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Cruising Guide to the Philippines
Cruising Guide to the Philippines For Yachtsmen By Conant M. Webb Draft of 06/16/09 Webb - Cruising Guide to the Phillippines Page 2 INTRODUCTION The Philippines is the second largest archipelago in the world after Indonesia, with around 7,000 islands. Relatively few yachts cruise here, but there seem to be more every year. In most areas it is still rare to run across another yacht. There are pristine coral reefs, turquoise bays and snug anchorages, as well as more metropolitan delights. The Filipino people are very friendly and sometimes embarrassingly hospitable. Their culture is a unique mixture of indigenous, Spanish, Asian and American. Philippine charts are inexpensive and reasonably good. English is widely (although not universally) spoken. The cost of living is very reasonable. This book is intended to meet the particular needs of the cruising yachtsman with a boat in the 10-20 meter range. It supplements (but is not intended to replace) conventional navigational materials, a discussion of which can be found below on page 16. I have tried to make this book accurate, but responsibility for the safety of your vessel and its crew must remain yours alone. CONVENTIONS IN THIS BOOK Coordinates are given for various features to help you find them on a chart, not for uncritical use with GPS. In most cases the position is approximate, and is only given to the nearest whole minute. Where coordinates are expressed more exactly, in decimal minutes or minutes and seconds, the relevant chart is mentioned or WGS 84 is the datum used. See the References section (page 157) for specific details of the chart edition used. -
Appendix 8: Damages Caused by Natural Disasters
Building Disaster and Climate Resilient Cities in ASEAN Draft Finnal Report APPENDIX 8: DAMAGES CAUSED BY NATURAL DISASTERS A8.1 Flood & Typhoon Table A8.1.1 Record of Flood & Typhoon (Cambodia) Place Date Damage Cambodia Flood Aug 1999 The flash floods, triggered by torrential rains during the first week of August, caused significant damage in the provinces of Sihanoukville, Koh Kong and Kam Pot. As of 10 August, four people were killed, some 8,000 people were left homeless, and 200 meters of railroads were washed away. More than 12,000 hectares of rice paddies were flooded in Kam Pot province alone. Floods Nov 1999 Continued torrential rains during October and early November caused flash floods and affected five southern provinces: Takeo, Kandal, Kampong Speu, Phnom Penh Municipality and Pursat. The report indicates that the floods affected 21,334 families and around 9,900 ha of rice field. IFRC's situation report dated 9 November stated that 3,561 houses are damaged/destroyed. So far, there has been no report of casualties. Flood Aug 2000 The second floods has caused serious damages on provinces in the North, the East and the South, especially in Takeo Province. Three provinces along Mekong River (Stung Treng, Kratie and Kompong Cham) and Municipality of Phnom Penh have declared the state of emergency. 121,000 families have been affected, more than 170 people were killed, and some $10 million in rice crops has been destroyed. Immediate needs include food, shelter, and the repair or replacement of homes, household items, and sanitation facilities as water levels in the Delta continue to fall. -
Member Report (Malaysia)
MEMBER REPORT (MALAYSIA) ESCAP/WMO Typhoon Committee 15th Integrated Workshop Video Conference 1-2 December 2020 Organised by Viet Nam Table of Contents I. Overview of tropical cyclones which have affected/impacted Malaysia in 2020 1. Meteorological Assessment (highlighting forecasting issues/impacts) 2. Hydrological Assessment (highlighting water-related issues/impact) (a) Flash flood in Kajang & Kuala Lumpur in July and September 2020 (b) Enhancement of Hydrological Data Management for DID Malaysia (c) Hydrological Instrumentation Updates for Malaysia (d) Drought Monitoring Updates 3. Socio-Economic Assessment (highlighting socio-economic and DRR issues/impacts) 4. Regional Cooperation Assessment (highlighting regional cooperation successes and challenges) II. Summary of progress in Priorities supporting Key Result Areas 1. Annual Operating Plan (AOP) for Working Group of Meteorology [AOP4: Radar Integrated Nowcasting System (RaINS)] 