Hkmets BULLETIN, Volume 5, Number 1, 1995
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A Study of the Foehn Phenomenon Induced by Typhoon in Taiwan
A Study of the Foehn Phenomenon Induced by Typhoon in Taiwan Wen-Kuei Huang *, Yu-Ting Liou*, Ben Jong-Dao,Jou ** Fire Bureau Taitung, County, Taiwan* Department of Atmospheric Sciences, National Taiwan University** ABSTRACT: There’re 171 typhoons making landfall all over Taiwan during the period (1960~2009), the research is on the basis of all weather stations belonging to Central Weather Bureau (CWB) records, and it has been found that there’re 123 typhoons at least ever inducing Foehn wind event in one weather station in that area, the tract frequencies were around 71.9%. Among them, the total number of the class 2 tract is 24 for 19.5% of the total, the 1st, the total number of the class 5 tract is 22 for 17.9% of the total, the 2nd,the total number of the class 3 tract is 19 for 15.5% of the total, the 3rd. There’re 59 foehn phenomena induced by typhoon affecting Taiwan in the eastern Taiwan area, when the center of the class 1 typhoon tract was placed among the area ranged from 120。E to 124。E, 25。N to 28。N, would induce obvious foehn phenomena in Taitung, Dawu district in the eastern Taiwan. There’re 110 foehn phenomena induced by typhoon affecting Taiwan in the western Taiwan area. When the center of the class 5 typhoon tract was placed among the area ranged from 123。E to 126。E, 17。N to 20。N and 19。N to 22。N, 119。E to 123。E, would induce foehn phenomena in Taichung, Hsinchu, Taipei district in the western Taiwan area. -
Climatology, Variability, and Return Periods of Tropical Cyclone Strikes in the Northeastern and Central Pacific Ab Sins Nicholas S
Louisiana State University LSU Digital Commons LSU Master's Theses Graduate School March 2019 Climatology, Variability, and Return Periods of Tropical Cyclone Strikes in the Northeastern and Central Pacific aB sins Nicholas S. Grondin Louisiana State University, [email protected] Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_theses Part of the Climate Commons, Meteorology Commons, and the Physical and Environmental Geography Commons Recommended Citation Grondin, Nicholas S., "Climatology, Variability, and Return Periods of Tropical Cyclone Strikes in the Northeastern and Central Pacific asinB s" (2019). LSU Master's Theses. 4864. https://digitalcommons.lsu.edu/gradschool_theses/4864 This Thesis is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Master's Theses by an authorized graduate school editor of LSU Digital Commons. For more information, please contact [email protected]. CLIMATOLOGY, VARIABILITY, AND RETURN PERIODS OF TROPICAL CYCLONE STRIKES IN THE NORTHEASTERN AND CENTRAL PACIFIC BASINS A Thesis Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Master of Science in The Department of Geography and Anthropology by Nicholas S. Grondin B.S. Meteorology, University of South Alabama, 2016 May 2019 Dedication This thesis is dedicated to my family, especially mom, Mim and Pop, for their love and encouragement every step of the way. This thesis is dedicated to my friends and fraternity brothers, especially Dillon, Sarah, Clay, and Courtney, for their friendship and support. This thesis is dedicated to all of my teachers and college professors, especially Mrs. -
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. -
Tropical Cyclones in 1994
ROYAL OBSERVATORY HONG KONG TROPICAL CYCLONES IN 1994 CROWN COPYRIGHT RESERVED Published May 1995 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, express 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 1994 FIGURES 4 TABLES 5 HONG KONG'S TROPICAL CYCLONE WARNING SIGNALS 6 1. INTRODUCTION 7 2. TROPICAL CYCLONE OVERVIEW FOR 1994 11 3. REPORTS ON TROPICAL CYCLONES AFFECTING HONG KONG IN 1994 21 (a) Severe Tropical Storm Russ (9403) : 3 - 9 June 22 (b) Tropical Storm Sharon (9404) : 23 - 25 June 26 (c) Severe Tropical Storm Harry (9418) : 25 - 29 August 31 (d) Tropical Storm Luke, (9423) : 7 - 14 September 35 4. TROPICAL CYCLONE STATISTICS AND TABLES 39 5. TROPICAL CYCLONE POSITION AND INTENSITY DATA, 1994 55 4 FIGURES Page 1. -
Extension of the Systematic Approach to Tropical Cyclone Track Forecasting in the Eastern and Central North Pacific
