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Severe Tropical Cyclone Glenda 27 - 31 March 2006
Severe Tropical Cyclone Glenda 27 - 31 March 2006 Perth Tropical Cyclone Warning Centre Bureau of Meteorology A. Summary Severe Tropical Cyclone Glenda was a small and intense system that developed very rapidly after moving off the northwest Kimberley coast. Glenda reached category 5 intensity but weakened as it approached the Pilbara coast. Although threatening to cross the coast near the populated Dampier/Karratha region as a Category 4 system close to the time of high tide, Glenda took a more SW course towards Onslow and weakened before finally crossing the coast near Onslow at 2200 WST 30 March as a marginal category 3 system. Very destructive winds were recorded on the coast at Mardie prior to crossing. A total of 206 mm of rain fell at Onslow in the 24 hours to 0900 WST 31 March, representing the sixth wettest day on record for the town. Other centres in the Pilbara also recorded cumulative totals of over 200mm, and although in general Glenda produced less than average rainfall for a landfalling tropical cyclone, rainfall was sufficient to cause problems for transport. The weakening of TC Glenda prior to impact on Onslow, together with the preparedness of the town helped to avert major damage. B. Meteorological Description A weak low developed in the Gulf of Carpentaria during the middle of March and slowly progressed westwards over the Northern Territory. On 24 March it moved temporarily into the Joseph Bonaparte Gulf north of Wyndham, then accelerated across the Kimberley overnight. On 26 March vertical wind shear eased and by about 1200 UTC the system moved off the coast and developed rapidly. -
6. Annual Review and Significant Events
6. Annual Review and Significant Events January-April: wet in the tropics and WA, very hot in central to eastern Australia For northern Australia, the tropical wet season (October 2005 – April 2006) was the fifth wettest on record, with an average of 674 mm falling over the period. The monsoon trough was somewhat late in arriving over the Top End (mid-January as opposed to the average of late December), but once it had become established, widespread heavy rain featured for the next four months, except over the NT and Queensland in February. One particularly noteworthy event occurred towards the end of January when an intense low (central pressure near 990 hPa) on the monsoon trough, drifted slowly westward across the central NT generating large quantities of rain. A two-day deluge of 482 mm fell at Supplejack in the Tanami Desert (NT), resulting in major flooding over the Victoria River catchment. A large part of the central NT had its wettest January on record. Widespread areas of above average rain in WA were mainly due to the passages of several decaying tropical cyclones, and to a lesser extent southward incursions of tropical moisture interacting with mid-latitude systems. Severe tropical cyclone Clare crossed the Pilbara coast on 9t h January and then moved on a southerly track across the western fringes of WA as a rain depression. Significant flooding occurred around Lake Grace where 226 mm of rain fell in a 24-hour period from 12 t h to 13 t h January. Tropical cyclone Emma crossed the Pilbara coast on 28 th February and moved on a southerly track; very heavy rain fell in the headwaters of the Murchison River on 1s t March causing this river’s highest flood on record. -
Summary of 2005/6 Australian-Region Tropical Storm Season and Verification of Authors’ Seasonal Forecasts