2. Annual Operating Plan (AOP) for Working Group of Hydrology (AOP2, AOP4, AOP5, AOP6) 3. The Government of Malaysia’s Commitment Towards Supporting the Sendai Framework for Disaster Risk Reduction I. Overview of tropical cyclones which have affected/impacted Malaysia in 2020 1. Meteorological Assessment (highlighting forecasting issues/impacts) During the period of 1 November 2019 to 31 October 2020, 27 tropical cyclones (TCs) formed over the Western Pacific Ocean, the Philippines waters as well as the South China Sea. Eight of the TCs entered the area of responsibility of the Malaysian Meteorological Department (MET Malaysia) as shown in Figure 1. The TCs, which consisted of seven typhoons and a tropical storm that required the issuance of strong winds and rough seas warnings over the marine regions under the responsibility of MET Malaysia, are listed in Table 1. -
Minnesota Weathertalk Newsletter for Friday, January 3, 2014
Minnesota WeatherTalk Newsletter for Friday, January 3, 2014 To: MPR's Morning Edition From: Mark Seeley, Univ. of Minnesota, Dept of Soil, Water, and Climate Subject: Minnesota WeatherTalk Newsletter for Friday, January 3, 2014 HEADLINES -December 2013 was climate near historic for northern communities -Cold start to 2014 -Weekly Weather potpourri -MPR listener questions -Almanac for January 3rd -Past weather -Outlook Topic: December 2013 near historic for far north In assessing the climate for December 2013 it should be said that from the standpoint of cold temperatures the month was quite historic for many northern Minnesota communities, especially due to the Arctic cold that prevailed over the last few days of the month. Minnesota reported the coldest temperature in the 48 contiguous states thirteen times during the month, the highest frequency among all 48 states. Many northern observers saw overnight temperatures drop below -30 degrees F on several occasions. The mean monthly temperature for December from several communities ranked among the coldest Decembers ever. A sample listing includes: -4.1 F at International Falls, 2nd coldest all-time 4.6 F at Duluth, 8th coldest all-time 0.1 F at Crookston, 3rd coldest all-time -3.1 F at Roseau, 3rd coldest all-time 0.3 F at Park Rapids, 3rd coldest all-time -4.4 F at Embarrass, 2nd coldest all-time -4.1 F at Baudette, coldest all-time -3.7 F at Warroad, coldest all-time -2.9 F at Babbitt, coldest all-time -2.8 F at Gunflint Lake, coldest all-time In addition, some communities reported an exceptionally snowy month of December. -
Words: Corner Beam-Column Joint; Hysteresis Loops; Seismic Design; Ductility; Stiffness; Equivalent Viscous Damping
Journal of Mechanical Engineering Vol 16(1), 213-226, 2019 Validation of Corner Beam-column Joint’s Hysteresis Loops between Experimental and Modelled using HYSTERES Program N.F. Hadi, M. Mohamad Faculty of Civil Engineering, Universiti Teknologi MARA 40450 Shah Alam, Selangor, Malaysia N.H. Hamid Institute of Infrastructure Engineering Sustainability and Management Universiti Teknologi MARA 40450 Shah Alam, Selangor, Malaysia ABSTRACT The beam - column joint is an important part of a multi-storey RC building as it caters for lateral and gravitational load during an earthquake event. The beam-column joints should have a medium to high ductility for transferring the earthquake load and gravity load to the foundation. By designing multi- storey RC buildings using Eurocode 8 can avoid any diagonal shear cracks in column which is a major problem in non-seismic design buildings using British Standard (BS8110). This paper presents the experimental hysteresis loops of monolithic corner beam-column joints of multi-storey building which had been designed using Eurocode 8 and tested under in-plane lateral cyclic loading. The experimental hysteresis loops of corner beam-column joint was compared with modelled using the HYSTERES program. The full-scale corner beam- column joint of a two story precast school building was designed, constructed, tested and modelled is presented herein. The seismic performance parameters such as lateral strength capacity, stiffness, ductility and equivalent viscous damping were compared between experimental and modelled hysteresis loops. The experimental hysteresis loops have similar shape with the modeling hysteresis loops with small percentage differences between them. Keywords: Corner beam-column joint; hysteresis loops; seismic design; ductility; stiffness; equivalent viscous damping ___________________ ISSN 1823-5514, eISSN2550-164X Received for review: 2017-07-10 © 2016 Faculty of Mechanical Engineering, Accepted for publication: 2018-05-18 Universiti Teknologi MARA (UiTM), Malaysia. -