NPS ARCHIVE 1997.12 BOOTHE, M. NAVAL POSTGRADUATE SCHOOL Monterey, California THESIS EXTENSION OF THE SYTEMATIC APPROACH TO TROPICAL CYCLONE TRACK FORECASTING IN THE EASTERN AND CENTRAL NORTH PACIFIC by Mark A. Boothe December, 1997 Thesis Co-Advisors: Russell L.Elsberry Lester E. Carr III Thesis B71245 Approved for public release; distribution is unlimited. DUDLEY KNOX LIBRARY NAVAl OSTGRADUATE SCHOOL MONTEREY CA 93943-5101 REPORT DOCUMENTATION PAGE Form Approved OMB No. 0704-0188 Public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instruction, searching casting data sources, gathering and maintaining the data needed, and completing and reviewing the collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden, to Washington Headquarters Services, Directorate for Information Operations and Reports, 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302, and to the Office of Management and Budget, I'aperwork Reduction Project (0704-0188) Washington DC 20503. 1 . AGENCY USE ONLY (Leave blank) 2. REPORT DATE 3. REPORT TYPE AND DATES COVERED December 1997. Master's Thesis TITLE AND SUBTITLE EXTENSION OF THE SYSTEMATIC 5. FUNDING NUMBERS APPROACH TO TROPICAL CYCLONE TRACK FORECASTING IN THE EASTERN AND CENTRAL NORTH PACIFIC 6. AUTHOR(S) Mark A. Boothe 7. PERFORMING ORGANIZATION NAME(S) AND ADDR£SS(ES) PERFORMING Naval Postgraduate School ORGANIZATION Monterey CA 93943-5000 REPORT NUMBER 9. SPONSORING/MONITORING AGENCY NAME(S) AND ADDRESSEES) 10. SPONSORING/MONTTORIN G AGENCY REPORT NUMBER 11. SUPPLEMENTARY NOTES The views expressed in this thesis are those of the author and do not reflect the official policy or position of the Department of Defense or the U.S. -
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. -
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. -
Notable Tropical Cyclones and Unusual Areas of Tropical Cyclone Formation
A flood is an overflow of an expanse of water that submerges land.[1] The EU Floods directive defines a flood as a temporary covering by water of land not normally covered by water.[2] In the sense of "flowing water", the word may also be applied to the inflow of the tide. Flooding may result from the volume of water within a body of water, such as a river or lake, which overflows or breaks levees, with the result that some of the water escapes its usual boundaries.[3] While the size of a lake or other body of water will vary with seasonal changes in precipitation and snow melt, it is not a significant flood unless such escapes of water endanger land areas used by man like a village, city or other inhabited area. Floods can also occur in rivers, when flow exceeds the capacity of the river channel, particularly at bends or meanders. Floods often cause damage to homes and businesses if they are placed in natural flood plains of rivers. While flood damage can be virtually eliminated by moving away from rivers and other bodies of water, since time out of mind, people have lived and worked by the water to seek sustenance and capitalize on the gains of cheap and easy travel and commerce by being near water. That humans continue to inhabit areas threatened by flood damage is evidence that the perceived value of living near the water exceeds the cost of repeated periodic flooding. The word "flood" comes from the Old English flod, a word common to Germanic languages (compare German Flut, Dutch vloed from the same root as is seen in flow, float; also compare with Latin fluctus, flumen). -
Packery Channel Restoration Still on Hold
Inside the Moon Sandcastle Run A2 Biz Briefs A3 Stuff I Heard A5 Fishing A11 Issue 894 The 27° 37' 0.5952'' N | 97° 13' 21.4068'' W Island Free The voiceMoon of The Island since 1996 June 3, 2021 Weekly www.islandmoon.com FREE Photo by Evelyn Pless-Schuberth Around The Island Memorial Day From the Air Return By Dale Rankin The consensus among long-time of the Islanders seems to be that we have never seen as many people on our beaches as we saw last weekend. When the weather broke the crowds Litter turned out in a hurry and the driving conditions on the beach south of Beach Access Road 6 meant that very few beachgoers to could make their Critter! View Sunday looking north toward Newport Pass way down there. For a while Sunday View from Newport Pass looking south, Packery The return of the long-gone Litter afternoon the beach there looked from Packery Channel. Channel Jetties are at the top of the photo. Critter is at hand! like a used car lot as a long line of vehicles were stuck in the soft sand. The inability of drivers to use that part of the beach pushed everyone north packing the beaches there. There have been ongoing discussions for years about removing vehicles from the beach along the Michael J. Ellis Seawall but last weekend there would have been nowhere to park them except on Windward. There The City of Corpus Christi is renewed talk at city hall about announced Wednesday that The the need for a beach renourishment Critter will arrive on Padre Island on project to widen the beach but the Saturday, June 5 and to Flour Bluff problem is that the consultants hired July 10. -
Port Aransas
