TIROS V VIEWS FINAL STAGES in the LIFE of TYPHOON SARAH AUGUST 1962 CAPT.ROBERT W
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
An Evaluation of the Harbor of Cebu City, Republic of the Philippines As a Typhoon Haven
1 AN EVALUATION OF THE HARBOR OF CEBU CITY, REPUBLIC OF THE PHILIPPINES AS A TYPHOON HAVEN Benny K. Hassel DUDLEY KNOX i-.iiKAKY NAVAL POSTGRADUATE SCHOo. MONTEREY. CALIFORNIA 9394U NAVAL POSTGRADUATE SCHOOL Monterey, California THESIS An Evaluation of the Harbor of Cebu C ity, Republic of the Philipp ines as a Typhoon Haven by Benny K. Hasse 1 1 March 1976 Thesis Advisor: G. J. Haltiner Approved for public release; distribution unlimited. U173527 n A.S^IFIF Q SECURITY CUASSlFICAnoM OF THIS t'AGF. (•^Ti.n Darn ZnlTod) READ INSTRUCTIONS REPORT DOCUMENTATION PAGE BEFORK COMPLETING FORM t. REPORT NUMSER 2. GOVT ACCESSION NO. 3. REC1?"ICNT'S CATALOG NUMOER 4. TITLE (and Subtlllo) 5. TYPE OF REPORT 4 PERIOD COVERED Master ' s Thes i s An Evaluation of the Harbor of Cebu, March 1976 Republic of the Philippines 6. PERFORMING ORG. REPORT NUMBER as a Typhoon Haven 7. AUTHORf»; 8. CONTRACT OR GRANT NUMBERCaJ Benny Kyle Hassell 9 PERFORMING ORGANIZATION NAME ANO ADDRESS 10. PROGRAM ELEMENT. PROJECT. TASK AREA 4 WORK UNIT NUMBERS Naval Postgraduate School Monterey, CA 93940 tl. CONTROLLING OFFICE NAME AND ADDRESS 12 REPORT DATE Naval Postgraduate School March 1976 13. NUMBER OF PAGES Monterey, CA 93940 74 U. MONITORING AGENCY fiAME 4 ADOR ESSri/ i///or«n» Irom Controlllnt Oltlc») 15. SECURITY CLASS, (ol thl» report) Naval Postgraduate School UNCLASSIFIED Monterey, CA 93940 15«. DECLASSIFICATION/ DOWN GRADING SCHEDULE IS. DISTRIBUTION ST AT EMEN T fo/ ;h(» Report; Approved for public release; distribution unlimited. 17. DISTRIBUTION STATEMENT (ol th» abttract *nfr»d In Block 30, // dlllmrtnt Itom Rmpott) 19. -
Vulnerability Assessment of Olango Island to Predicted Climate Change and Sea Level Rise
Vulnerability assessment of Olango Island to predicted climate change and sea level rise Amuerfino Mapalo Department of Environment and Natural Resources, Region 7 Banilad, Mandaue City, Cebu, Philippines, 6014 ([email protected]) Executive summary The Asia-Pacific Network for Global Change Research (APN) funded a study assessing the vulnerability of Olango Island, in the Central Philippines, to predicted climate change and sea level rise. The study was coordinated by the Environmental Research Institute of the Supervising Scientist (eriss), in Australia, and Wetlands International–Oceania, with the major local collaborator being the Philippines Department of Environment and Natural Resources (DENR). The study’s major objectives were to raise awareness of the issue of climate change and sea level rise in the Asia-Pacific region, to provide advice and training to national and local agencies on procedures for Vulnerability Assessment, and specifically, to obtain a preliminary understanding of the potential impacts of climate change and sea level rise on the biological, physical and socio-economic attributes of Olango Island. Olango Island was chosen as a study site for several reasons: It is a small, coral reef island (~6 × 3 km) with low topographical relief and a maximum elevation above sea level of only 9 m; it sustains a population of over 20 000 and is already under pressure from anthropogenic activities including fishing, groundwater extraction and mangrove harvesting; it is a major wetland site for shorebirds, being nominated for the East Asian–Australasian Shorebird Reserve Network and listed as a wetland of international importance by the Ramsar Wetland Convention. Due to its importance as a flyway stopover site, a 920 ha wildlife sanctuary was established in the south of the island. -
Disaster Preparedness Checklist