Information Bulletin Philippines: Typhoon Ambo (Vongfong)
Information bulletin Philippines: Typhoon Ambo (Vongfong) Glide n° TC-2020-000134-PHL Date of issue: 14 May 2020 Date of disaster Expected landfall on 14 May 2020 Point of contact: Leonardo Ebajo, PRC Disaster Management Services Operation start date: N/A Expected timeframe: N/A Category of disaster: N/A Host National Society: Philippine Red Cross (PRC) Number of people affected: 7.1 million exposed Number of people to be assisted: N/A N° of National Societies currently involved in the operation: N/A N° of other partner organizations involved in the operation: N/A This bulletin is being issued for information only and reflects the current situation and details available at this time. The Philippine Red Cross (PRC), with the support of the International Federation of Red Cross and Red Crescent Societies (IFRC) is not seeking funding or other assistance from donors for this operation at this time. However, this might change as the situation evolves, especially after the storm makes landfall. An imminent DREF activation is currently under consideration. <click here to view the map of the affected area, and click here for detailed contact information> The situation According to the Philippines Atmospheric Geophysical and Astronomical Services Administration (PAGASA) as of 04:00 hours local time on 14 May 2020, Typhoon Vongfong is approximately 230 kilometers east of the Catarman, Northern Samar, moving west at 15 kmph. On entering the Philippine Area of Responsibility (PAR), it has been locally named “Typhoon Ambo”. PAGASA reports that Typhoon Ambo has maximum sustained winds of 150 kmph near the center and gustiness of up to 185 kmph. -
Cover 2Nd Asean Env Report 2000
SecondSecond ASEANASEAN State State ofof thethe EnvironmentEnvironment ReportReport 20002000 Second ASEAN State of the Environment Report 2000 Our Heritage Our Future Second ASEAN State of the Environment Report 2000 Published by the ASEAN Secretariat For information on publications, contact: Public Information Unit, The ASEAN Secretariat 70 A Jalan Sisingamangaraja, Jakarta 12110, Indonesia Phone: (6221) 724-3372, 726-2991 Fax : (6221) 739-8234, 724-3504 ASEAN website: http://www.aseansec.org The preparation of the Second ASEAN State of the Environment Report 2000 was supervised and co- ordinated by the ASEAN Secretariat. The following focal agencies co-ordinated national inputs from the respective ASEAN member countries: Ministry of Development, Negara Brunei Darussalam; Ministry of Environment, Royal Kingdom of Cambodia; Ministry of State for Environment, Republic of Indonesia; Science, Technology and Environment Agency, Lao People’s Democratic Republic; Ministry of Science Technology and the Environment, Malaysia; National Commission for Environmental Affairs, Union of Myanmar; Department of Environment and Natural Resources, Republic of the Philippines; Ministry of Environment, Republic of Singapore; Ministry of Science, Technology and the Environment, Royal Kingdom of Thailand; and Ministry of Science, Technology and the Environment, Socialist Republic of Viet Nam. The ASEAN Secretariat wishes to express its sincere appreciation to UNEP for the generous financial support provided for the preparation of this Report. The ASEAN Secretariat also wishes to express its sincere appreciation to the experts, officials, institutions and numerous individuals who contributed to the preparation of the Report. Every effort has been made to ensure the accuracy of the information presented, and to fully acknowledge all sources of information, graphics and photographs used in the Report. -
Effect of Fine Content on Soil Dynamic Properties