Summary of 2005/6 Australian-Region Tropical Storm Season and Verification of Authors’ Seasonal Forecasts Issued: 15th May 2006 by Professor Mark Saunders and Dr Adam Lea Benfield Hazard Research Centre, UCL (University College London), UK. Summary ¢¡¤£¦¥¨§¨§¨© £¨¨ £¨£¨ ¨£"!$#%¨&('(¨)¨'*+%,¨-'(.¨&/%¨01¨.%'23'(%546¨7+£¨ ¤£¨ ¨£8!$#%¨&('(¨9&*¨¤7:¨&(&*'( ;¨.%'23'*%54=<3 ¢¡¤'*>.¨¤%¨%?@'(%¡9%¡£A:B¨#A-,£C3'(¨#/!$#%¨&('(¨ %,¨-¤'*.¨&%¨0D£¨¨E@¡'(.¡F¨&(&3¡¤¨7F)£&(,@£¨ ¨£"¨.%'23'(%54¨<G ¢¡£" ¢HIJ%£,.'(&(£K-,¨)¤¨)'(&*'(%54 :B¨,£.¨%¦:L¨M%¡¤£¥¨§¨§¨© N £¨¨O¡,@£7P£Q¨.£&*&(£%$R¤'*&(&(ST-,£7'(.%'( :,¨0VUW 4X¥¨§¨§¨©+%¡¨% !K#%¨&('*¨ )¨'( ¨7 &(¨7¤:¨&*&('( Y¨.%'Z3'(%54Y[¨#&(7 )£\.&*¨£\%Y£¨ ¨£<X ¢¡¤£] ¢H¤I 7¤£%£0^'*¤'*%'*.¦:B¨,£.¨%A¡,@£76 ¨¨¨76R¤'*&(&_:B¨;)¤¨'(`¨.%'23'(%54a¨76:B¨¦&*¨¤7:¨&(&*'( M%,¨-'(.¨& %¨0b¤#0^)£_:,¨0bUc 4d¥¨§¨§¨©¨< egf3hejilk m3n(opqsr=t k iu1vKn(wyxOze{r|vK}$ok ~3wk it nZ¨u1m¨ilhwh~¨tNw@pFwy¨u[upiOk¨st(f3h¨¨¨ ^"3wyt(ilpq(n*p~3 ilh,¨n(k ~;t*ilk m3n(opqwtNk iyuwhpwk ~9p~3¦p8gpq(n(¨pt n(k ~k¨t(f3hniwhpwk ~3pqm¨ilk 3p3n(q*n(wyt n(oAp~3¦¨ht hiunZ~3n(wyt n*o k ilhopwyt w>k i?t(f3n(w>potNn 3nZt*¨¤egf3hwh$k ilhopwyt w{@hilh$n*wwy3hKuk ~¨t(f3qZ95ilk ut*f3h$ t(f¦Wp9¨¨¨ "tNk"t*f3h t(f@hohu[3hi8¨¨¨ p~3nZ~3oqZ3¨hKwhm3pilptNhTm¨ilh¨n(otNn(k ~3wsk i{~¨¨u3hilwsk¨¤t*ilk m3n(opqwyt k iuw~¨¨u[3hilw k¨¢wh¤hilh t(ilk m3n(opq¡oC3oq(k ~3hw"p~3¢t(f3h A£E¤¥z5@oo¨u3q(ptNh^£E3oq*k ~3h¦¤¡~3hi 3}snZ~3¨h§3egf3h[q*pt(tNhiKn(w ¨n ¤h~dk i¨t*f3h/"f3k¨q(h/"3wyt(ilpq*n(p~35ilh ¨n(k ~3 Features of the 2005/6 Australian-Region Season • The 2005/6 Australian-region tropical storm season featured 11 storms of which 7 made severe tropical cyclone strength (U.S. -
Polarimetric Radar Observations of the Persistently Asymmetric Structure of Tropical Cyclone Ingrid
616 MONTHLY WEATHER REVIEW VOLUME 136 Polarimetric Radar Observations of the Persistently Asymmetric Structure of Tropical Cyclone Ingrid PETER T. MAY,J.D.KEPERT, AND T. D. KEENAN Bureau of Meteorology Research Centre, Melbourne, Australia (Manuscript received 3 November 2006, in final form 3 May 2007) ABSTRACT Tropical Cyclone Ingrid had a distinctly asymmetric reflectivity structure with an offshore maximum as it passed parallel to and over an extended coastline near a polarimetric weather radar located near Darwin, northern Australia. For the first time in a tropical cyclone, polarimetric weather radar microphysical analyses are used to identify extensive graupel and rain–hail mixtures in the eyewall. The overall micro- physical structure was similar to that seen in some other asymmetric storms that have been sampled by research aircraft. Both environmental shear and the land–sea interface contributed significantly to the asymmetry, but their relative contributions were not determined. The storm also underwent very rapid changes in tangential wind speed as it moved over a narrow region of open ocean between a peninsula and the Tiwi Islands. The time scale for changes of 10 m sϪ1 was of the order of 1 h. There were also two distinct types of rainbands observed—large-scale principal bands with embedded deep convection and small-scale bands located within 50 km of the eyewall with shallow convective cells. 1. Introduction larimetric radar (Keenan et al. 1998). Ingrid was a long- lived storm that reached Australian category 5 intensity The structure and intensity of tropical cyclones (TCs) twice—initially before it crossed the North Queensland around landfall are a major topic of research because of coast, and then again as it reintensified over the Gulf of the potential impact on human populations and prop- Carpentaria, where the eye structure was quite sym- erty. -
TROPICAL CYCLONE INFORMATION SERVICE Prepared by Coastal Services Unit, Environmental Sciences Division
TROPICAL CYCLONE INFORMATION SERVICE Prepared by Coastal Services Unit, Environmental Sciences Division Interim report on severe tropical cyclone Ingrid Issued April 2005. • Category 5 cyclone with wind gusts to 320 kilometres per hour near the centre. • Cyclone crossed the Queensland east coast as category 4, 57km south east of Lockhart River. • Estimated peak water level reached 4.0 metres above Australian height Datum (AHD) near Voaden Point (at the southern end of the Lockhart River Aboriginal Reserve). • Extensive environmental damage in vicinity of landfall location. • Cyclone recrossed Queensland west coast into Gulf of Carpentaria 70km south of Weipa. • Storm tide exceeded the Highest Astronomical Tide (HAT) at Cooktown by 