Boards of County Commissioners, cooperating.Printed and distributed in furtherance af the Actsof Congressof May 8 andJune 14, 1914.The Florida Sea Grant Collegeis an Equal Opportunity-AffirmativeAction employer authorizedto provide research, educational information and other servicesonly to individuals and institutions that function without regardto race,color, sex, age,handicap or nationalorigin. Coverphoto: Hank Brandli & Rob Downey LOANCOPY ONLY Florida Hurricanes and Tropical Storms 1871-1995: An Historical survey Fred Doehring, Iver W. Duedall, and John M. Williams Division of Marine and Environmental Systems, Florida Institute of Technology Melbourne, FL 32901 Technical Paper - 71 June 1994 $5.00 Copies may be obtained from: Florida Sea Grant College Program University of Florida Building 803 P.O. Box 110409 Gainesville, FL 32611-0409 904-392-2801 II Our friend andcolleague, Fred Doehringpictured below, died on January 5, 1993, before this manuscript was completed. Until his death, Fred had spent the last 18 months painstakingly researchingdata for this book. -
Project STORMFURY: a Scientific Chronicle 1962-1983
Project STORMFURY: H. E. Willoughby, D. P. Jorgensen1, R. A. Black, and S. L. Rosenthal A Scientific Chronicle Hurricane Research Division, AOML/NOAA 4301 Rickenbacker Causeway 1962-1983 Miami, FL 33149 Abstract of Georgia and North Florida. After seeding, observers aboard the experimental aircraft noted changes in the visual Between 1962 and 1983, research in hurricane modification centered appearance of the clouds, but they could not demonstrate on an ambitious experimental program, Project STORMFURY. any other effects on structure or intensity. The one indisput- The proposed modification technique involved artificial stimulation of convection outside the eye wall through seeding with silver iodide. able change—although apparently not the result of seeding The artificially invigorated convection, it was argued, would compete (Mook et al., 1957)—was a reversal of track toward the west, with the convection in the original eye wall, lead to reformation of which ultimately led to landfall on the coasts of Georgia and the eye wall at larger radius, and thus produce a decrease in the max- South Carolina. Claims by Langmuir (Byers, 1974) that the imum wind. track had been influenced through human intervention were Since a hurricane's destructive potential increases rapidly as its maximum wind becomes stronger, a reduction as small as 10% an embarrassment at the time and left a legacy that had an would have been worthwhile. Modification was attempted in four adverse effect upon political and legal arrangements for later hurricanes on eight different days. On four of these days, the winds hurricane modification efforts. decreased by between 10 and 30%. The lack of response on the other The years 1954 and 1955 each brought three major hurri- days was interpreted to be the result of faulty execution of the exper- iment or poorly selected subjects. -
Downloaded 09/28/21 10:59 AM UTC 1 76 MONTHLY WEATHER REVIEW Vol
March 1965 Gordon E. Dunn and Staff 175 THEHURRICANE SEASON OF 1964 GORDON E. DUNN AND STAFF* U.S. Weather Bureau Office, Miami, Fla. 1. GENERALSUMMARY spondvery well withthe composite chart for atverage Twelvetropical cyclones,six of hurricaneintensity, departures from nornml for seasons of maxinlum tropical developedover tropical Atlantic waters during 1964. cycloneincidence inthe southeastern United States as This is the largest number since 1955 and compares with developed by Ballenzweig [a]. an average of 10during the past three decades. The September was aneven more active month and cor- centers of four hurricanes penetrated the mainland of the respondence between Ballenzweig'scomposite chrt and United States, the largest number to do so since the five theobserved values was better, particularly south of in 1933. There have been only four other years with four latitude 40' W. According toGreen [3] thesubtropical or more since 1900; four in 1906, 1909, and 1926, and six High was abnornlallystrong and displacedslightly in 1916.While none of thefour renching the mainland northwardfrom normal (favorable for tropical cyclone in 1964 wits :L