DISASTER PREPAREDNESS GO BAG: What to prepare? Emergency Contacts Out of Region Contact THE CHECKLIST Name: _______________________________________ Address: _____________________________________ _____________________________________________ Cell Phone ____________________________________ Home Phone __________________________________ Emergency Kit Work Phone ___________________________________ Local Contact Name: _______________________________________ Address: ______________________________________ _____________________________________________ Cell Phone: ___________________________________ Gears and Tools Home Phone __________________________________ Work Phone: __________________________________ The Philippine Quakes The Philippine Typhoons The Philippine archipelago is located along the Pacific Ring of Fire, the home ...in the next of 90 percent of earthquakes. As a country, Philippines had experienced some Typhoon Yolanda, after sustaining at the speed major tremors and the most recent was the October 15, 2013 in the islands of Bohol, which epicenter was located at the municipality of Sagbayan. of 314 km per hour, accelerated to 378kph making the When disaster happens… 4th strongest typhoon to hit in the country. Among the most destructive earthquakes in the country according to the magnitude of the tremors scaled at Philippine Seismic Intensity standard Will you survive the next 72 hours? 1. Unleashing the windy fury in the islands of Ormoc were: and Leyte on November 15, 1991, Tropical What do you have to sustain in the next three days without an Storm Thelma killed 5,100 people. 1. The 7.3 magnitude that hit the town of Casiguan, Aurora in 1968. The open shop around? tremor was felt almost in the entire Luzon area. Some business towers 2. Typhoon Bopha hit Southern Mindanao on in Manila area collapsed, killing 300 tenants inside the six-story Ruby December 3, 2012, unleashing its strength to the Tower in Binondo. -
Tropical Cyclones in 1991
ROYAL OBSERVATORY HONG KONG TROPICAL CYCLONES IN 1991 CROWN COPYRIGHT RESERVED Published March 1993 Prepared by Royal Observatory 134A Nathan Road Kowloon Hong Kong Permission to reproduce any part of this publication should be obtained through the Royal Observatory This publication is prepared and disseminated in the interest of promoting the exchange of information. The Government of Hong Kong (including its servants and agents) makes no warranty, statement or representation, expressed or implied, with respect to the accuracy, completeness, or usefulness of the information contained herein, and in so far as permitted by law, shall not have any legal liability or responsibility (including liability for negligence) for any loss, damage or injury (including death) which may result whether directly or indirectly, from the supply or use of such information. This publication is available from: Government Publications Centre General Post Office Building Ground Floor Connaught Place Hong Kong 551.515.2:551.506.1 (512.317) 3 CONTENTS Page FRONTISPIECE: Tracks of tropical cyclones in the western North Pacific and the South China Sea in 1991 FIGURES 4 TABLES 5 HONG KONG'S TROPICAL CYCLONE WARNING SIGNALS 6 1. INTRODUCTION 7 2. TROPICAL CYCLONE OVERVIEW FOR 1991 11 3. REPORTS ON TROPICAL CYCLONES AFFECTING HONG KONG IN 1991 19 (a) Typhoon Zeke (9106): 9-14 July 20 (b) Typhoon Amy (9107): 16-19 July 24 (c) Severe Tropical Storm Brendan (9108): 20-24 July 28 (d) Typhoon Fred (9111): 13-l8 August 34 (e) Severe Tropical Storm Joel (9116): 3-7 September 40 (f) Typhoon Nat (9120): 16 September-2 October 44 4. -
Super Typhoon Haiyan / Yolanda – Report
Center for Disaster Management and Risk Reduction Technology CEDIM Forensic Disaster Analysis Group (FDA) Super Typhoon Haiyan / Yolanda – Report 13.11.2013 – Report No. 2, Focus on Philippines – 18:00 GMT Authors: James Daniell, Bernhard Mühr, Trevor Girard, André Dittrich, Joachim Fohringer, Christian Lucas, Tina Kunz-Plapp Official Disaster Name Date Landfall UTC Local Duration (PHL) Yolanda (International: Haiyan) From 4-11 7.11. 20:40 +8 30 hours Preferred Hazard Information: Path Speed Definition Width (km) Gust (Peak) Landfall Sustained 280W (PH) then 325W (VN) 30-40kph Category 5 Max: 150 379kph 312kph 250kph JTWC JTWC Location Information: Economic Country ISO Provinces/Regions Most Impact Exposure HDI (2012) Urbanity Pop. affected IV, V, VI, VII, VIII, Leyte, Samar, Philippines PH X, XI, XIII Tacloban Ca. $104b 0.654 55% Ca. 14 million Vietnam, China VN North of Da Nang Coastal regions n/a 0.617 45% 600,000 evac. Preferred Hazard Information: Philippines Vietnam China Key Hazard Metrics Typhoon (Cat. 5) Category 4 Unk. Leyte, Dinagat, Samar, Aklan, Capiz, Guimares, Cebu (all on Hazard Description (Wind speed etc.) Philippines), with wind speeds exceeding 185kph The category 5 typhoon made landfall near Guiuan on Eastern Samar at 07.11 at 20:40 UTC and hit with the strongest landfall wind speeds ever observed. Previously, the typhoon had hit the small nation of Palau causing some damage. Wind gust speeds reached a predicted 380 kph shortly before impact.The warm sea water and low wind shear has contributed to the maximum intensity of this typhoon before landfall. The central pressure was estimated 885 hPa (according Joint Typhoon Warning Center), which makes it only the 5th in 25 years in the Western Pacific to do so (Megi 2010, Flo 1990, Ruth 1991, Yuri 1991). -
A Community Based Mangrove Rehabilitation of High Energy Coasts in Pedada Bay, Philippines
Journal of Tropical Forest Research 3 (1) : 36-53 (2019) Original article A Community Based Mangrove Rehabilitation of High Energy Coasts in Pedada Bay, Philippines Keita Furukawa1, 2, 3* Jurgenne H. Primavera4 Rona Joy A. Loma4 Christian L. Montilijao4 Jofel D. Coching4 Yvainne Y. Sta. Maria5 Fernando P. Siringan5 1Ocean Policy Research Institute, SPF, Toranomon, Minato-ku, Tokyo 1058524 Japan 2Yokohama National University, Tokiwadai, Hodogaya-ku, Yokohama, 2408531 Japan 3Association for Shore Environment Creation, Hiranuma, Nishi-ku, Yokohama, 2200023 Japan 4Zoological Society of London-Philippines, Brgy. Magdalo, La Paz, Iloilo City, 5000 Philippines 5Marine Science Institute, University of the Philippines, Diliman, Quezon City, 1101 Philippines *Corresponding Author, E-mail: [email protected] Received: Feb 13, 2019 Revised : May 7, 2019 Accepted : Jun 11, 2019 ABSTRACT For coastal communities, fringe mangrove forests can help to protect their coasts from high energy waves and provide various ecosystem services. Nevertheless, these forests are under threat of damage caused by climate change and variability and stress related to development. Coastal hydrology / morphology is one of key processes to be monitored and assessed to implement an appropriate management especially for mangrove rehabilitation. This paper reports on the lessons learnt from the Community based mangrove rehabilitation of a fringed mangrove project in the Pedada bay, Philippine. The sea floor level in the area was too low (less than 0.5 m below the Mean Sea Level or MSL) and exposed to high energy waves from the sea. A pair of breakwaters was constructed for reducing the wave energy, but sea floor level could not be amended artificially in January 2010. -
Holds Info Its Second Day Today Typhoon Thelma Strikes Taiwan
/ .. / VOLUME 14 KWAJALEIN ATOLL, MARSHALL ISLANDS, TUESDAY, JULY 26, 1977 NUMBER 144 Libyan.Egyptian Cease·fire Shaleily fULL·SCALE RECOGNITION GRANTED Holds Info Its Second Day Today DESPITE A REQUEST fROM CARTER CAIRO (UPI) -- The Libyan-Egyptian cease-fire apparently held TEL AVIV (UPI) -- Israel granted full-scale recognltlon today lnto ltS second day today despite no publlC acceptance by Llbya, to three Jewish settlements in the occupied West Bank of Jordan. reportedly because Egyptian President Anwar Sadat wants sophisti The move came desplte a reported request by President Carter cated Sovlet equipment removed from the border. to avold such actlons until a peace conference wlth the Arabs Neither side had reported any further shootlng after six days that may be convened ln the fall. It came a day after Prime Mln of warplane, tank and artlllery battles which ended Sunday night, ister Benahem Begin's return from the United States. as Sadat prepared to make a maJor natlonally-televlsed speech in "We were expecting lt and it was self-understood, blessed be Alexandria tonight. God," said Zvi Slonim, a spokesman for the Gush Emunlm movement. Informed political sources said Libyan leader Col. Moammar The group established unauthorized settlements in the West Bank Khadafy was withholding any desplte the oppositlon of the public acknowledgment of the de previous Labor Party government. facto cease-fire because one of u.s. AGREES TO LEA VE HEADQUARTERS Of The settlements affected by Sadat's demands is that sensi the decision of a Joint -
Estimation of Probable Maximum Precipitation in Korea Using a Regional Climate Model