0.28m. • National Disaster Relief Funding activated by Queensland Emergency Services Minister. Figure 1 –Track of severe tropical cyclone Ingrid (based on Tropical Cyclone Advices from Bureau of Meteorology). Summary Severe tropical cyclone Ingrid formed in the Coral Sea some time around 14:00 (AEST) on Sunday 6 March 2005 after drifting eastwards across Cape York along a monsoon trough line extending through northern Australia. The first Tropical Cyclone Advice was issued by the Bureau of Meteorology in Brisbane at 15:56 (AEST) on Monday 7 March, at which time Ingrid had deepened into a Category 3 cyclone (on a scale of 1 to 5). The timing of the cyclone corresponded to high spring tides, at or near the Highest Astronomical Tide (HAT), along the east coast of Cape York Peninsula, between Cairns and Thursday Island. Environmental Protection Agency (EPA) storm tide advisers reported to the Department of Emergency Services, State Disaster Coordination Centre at 13:00 (AEST) on Tuesday 8 March. -
Tropical Cyclone Risk and Impact Assessment Plan Final Feb2014.Pdf
© Commonwealth of Australia 2013 Published by the Great Barrier Reef Marine Park Authority Tropical Cyclone Risk and Impact Assessment Plan Second Edition ISSN 2200-2049 ISBN 978-1-922126-34-4 Second Edition (pdf) This work is copyright. Apart from any use as permitted under the Copyright Act 1968, no part may be reproduced by any process without the prior written permission of the Great Barrier Reef Marine Park Authority. Requests and enquiries concerning reproduction and rights should be addressed to: Director, Communications and Parliamentary 2-68 Flinders Street PO Box 1379 TOWNSVILLE QLD 4810 Australia Phone: (07) 4750 0700 Fax: (07) 4772 6093 [email protected] Comments and enquiries on this document are welcome and should be addressed to: Director, Ecosystem Conservation and Resilience [email protected] www.gbrmpa.gov.au ii Tropical Cyclone Risk and Impact Assessment Plan — GBRMPA Executive summary Waves generated by tropical cyclones can cause major physical damage to coral reef ecosystems. Tropical cyclones (cyclones) are natural meteorological events which cannot be prevented. However, the combination of their impacts and those of other stressors — such as poor water quality, crown-of-thorns starfish predation and warm ocean temperatures — can permanently damage reefs if recovery time is insufficient. In the short term, management response to a particular tropical cyclone may be warranted to promote recovery if critical resources are affected. Over the long term, using modelling and field surveys to assess the impacts of individual tropical cyclones as they occur will ensure that management of the Great Barrier Reef represents world best practice. This Tropical Cyclone Risk and Impact Assessment Plan was first developed by the Great Barrier Reef Marine Park Authority (GBRMPA) in April 2011 after tropical cyclone Yasi (one of the largest category 5 cyclones in Australia’s recorded history) crossed the Great Barrier Reef near Mission Beach in North Queensland. -
Use of the European Severe Weather Database to Verify Satellite-Based Storm Detection Or Nowcasting
USE OF THE EUROPEAN SEVERE WEATHER DATABASE TO VERIFY SATELLITE-BASED STORM DETECTION OR NOWCASTING Nikolai Dotzek1,2, Caroline Forster1 1 Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, 82234 Wessling, Germany 2 European Severe Storms Laboratory, Münchner Str. 20, 82234 Wessling, Germany Abstract Severe thunderstorms constitute a major weather hazard in Europe, with an estimated total damage of € 5-8 billion each year. Yet a pan-European database of severe weather reports in a homogeneous data format has become available only recently: the European Severe Weather Database (ESWD). We demonstrate the large potential of ESWD applications for storm detection and forecast or now- casting/warning verification purposes. The study of five warm-season severe weather days in Europe from 2007 and 2008 revealed that up to 47% of the ESWD reports were located exactly within the polygons detected by the Cb-TRAM algorithm for three different stages of deep moist convection. The cool-season case study of extratropical cyclone “Emma” on 1 March 2008 showed that low-topped winter thunderstorms can provide a challenge for satellite storm detection and nowcasting adapted to warm-season storms with high, cold cloud tops. However, this case also demonstrated how ESWD reports alone can still be valuable to identify the hazardous regions along the cold front of the cyclone. 