Journal of Engineering Science and Technology Vol. 13, No. 4 (2018) 851 - 861 © School of Engineering, Taylor’s University EFFECT OF FINE CONTENT ON SOIL DYNAMIC PROPERTIES J. X. LIM, M. L. LEE*, Y. TANAKA Department of Civil Engineering, Lee Kong Chian Faculty of Engineering and Science, Universiti Tunku Abdul Rahman, 43000, Kajang, Selangor DE, Malaysia *Corresponding Author: [email protected] Abstract Dynamic properties of soil have attracted an increasing attention among geotechnical engineers in Malaysia owing to the frequent earthquake incidents reported recently and the demand of high speed railway infrastructures. The present study investigated the effect of fine content on the soil dynamic properties based on three selected soils in Malaysia. One sand mining trail (i.e. silty sand) and two tropical residual soils (i.e. sandy clay and sandy silt) were tested on a 1 g shaking table. The experimental shear moduli were compared with the established degradation curves of sandy and clayey soils obtained from literature. The shear moduli attenuated with the increase of shear strain amplitude for the three soil samples. The amount of fine content in the soil was found to be a more dominant factor affecting the dynamic properties of soil compared with the plasticity and geological characteristics of the soil. The experimental shear moduli of sandy silt were similar to that of sandy clay. It may be attributed to the fact that the two studied residual soils have a similar amount of fine content. In addition, the shear moduli of the studied residual soils could not be fitted to the degradation curves of sand and clay which have been well studied in the past. -
Capital Adequacy (E) Task Force RBC Proposal Form
Capital Adequacy (E) Task Force RBC Proposal Form [ ] Capital Adequacy (E) Task Force [ x ] Health RBC (E) Working Group [ ] Life RBC (E) Working Group [ ] Catastrophe Risk (E) Subgroup [ ] Investment RBC (E) Working Group [ ] SMI RBC (E) Subgroup [ ] C3 Phase II/ AG43 (E/A) Subgroup [ ] P/C RBC (E) Working Group [ ] Stress Testing (E) Subgroup DATE: 08/31/2020 FOR NAIC USE ONLY CONTACT PERSON: Crystal Brown Agenda Item # 2020-07-H TELEPHONE: 816-783-8146 Year 2021 EMAIL ADDRESS: [email protected] DISPOSITION [ x ] ADOPTED WG 10/29/20 & TF 11/19/20 ON BEHALF OF: Health RBC (E) Working Group [ ] REJECTED NAME: Steve Drutz [ ] DEFERRED TO TITLE: Chief Financial Analyst/Chair [ ] REFERRED TO OTHER NAIC GROUP AFFILIATION: WA Office of Insurance Commissioner [ ] EXPOSED ________________ ADDRESS: 5000 Capitol Blvd SE [ ] OTHER (SPECIFY) Tumwater, WA 98501 IDENTIFICATION OF SOURCE AND FORM(S)/INSTRUCTIONS TO BE CHANGED [ x ] Health RBC Blanks [ x ] Health RBC Instructions [ ] Other ___________________ [ ] Life and Fraternal RBC Blanks [ ] Life and Fraternal RBC Instructions [ ] Property/Casualty RBC Blanks [ ] Property/Casualty RBC Instructions DESCRIPTION OF CHANGE(S) Split the Bonds and Misc. Fixed Income Assets into separate pages (Page XR007 and XR008). REASON OR JUSTIFICATION FOR CHANGE ** Currently the Bonds and Misc. Fixed Income Assets are included on page XR007 of the Health RBC formula. With the implementation of the 20 bond designations and the electronic only tables, the Bonds and Misc. Fixed Income Assets were split between two tabs in the excel file for use of the electronic only tables and ease of printing. However, for increased transparency and system requirements, it is suggested that these pages be split into separate page numbers beginning with year-2021. -
Structural and Intensity Changes of Concentric Eyewall Typhoons in the Western North Pacific Basin
2632 MONTHLY WEATHER REVIEW VOLUME 141 Structural and Intensity Changes of Concentric Eyewall Typhoons in the Western North Pacific Basin YI-TING YANG AND HUNG-CHI KUO Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan ERIC A. HENDRICKS AND MELINDA S. PENG Naval Research Laboratory, Monterey, California (Manuscript received 31 August 2012, in final form 7 February 2013) ABSTRACT An objective method is developed to identify concentric eyewalls (CEs) for typhoons using passive mi- crowave satellite imagery from 1997 to 2011 in the western North Pacific basin. Three CE types are identified: a CE with an eyewall replacement cycle (ERC; 37 cases), a CE with no replacement cycle (NRC; 17 cases), and a CE that is maintained for an extended period (CEM; 16 cases). The inner eyewall (outer eyewall) of the ERC (NRC) type dissipates within 20 h after CE formation. The CEM type has its CE structure maintained for more than 20 h (mean duration time is 31 h). Structural and intensity changes of CE typhoons are dem- onstrated using a T–Vmax diagram (where T is the brightness temperature and Vmax is the best-track es- timated intensity) for a time sequence of the intensity and convective activity (CA) relationship. While the intensity of typhoons in the ERC and CEM cases weakens after CE formation, the CA is maintained or increases. In contrast, the CA weakens in the NRC cases. The NRC (CEM) cases typically have fast (slow) northward translational speeds and encounter large (small) vertical shear and low (high) sea surface tem- 2 peratures. The CEM cases have a relatively high intensity (63 m s 1), and the moat size (61 km) and outer eyewall width (70 km) are approximately 50% larger than the other two categories. -