major hurricane at the time of landfall, formation) while the 700-mb. jet was slightlysouth of three-Cleo, Dora, and EIi1da"were severe. normal (unfavorable). The long-wave position fluctuated Florida was struck by three hurricanes in addition to back and forth from the Rockies and Great Plains east- dyinghurricane Hilda and one tropical cyclone of less ward and the tropical cyclones experienced considerable than hurricane intensity; thus ended an unequalled rela- difficulty in penetrating the westerlies. During the major tively hurricane-free period of 13 years from 1951 through hurricanemonths in 1964 the long-wavetrough failed 1963. -
SELECTION of DATA for TROPICAL CYCLONE RAINFALL STUDIES Donald Brandes Rainfall Which Occurs During the Passage of a Hurricane O
SELECTION OF DATA FOR TROPICAL CYCLONE RAINFALL STUDIES Donald Brandes tt Rainfall which occurs during the passage of a hurricane or tropical storm center several hundred miles away mayor may not be directly related to the passing tropical cyclone. Satellite remote sensing imagery may be used to de termine the areal distribution of clouds associated with the tropical cyclone • and reveal the areas where rainfall was directly attributable to such a storm. Satellite imagery, however, exists only from 1960 to the present, and is diffi cult to obtain for 1960 through 1968. No such record of the continuity of cloud coverage is available for earlier times. Without knowing if an area was covered by clouds which emanated from a tropical system, it is not possible to determine with certainty if rain which fell at a given place was the result of the passing tropical cyclone or of other local or extra-tropical causes. Previous Studies Previous studies of tropical cyclone rainfall have failed to address the problem of whether a given observation of rain actually resulted from a specific storm. Cry (1967) discussed the problem of wind reducing the effectiveness of rain collection devices but neglects the question of whether the given sample should be considered at all. Goodyear (1968) avoided raw climatological data by using the United States Army Corps of Engineers information whenever possible. For earlier times he draws his information directly from summaries of weather station records, but gives no explanation of how it is known that the rainfall is the result of tropical cyclones in either situation. -
Geology and Hurricane- Protection Strategies in the Greater New Orleans Area
Geology and Hurricane- Protection Strategies in the Greater New Orleans Area PUBLIC INFORMATION SERIES NO. 11 SUMMER 2006 Louisiana Geological Survey 3079 Energy, Coast & Environment Building Baton Rouge, Louisiana 70803 Tel: 225 578 5320 Fax: 225 578 3662 Richard P. McCulloh, Paul V. Heinrich, and Bill Good www.lgs.lsu.edu Geology and Hurricane-Protection Strategies in the Greater New Orleans Area State of Louisiana Kathleen B. Blanco, Governor Louisiana State University, Baton Rouge Sean O’Keefe, Chancellor Louisiana Geological Survey Chacko J. John, Director and State Geologist Front cover: Canal Street, New Orleans, Louisiana, September 005 by Rocky Beach. This public information document is part of a series published periodically by the Louisiana Geological Survey, whose offices are located at Louisiana State University, Room 3079 Energy, Coast & Environment Building, Baton Rouge, LA 70803-40. This information is distrib- uted free of charge. The publisher does not guarantee the accuracy or correctness of any information. Contact the LGS business office at (5) 578-530 for extra copies or for more information, or visit the web site at http://www.lgs.lsu.edu. This public document was published at a total cost of $3589.6. One thousand copies of this document were published in this printing at a cost of $493.00. This document was published by the Louisiana Geological Survey, 3079 Energy, Coast and Environment, Louisiana State University, Baton Rouge, Louisiana, 70803, to aid in public understanding of the geology of Louisiana under the authority of R.S. 30:06. This material was printed in accordance with standards for printing by state agencies established pursuant to R.S. -