Inside the Moon Fun in the Sun A2 Canal Clean-up A4 Traveling Moon A9 Art Fest A16 Live Music A18 Issue 737 The Photo by Steve Coons Island Free The voiceMoon of The Island since 1996 May 31, 2018 Weekly www.islandmoon.com FREE Around The 8000 Kemp’s Ridley Turtles Predictions Island for Hurricane By Dale Rankin Season 2018 So far it’s been a bit of a strange in One Day! season here on our little sandbar Active season much with two of the four major tourist invasions behind us but the High Active season much like 2017 like 2017 100 Day Season is only a week old. By Dale Rankin Spring Break 2018 repeated the pattern of spring breaks past with full As the Coastal Bend continues to beaches and roads jammed from the dig out after Hurricane Harvey we ferry landings in Port A to Flour Bluff plow right into Hurricane Season Drive. 2018 with predictions from three of the most-followed predictors calling Memorial Day saw packed beaches for an average to above-average and some traffic backups, to Flour season. An average hurricane season Bluff Drive on Saturday and Sunday. produces 12 named storms, of which But a drive up State Highway 361 six become hurricanes, including early Sunday afternoon found very three major hurricanes. light traffic up the Landing Strip between Padre and Port A and light The National Oceanic and traffic on the streets in Port Aransas. Atmospheric Organization’s (NOAA) hurricane forecast was But there was something different released this week predicting 10- about this year’s Memorial Day and 16 named storms between June 1 it’s a pattern we’ve seen for a couple of and November 30, 2018 with five of years, maybe exacerbated by the lack those reaching hurricane-force winds of hotel space in both Port Aransas of 75 mph or higher, and one to four and on Padre Island. -
MASARYK UNIVERSITY BRNO Diploma Thesis
MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION DEPARTMENT OF ENGLISH LANGUAGE AND LITERATURE Presentation Sentences in Wikipedia: FSP Analysis Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský Declaration I declare that I have worked on this thesis independently, using only the primary and secondary sources listed in the bibliography. I agree with the placing of this thesis in the library of the Faculty of Education at the Masaryk University and with the access for academic purposes. Brno, 30th March 2018 …………………………………………. Bc. Lukáš Opavský Acknowledgements I would like to thank my supervisor, doc. Mgr. Martin Adam, Ph.D. for his kind help and constant guidance throughout my work. Bc. Lukáš Opavský OPAVSKÝ, Lukáš. Presentation Sentences in Wikipedia: FSP Analysis; Diploma Thesis. Brno: Masaryk University, Faculty of Education, English Language and Literature Department, 2018. XX p. Supervisor: doc. Mgr. Martin Adam, Ph.D. Annotation The purpose of this thesis is an analysis of a corpus comprising of opening sentences of articles collected from the online encyclopaedia Wikipedia. Four different quality categories from Wikipedia were chosen, from the total amount of eight, to ensure gathering of a representative sample, for each category there are fifty sentences, the total amount of the sentences altogether is, therefore, two hundred. The sentences will be analysed according to the Firabsian theory of functional sentence perspective in order to discriminate differences both between the quality categories and also within the categories. -
On Tropical Cyclones
Frequently Asked Questions on Tropical Cyclones Frequently Asked Questions on Tropical Cyclones 1. What is a tropical cyclone? A tropical cyclone (TC) is a rotational low-pressure system in tropics when the central pressure falls by 5 to 6 hPa from the surrounding and maximum sustained wind speed reaches 34 knots (about 62 kmph). It is a vast violent whirl of 150 to 800 km, spiraling around a centre and progressing along the surface of the sea at a rate of 300 to 500 km a day. The word cyclone has been derived from Greek word ‘cyclos’ which means ‘coiling of a snake’. The word cyclone was coined by Heary Piddington who worked as a Rapporteur in Kolkata during British rule. The terms "hurricane" and "typhoon" are region specific names for a strong "tropical cyclone". Tropical cyclones are called “Hurricanes” over the Atlantic Ocean and “Typhoons” over the Pacific Ocean. 2. Why do ‘tropical cyclones' winds rotate counter-clockwise (clockwise) in the Northern (Southern) Hemisphere? The reason is that the earth's rotation sets up an apparent force (called the Coriolis force) that pulls the winds to the right in the Northern Hemisphere (and to the left in the Southern Hemisphere). So, when a low pressure starts to form over north of the equator, the surface winds will flow inward trying to fill in the low and will be deflected to the right and a counter-clockwise rotation will be initiated. The opposite (a deflection to the left and a clockwise rotation) will occur south of the equator. This Coriolis force is too tiny to effect rotation in, for example, water that is going down the drains of sinks and toilets.