1. INTRODUCTION Severe thunderstorms, with their attendant strong winds, hail, flooding, and tornadoes, are common phenomena in many European countries, leading to a total damage estimate of 5 to 8 billion euros per year (source: Munich Re Group). Extreme events like an F4 tornado in France and an F3 downburst in Austria in 2008 exemplify these damage totals. -
Identification of Climate Change Adaptation Best Practices in the Waste Management Sector ______
Identification of climate change adaptation Best Practices in the Waste Management Sector ___________________________________________ Disaster Waste Management Best practices FINAL REPORT – SEPTEMBER 4TH , 2013 IDENTIFICATION OF CLIMATE CHANGE ADAPTATION BEST PRACTICES IN THE WASTE MANAGEMENT SECTOR PART I REVISIONS VERSION DATE COMMENTS AUTHOR : CHECKED Final document incl. 2 02/09/2013 MLL ThM comments from client 1 19/08/2013 Final document MLL & JW ThM 0 09/08/2013 Draft document part I MLL & JW ThM This document is submitted by Pöyry France – Pöyry France becomes Naldeo Contact : Thierry Martin Manager International Department Naldeo France Phone + 33.4.91.13.97.56 Mobile + 33.6.82.56.92.94 55 rue de la Villette 69425 Lyon cedex 03 - France E-mail : [email protected] Page 2 NALDEO- PÖYRY 2013 IDENTIFICATION OF CLIMATE CHANGE ADAPTATION BEST PRACTICES IN THE WASTE MANAGEMENT SECTOR PART I CONTENTS PART I 1 IDENTIFICATION OF GEOGRAPHIC AREAS AFFECTED BY DESTRUCTIVE EVENTS LINKED TO CLIMATE CHANGE ................................................................................................................ 11 1.1 Effects of climat change .............................................................................................................. 11 1.1.1 Effects of climate change in the Pacific Region .....................................................................................................................11 1.1.2 Affected geographic areas ......................................................................................................................................................13 -
The Age Natural Disaster Posters
The Age Natural Disaster Posters Wild Weather Student Activities Wild Weather 1. Search for an image on the Internet showing damage caused by either cyclone Yasi or cyclone Tracy and insert it in your work. Using this image, complete the Thinking Routine: See—Think— Wonder using the table below. What do you see? What do you think about? What does it make you wonder? 2. World faces growing wild weather threat a. How many people have lost their lives from weather and climate-related events in the last 60 years? b. What is the NatCatService? c. What does the NatCatService show over the past 30 years? d. What is the IDMC? e. Create a line graph to show the number of people forced from their homes because of sudden, natural disasters. f. According to experts why are these disasters getting worse? g. As human impact on the environment grows, what effect will this have on the weather? h. Between 1991 and 2005 which regions of the world were most affected by natural disasters? i. Historically, what has been the worst of Australia’s natural disasters? 3. Go to http://en.wikipedia.org/wiki/File:Global_tropical_cyclone_tracks-edit2.jpg and copy the world map of tropical cyclones into your work. Use the PQE approach to describe the spatial distribution of world tropical cyclones. This is as follows: a. P – describe the general pattern shown on the map. b. Q – use appropriate examples and statistics to quantify the pattern. c. E – identifying any exceptions to the general pattern. 4. Some of the worst Question starts a. -