Análisis De La Marea De Tormenta En Registros Mareográficos, Asociada a Huracanes En Las Costas Del Golfo De México, Periodo 1950-2010 T E S I S
UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO FACULTAD DE CIENCIAS ANÁLISIS DE LA MAREA DE TORMENTA EN REGISTROS MAREOGRÁFICOS, ASOCIADA A HURACANES EN LAS COSTAS DEL GOLFO DE MÉXICO, PERIODO 1950-2010 T E S I S QUE PARA OBTENER EL TÍTULO DE: FÍSICO P R E S E N T A : SERGIO VALENTE GUTIERREZ QUIJADA DIRECTOR DE TESIS: DR. JORGE ZAVALA HIDALGO CIUDAD UNIVERSITARIA, CDMX, 2018 UNAM – Dirección General de Bibliotecas Tesis Digitales Restricciones de uso DERECHOS RESERVADOS © PROHIBIDA SU REPRODUCCIÓN TOTAL O PARCIAL Todo el material contenido en esta tesis esta protegido por la Ley Federal del Derecho de Autor (LFDA) de los Estados Unidos Mexicanos (México). El uso de imágenes, fragmentos de videos, y demás material que sea objeto de protección de los derechos de autor, será exclusivamente para fines educativos e informativos y deberá citar la fuente donde la obtuvo mencionando el autor o autores. Cualquier uso distinto como el lucro, reproducción, edición o modificación, será perseguido y sancionado por el respectivo titular de los Derechos de Autor. JURADO M. EN C. MANUEL RENÉ DE JÉSUS GARDUÑO LÓPEZ DRA. CATALINA ELIZABETH STERN FORGACH DR. JORGE ZAVALA HIDALGO DRA. BERTHA MOLINA BRITO DRA. ANA MARÍA SOLER ARECHALDE RESUMEN En este trabajo se presenta un análisis de la marea de tormenta asociada a ciclones tropicales en las costas del Golfo de México de 1950 a 2010. Se incluyen los sitios en donde se cuenta con registros de nivel del mar obtenidos de las estaciones del Servicio Mareográfico Nacional, operado por el Instituto de Geofísica de la UNAM. Se analizaron los registros de 18 ciclones tropicales, ocho con observaciones en un sitio, cuatro en dos sitios, tres en tres sitios, uno en cuatro y dos en siete. -
The Atlantic Hurricane Season of 1968
March 1969 225 UDC 551.515.2(261.1)"1968" THE ATLANTICHURRICANE SEASON OF 1968 ARNOLD L. SUGG and PAUL J. HEBERT' National Hurricane Center, Weather Bureau, ESSA, Miami, Fla. ABSTRACT The 1968 hurricane season in the North Atlantic area, considered in its entirety, and synoptic and statistical aspects of individual storms are discussed. 1. GENERAL SUMMARY TABLE1.-Hurricane days, 1954-1968 The two hurricanes and onetropical storm inJune Year Jan. Feb. Mar. Apr. May June July Aug. Sept. Dec. Total Nov. Oct. equaled a record established in 1886.2 While there were __-_________ two other years, 1959 and 1936, with a total of three June 1954 ___.__.__.___._..... _____ ..-.-..... 1 ..". 5 8 16 ___._1 31 tropical cyclones, each is not unique as there were two I955 ___.___...4 ..". .____ _____ ..... ._.._..". 22 28 2 .." ~ _____ 56 1956___._..__. ..-....". ___._ ..... ..". ..-.- 1 9 2 ___..3 ____ ._ 15 storms and one hurricane in those years. Two hurricanes 1957__.____.._ _._._..... ..". __.__..". 3 ..... _.___19 _._._ .._.______ 22 occurring inJune are noteworthy when one considers 1958__.___..._ _.___..... ..". _____ .".. _____ .__._14 16 5 ..____.___ 35 1959 __._....._..... __.._ .-..._.___ ..". 1 2 ..___10 11 .._______. 24 there have only been 20 since 1886. This is approximately 1960___......_ ..-.._._._ .".. .____..___4 2 ____.13 ~ ____ .____ ____. 10 one every 4 yr, rather than two for any one June. In spite 1961 ___......_..... ..-.- ..". ___.._____ .... -
Attachment C3-3: Storms in the ICM Boundary Conditions
Coastal Protection and Restoration Authority 150 Terrace Avenue, Baton Rouge, LA 70802 | [email protected] | www.coastal.la.gov 2017 Coastal Master Plan Attachment C3-3: Storms in the ICM Boundary Conditions Report: Version I Date: July 2015 Prepared By: ARCADIS (Haihong Zhao, John Atkinson, and Hugh Roberts) 2017 Coastal Master Plan: Storms in the ICM Boundary Conditions Coastal Protection and Restoration Authority This document was prepared in support of the 2017 Coastal Master Plan being prepared by the Coastal Protection and Restoration Authority (CPRA). CPRA was established by the Louisiana Legislature in response to Hurricanes Katrina and Rita through Act 8 of the First Extraordinary Session of 2005. Act 8 of the First Extraordinary Session of 2005 expanded the membership, duties and responsibilities of CPRA and charged the new authority to develop and implement a comprehensive coastal protection plan, consisting of a master plan (revised every five years) and annual plans. CPRA’s mandate is to develop, implement and enforce a comprehensive coastal protection and restoration master plan. Suggested Citation: Zhao, H., Atkinson, J., and Roberts, H. (2016). 