water Article Estimation of Probable Maximum Precipitation in Korea using a Regional Climate Model Jeonghoon Lee 1, Jeonghyeon Choi 1, Okjeong Lee 1, Jaeyoung Yoon 2 and Sangdan Kim 3,* 1 Environmental System Science (Major of Environmental Engineering), Pukyong National University, Busan 48513, Korea; [email protected] (J.L.); [email protected] (J.C.); [email protected] (O.L.) 2 Department of Environmental Engineering, Korea University, Sejong 30019, Korea; [email protected] 3 Department of Environmental Engineering, Pukyong National University, Busan 48513, Korea * Correspondence: [email protected]; Tel.: +82-051-629-6529 Academic Editor: Athanasios Loukas Received: 19 January 2017; Accepted: 24 March 2017; Published: 30 March 2017 Abstract: Extreme precipitation events have been extensively applied to the design of social infra structures. Thus, a method to more scientifically estimate the extreme event is required. This paper suggests a method to estimate the extreme precipitation in Korea using a regional climate model. First, several historical extreme events are identified and the most extreme event of Typhoon Rusa (2002) is selected. Second, the selected event is reconstructed through the Weather Research and Forecasting (WRF) model, one of the Regional Climate Models (RCMs). Third, the reconstructed event is maximized by adjusting initial and boundary conditions. Finally, the Probable Maximum Precipitation (PMP) is obtained. The WRF could successfully simulate the observed precipitation in terms of spatial and temporal distribution (R2 = 0.81). The combination of the WRF Single-Moment (WSM 6-class graupel scheme (of microphysics), the Betts-Miller-Janjic scheme (of cumulus parameterization) and the Mellor-Yamada-Janjic Turbulent Kinetic Energy (TKE) scheme (of planetary boundary layer) was determined to be the best combination to reconstruct Typhoon Rusa. -
Herter Outlines Plan to Ease World Strife
« i"'' WEDNESDAY, SEPTEMBER 1*, 19BI tAGM TWENTY-ETGHT Hanrh^istpr lEnenittg 1|i?ralb Aveng* Daily N«t Pr«M Ron The Waalhar rw r Mm W s M i OWtod Peraeaat af 0. R. Waatbai •.ami lUy ttrfi. IMW msklflg 6 turn Into th# westbound ] I Mia* Busan King, daughter of MiH Judith Taitl, daughUr of Rockville Driver portion of the street. As her] Oeo) wtdeapread tro ti trndgM. Mr. and Mrs. James V. Tapi. Con the left lane, it^ L T. WOOD 00. Utr. and Mr*. Haiwey King, 218 ear moved Jnto 12,925 O m la 86a. P a ir cswitlaiM d aaal About Town HeniA- St . naa enrolled as a fresh- cord Rd , has returned to ,Mary-1 CUUIUITUcollided witlfrr.^.w -.a car.................. driven east ' ICE P U N T ' mount College, Tartytown, N Y . , i Injured in Crash •Uttber «f Mm AndH tamermw. Wgh aear aa. man ' at New Elngland College. thaTlane by Morgan F. Steele. 22, St BItMBLL OT. BorsMi pf OraolaMM Robert 2. HoUenbech, formerly Henniker, N. H Her sister. Miss to begin her. sophomore year. of 205 Porter St. Mancheater-r-A City of VUlago Chorm nf i3 Oreen Hill Rd., ha* Joined .Nancy King, has returned to Lea> ^ Rockville driver, John Martin. Damage was light, according t o , Cu beB-C.riukeiUBlockB the facuJtv of Ixw-ell TechnoloRi- ley College. Cambridge, Mass , as The first fall meeting of Cfiar-I 62, of Ellingtoir Av*„ was taken to police, and no one was hurl. Mr*.; cal Inatltiite. Lmvell. Maas., as an ter Oak lodges, B'nal B’rlth. -
Significant Data on Major Disasters Worldwide, 1900-Present
DISASTER HISTORY Signi ficant Data on Major Disasters Worldwide, 1900 - Present Prepared for the Office of U.S. Foreign Disaster Assistance Agency for International Developnent Washington, D.C. 20523 Labat-Anderson Incorporated Arlington, Virginia 22201 Under Contract AID/PDC-0000-C-00-8153 INTRODUCTION The OFDA Disaster History provides information on major disasters uhich have occurred around the world since 1900. Informtion is mare complete on events since 1964 - the year the Office of Fore8jn Disaster Assistance was created - and includes details on all disasters to nhich the Office responded with assistance. No records are kept on disasters uhich occurred within the United States and its territories.