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. -
Extreme Weather Events in Europe: Preparing for Climate Change Adaptation
Extreme Weather Events in Europe: preparing for climate change adaptation October 2013 ISBN (print) 978-82-7144-100-5 ISBN (electronic) 978-82-7144-101-2 In cooperation with This report can be found at www.dnva.no Produced by the Norwegian Meteorological Institute Extreme Weather Events in Europe: preparing for climate change adaptation Øystein Hov, Ulrich Cubasch, Erich Fischer, Peter Höppe, Trond Iversen, Nils Gunnar Kvamstø, Zbigniew W. Kundzewicz, Daniela Rezacova, David Rios, Filipe Duarte Santos, Bruno Schädler, Ottó Veisz, Christos Zerefos, Rasmus Benestad, John Murlis, M. Donat, Gregor C. Leckebusch, Uwe Ulbrich. Extreme Weather Events in Europe: preparing for climate change adaptation In cooperation with CONTRIBUTORS Professor Øystein Hov, Norwegian Meteorological Institute, Norway† Professor Ulrich Cubasch, Free University of Berlin, Germany* Dr Erich Fischer, Institute for Atmospheric and Climatic Science, ETH Zurich, Switzerland* Professor Peter Höppe, Geo Risks Research/Corporate Climate Centre, Munich Re, Germany* Professor Trond Iversen, Norwegian Meteorological Institute, Norway* Professor Nils Gunnar Kvamstø, Department of Geophysics, University of Bergen, Norway* Professor Zbigniew W. Kundzewicz, Polish Academy of Sciences, Warsaw, Poland* Professor Daniela Rezacova, Institute of Atmospheric Physics, Academy of Sciences of the Czech Republic, Prague, Czech Republic* Professor David Rios, Royal Academy of Sciences, Spain* Professor Filipe Duarte Santos, Lisbon University, Portugal* Dr Bruno Schädler, University of Berne, Switzerland* Professor Ottó Veisz, Agricultural Research Institute of the Hungarian Academy of Sciences, Budapest, Hungary* Professor Christos Zerefos, University of Athens, Greece* Dr Rasmus Benestad (Working Group Researcher), Norwegian Meteorological Institute, Oslo, Norway Professor John Murlis, EASAC Environment Programme Secretary Dr M. Donat, Institut für Meteorologie, Freie Universität Berlin, Germany; now at Climate Change Research Centre, University of New South Wales, Sydney, Australia Dr Gregor C. -
Damage Investigation of Buildings at Minjilang, Cape Don and Smith Point in NT Following Cyclone Ingrid
CYCLONE TESTING STATION Damage investigation of buildings at Minjilang, Cape Don and Smith Point in NT following Cyclone Ingrid Report: TR50 September, 2005 Cyclone Testing Station School of Engineering James Cook University Queensland, 4811 Phone: 07 4 781 4340 Fax: 07 477 5 11 84 CYCLONE TESTING STATION SCHOOL of ENGINEERING JAMES COOK UNIVERSITY TECHNICAL REPORT NO. 50 Damage investigation of buildings at Minjilang, Cape Don and Smith Point in NT following Cyclone Ingrid By David Henderson and Cam Leitch September 2005 © James Cook Cyclone Testing Station Henderson, David, 1967 - . Damage investigation of buildings at Minjilang, Cape Don and Smith Point in NT following Cyclone Ingrid Bibliography. ISBN 0 86443 748 X ISSN 0158 - 8338 1. Cyclone Ingrid 2005 2. Buildings – Natural disaster effects. 3. Cyclones – Northern Territory - 2005 I. Leitch, Campbell, 1954 - . II. James Cook University. Cyclone Testing Station. III. Title. (Series : Technical Report (James Cook University. Cyclone Testing Station); no. 50). 624.1772 Contents 1. Summary .......................................................................................................................... 4 2. Acknowledgements .......................................................................................................... 4 3. Cyclone Ingrid.................................................................................................................. 5 4. Minjilang .........................................................................................................................