2017 Coastal Master Plan Modeling: Attachment C3-3 – Storms in the ICM Boundary Conditions. Version I. (p. 63). Baton Rouge, Louisiana: Coastal Protection and Restoration Authority. Page | ii 2017 Coastal Master Plan: Storms in the ICM Boundary Conditions Acknowledgements This document was developed as part of a broader Model Improvement Plan in support of the 2017 Coastal Master Plan under the guidance of the Modeling Decision Team (MDT): The Water Institute of the Gulf - Ehab Meselhe, Alaina Grace, and Denise Reed Coastal Protection and Restoration Authority (CPRA) of Louisiana - Mandy Green, Angelina Freeman, and David Lindquist This effort was funded by CPRA of Louisiana under Cooperative Endeavor Agreement Number 2503-12-58, Task Order No. -
A Time Line of Cedar Bayou
A TIME LINE OF CEDAR BAYOU George H. Ward Center for Research in Water Resources The University of Texas at Austin TWDB - UTA Interagency Contract No. 0900010973 TWDB – TGLO Interagency Contract No. 0900010961 and 09-231-000-3774 MMS Contract No. M09AF15300 Biological Study of San Antonio Bay Task 5 – Cedar Bayou History Project Officer: Carla Guthrie, Ph.D. Surface Water Resources Division Texas Water Development Board 25 August 2010 THIS REPORT (STUDY) IS FUNDED WITH QUALIFIED OUTER CONTINENTAL SHELF OIL AND GAS REVENUES BY THE COASTAL IMPACT ASSISTANCE PROGRAM, U.S. FISH AND WILDLIFE SERVICE, U.S. DEPARTMENT OF THE INTERIOR. THE VIEWS AND CONCLUSIONS EXPRESSED HEREIN ARE THOSE OF THE AUTHOR(S) AND DO NOT NECESSARILY REFLECT THE VIEWS OF THE U.S. GOVERNMENT. ii EXECUTIVE SUMMARY Exchanges with the sea are an important feature of the hydrography of an estuary. For San Antonio Bay, the principal exchanges occur through the Pass Cavallo complex (including the Matagorda Entrance Channel) and through Aransas Pass. The closest inlet to the bay, however, is Cedar Bayou, which separates Matagorda Island and San Jose Island. When open, Cedar Bayou is an effective passage for migratory organisms, so analysis of long-term organism abundance data requires knowledge of the state of the pass. Cedar Bayou has existed as a channel crossing the barrier island for nearly 2500 years. Authoritative surveys establish that its gross physiographic features, notably its NNE-SSW trend across the island and the washover fan to its west, have not substantially changed since before the Civil War. This project constructed a chronology for Cedar Bayou for 1900-2009. -
Hurricane Sandy 2012
EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Open Access Open Access Nat. Hazards Earth Syst. Sci. Discuss.,Natural 1, 625–679, Hazards 2013 Natural Hazards www.nat-hazards-earth-syst-sci-discuss.net/1/625/2013/ and Earth System doi:10.5194/nhessd-1-625-2013and Earth System NHESSD Sciences Sciences © Author(s) 2013. CC Attribution 3.0 License. 1, 625–679, 2013 Discussions Open Access Open Access Atmospheric Atmospheric This discussion paper is/has been under review for the journal Natural Hazards and Earth Chemistry Chemistry Hurricane Sandy System Sciences (NHESS). Please refer to the corresponding final paper in NHESS if available. and Physics and Physics 2012 Discussions Open Access Open Access M. Kunz et al. Investigation ofAtmospheric superstorm SandyAtmospheric 2012 in Measurement Measurement a multi-disciplinaryTechniques approach Techniques Title Page Discussions Open Access 1,2 1,2 1,3 1,3 1,3 Open Access 1,3 M. Kunz , B. Muhr¨ , T. Kunz-Plapp , J.E. Daniell , B. Khazai , F. Wenzel , Abstract Introduction Biogeosciences M. Vannieuwenhuyse1,4,Biogeosciences T. Comes1,4, F. Elmer1,5, K. Schroter¨ 1,6, J. Fohringer1,7, Discussions Conclusions References T. Munzberg¨ 1,8, C. Lucas1,9, and J. Zschau1,10 Open Access 1 Open Access Tables Figures Center for Disaster Management and Risk Reduction Technology (CEDIM),Climate Potsdam and Karlsruhe, Germany Climate of the Past