* All OFDA 'declared' disasters are included - i.e., all those in uhich the Chief of the U.S. Diplmtic Mission in an affected country determined that a disaster exfsted uhich warranted U.S. govermnt response. OFDA is charged with responsibility for coordinating all USG foreign disaster relief. Significant anon-declared' disasters are also included in the History based on the following criteria: o Earthquake and volcano disasters are included if tbe mmber of people killed is at least six, or the total nmber uilled and injured is 25 or more, or at least 1,000 people art affect&, or damage is $1 million or more. o mather disasters except draught (flood, storm, cyclone, typhoon, landslide, heat wave, cold wave, etc.) are included if the drof people killed and injured totals at least 50, or 1,000 or mre are homeless or affected, or damage Is at least S1 mi 1l ion. o Drought disasters are included if the nunber affected is substantial. -
WAKE ISLAND HALS UM-1 (Wake Island National Historic Landmark) HALS UM-1 (Peale Island) (Wilkes Island) (Wake Atoll) Wake Island US Minor Islands
WAKE ISLAND HALS UM-1 (Wake Island National Historic Landmark) HALS UM-1 (Peale Island) (Wilkes Island) (Wake Atoll) Wake Island US Minor Islands PHOTOGRAPHS WRITTEN HISTORICAL AND DESCRIPTIVE DATA FIELD RECORDS HISTORIC AMERICAN LANDSCAPES SURVEY National Park Service U.S. Department of the Interior 1849 C Street NW Washington, DC 20240-0001 HISTORIC AMERICAN LANDSCAPES SURVEY WAKE ISLAND (Wake Island National Historic Landmark) HALS No. UM-1 Location: Wake Atoll is a small tropical coral atoll in the Pacific Ocean consisting of three islands (Peale, Wake, and Wilkes) enclosing the shallow, central lagoon and surrounded by a narrow fringing reef. From reef to reef, the atoll is approximately 5 miles long and 2.5 miles wide. At 19 degrees 17 minutes north latitude and 166 degrees 3 8 minutes east longitude, the atoll lies just west of the International Date Line. Wake Atoll is 2,458 miles west ofHawai'i, 1,591 miles east of Guam, and 691 miles north ofKwajalein in the Marshall Islands (Aaron 2008:1-1). (Refer to Figure 1). Present Owner: Wake Island is an unorganized, unincorporated territory (possession) of the United States, part of the United States Minor Outlying Islands, administered by the Office of Insular Affairs, U.S. Department of the Interior (Aaron 2008b and Aaron 2008: 1-1 ). Effective October 1, 2010, 611 th Air Force in Alaska assumed management responsibility for the atoll. Previously, this responsibility was under 15th Air Wing (AW) of the U.S. Air Force (USAF) at Hickam AFB in Honolulu. Present Occupant and Use: Access to the island is managed by the U.S. -
Prediction of a Typhoon Track Using a Generative Adversarial Network And
www.nature.com/scientificreports OPEN Prediction of a typhoon track using a generative adversarial network and satellite images Received: 25 September 2018 Mario Rüttgers , Sangseung Lee , Soohwan Jeon & Donghyun You Accepted: 29 March 2019 Tracks of typhoons are predicted using a generative adversarial network (GAN) with satellite images Published: xx xx xxxx as inputs. Time series of satellite images of typhoons which occurred in the Korea Peninsula in the past are used to train the neural network. The trained GAN is employed to produce a 6-hour-advance track of a typhoon for which the GAN was not trained. The predicted track image of a typhoon favorably identifes the future location of the typhoon center as well as the deformed cloud structures. Errors between predicted and real typhoon centers are measured quantitatively in kilometers. An averaged error of 95.6 km is achieved for tested 10 typhoons. Predicting sudden changes of the track in westward or northward directions is identifed as a challenging task, while the prediction is signifcantly improved, when velocity felds are employed along with satellite images. Every year tropical cyclones cause death and damage in many places around the world. Cyclones are formed when water at the sea surface becomes warm, evaporates, and rises in a form of clouds, and while it cools down, the con- densation releases strong energy in a form of winds. Rotation of the earth gives a cyclone its spinning motion. At the center usually a hole forms, which is called an eye of the cyclone. At the eye, the pressure is low and energetic clouds and winds get attracted.