DISASTER RISK MAPPING and ASSESSMENT (GEORISK 2019) 25-27 February 2019 @ KBN, KUNDASANG, SABAH
WORKSHOP & FORUM ON GEOSPATIAL TECHNOLOGY FOR DISASTER RISK MAPPING AND ASSESSMENT (GEORISK 2019) 25-27 February 2019 @ KBN, KUNDASANG, SABAH THEME: ADVANCING SCIENCE AND TECHNOLOGY FOR DISASTER RISK REDUCTION Workshop & Forum on Geospatial DATE: Technology for Disaster Risk Mapping and 25- 27 FEBRUARY 2019 Assessment (GeoRisk2019) aims to provide an insight into modern and advanced geospatial technology fo r mapping, VENUE: analysing and assessing multi-geohazard KBN KUNDASANG,SABAH and disaster risk in a complex environment. Organized by Global and regional ca s e studies, covering Universiti Teknologi Malaysia (UTM) Kuala Lumpur several benchmarking and best practices will be interactively discussed. This co u rs e With the support of Department of Minerals and Geoscience Malaysia (JMG) addresses the importance of Department of Surveying and Mapping Malaysia (JUPEM) understanding georisk, strengthening risk Sabah Lands and Surveys Department (JTU) governance and elevating disaster Royal Institution of Surveyors Malaysia (RISM) preparedness. New, cutting-edge mapping Society for Engineering Geology and Rock Mechanics (SEGRM) technology (UAV, Terrestrial laser scanning, LiDAR, GNSS, Remote Sensing) coupling Disaster Prevention Research Institute, Kyoto University, Japan with BigData Analytics, early-warning Japan-ASEAN Science, Technology and Innovative Platform system, monitoring system and predictive Climate Change and Disaster Risk Reduction WG, modelling will be shared. Ad va n ced earth Global Young Academy (GYA) observation and geospatial data are highly International Council for Science (ISC)ROAP in demand fo r disaster mitigation, prevention, risk assessment and reduction strategies in a changing climate. GeoRisk2019 promotes an intelligent, integrated and transdisciplinary approach for reducing disaster risk, as in line with the Fee: RM800/person - 3 Days 2 nights Sendai Framework fo r Disaster Risk • Inclusive airport transfer (only limited pick-up time); accommodation @ KBN Ku nd a sa n g; daily Reduction 2015-2030 and national policies. -
Tropical Cyclones 2019
<< LINGLING TRACKS OF TROPICAL CYCLONES IN 2019 SEP (), !"#$%&'( ) KROSA AUG @QY HAGIBIS *+ FRANCISCO OCT FAXAI AUG SEP DANAS JUL ? MITAG LEKIMA OCT => AUG TAPAH SEP NARI JUL BUALOI SEPAT OCT JUN SEPAT(1903) JUN HALONG NOV Z[ NEOGURI OCT ab ,- de BAILU FENGSHEN FUNG-WONG AUG NOV NOV PEIPAH SEP Hong Kong => TAPAH (1917) SEP NARI(190 6 ) MUN JUL JUL Z[ NEOGURI (1920) FRANCISCO (1908) :; OCT AUG WIPHA KAJIK() 1914 LEKIMA() 1909 AUG SEP AUG WUTIP *+ MUN(1904) WIPHA(1907) FEB FAXAI(1915) JUL JUL DANAS(190 5 ) de SEP :; JUL KROSA (1910) FUNG-WONG (1927) ./ KAJIKI AUG @QY @c NOV PODUL SEP HAGIBIS() 1919 << ,- AUG > KALMAEGI OCT PHANFONE NOV LINGLING() 1913 BAILU()19 11 \]^ ./ ab SEP AUG DEC FENGSHEN (1925) MATMO PODUL() 191 2 PEIPAH (1916) OCT _` AUG NOV ? SEP HALONG (1923) NAKRI (1924) @c MITAG(1918) NOV NOV _` KALMAEGI (1926) SEP NAKRI KAMMURI NOV NOV DEC \]^ MATMO (1922) OCT BUALOI (1921) KAMMURI (1928) OCT NOV > PHANFONE (1929) DEC WUTIP( 1902) FEB 二零一 九 年 熱帶氣旋 TROPICAL CYCLONES IN 2019 2 二零二零年七月出版 Published July 2020 香港天文台編製 香港九龍彌敦道134A Prepared by: Hong Kong Observatory 134A Nathan Road Kowloon, Hong Kong © 版權所有。未經香港天文台台長同意,不得翻印本刊物任何部分內容。 © Copyright reserved. No part of this publication may be reproduced without the permission of the Director of the Hong Kong Observatory. 本刊物的編製和發表,目的是促進資 This publication is prepared and disseminated in the interest of promoting 料交流。香港特別行政區政府(包括其 the exchange of information. The 僱員及代理人)對於本刊物所載資料 Government of the Hong Kong Special 的準確性、完整性或效用,概不作出 Administrative Region