Hawser Failure and Manoeuvring Difficulties on Board Dampier Spirit
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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. -
Characterizing the Hydrodynamics of Jurien Bay, Western Australia
Characterizing the Hydrodynamics of Jurien Bay, Western Australia Kellie Holloway June 2006 Professor Charitha Pattiaratchi ------------------------------------------------------------------------------------- This dissertation is submitted in partial fulfillment of the requirements for the Bachelor of Engineering (Applied Ocean Science) ------------------------------------------------------------------------------------- Abstract Abstract Jurien Bay is a small town on the Central West Coast of Western Australia. With an expanding economy based on fishing, aquaculture and tourism and proximity to Perth, Jurien Bay is expected to grow rapidly over the coming years. Increasing anthropogenic pressure has the potential to compromise the currently pristine natural environment. The livelihood of the town and the economy relies on the quality of the marine environment in particular; hence it is important to understand the dynamics of the system. This study investigates the characteristics of circulation in Essex Lagoon, a deep basin to the south of the main Jurien Bay settlement. This area is a particularly important for investigation due to the future impact of the adjacent Ardross Estates development and the aquaculture zone located within Essex Lagoon. An Acoustic Doppler Current Profiler (ADCP) was deployed in summer 2006 to obtain profiles of current velocity and magnitude over three weeks in Essex Lagoon. This data complemented similar data collected during winter 2002 in Essex Lagoon and was used to carry out a seasonal comparison of currents, to characterize circulation patterns and to examine the potential for outside forcing such as atmospheric pressure systems and the Leeuwin Current to influence circulation. A distinct seasonality was found in the circulation characteristics between summer and winter and this was primarily influenced by seasonality in the wind field. -
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 -
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. -
Title Author(S)
th 5 European Conference on Severe Storms 12 - 16 October 2009 - Landshut - GERMANY ECSS 2009 Abstracts by session ECSS 2009 - 5th European Conference on Severe Storms 12-16 October 2009 - Landshut – GERMANY List of the abstract accepted for presentation at the conference: O – Oral presentation P – Poster presentation Session 09: Severe storm case studies and field campaigns, e.g. COPS, THORPEX, VORTEX2 Page Type Abstract Title Author(s) An F3 downburst in Austria - a case study with special G. Pistotnik, A. M. Holzer, R. 265 O focus on the importance of real-time site surveys Kaltenböck, S. Tschannett J. Bech, N. Pineda, M. Aran, J. An observational analysis of a tornadic severe weather 267 O Amaro, M. Gayà, J. Arús, J. event Montanyà, O. van der Velde Case study: Extensive wind damage across Slovenia on July M. Korosec, J. Cedilnik 269 O 13th, 2008 Observed transition from an elevated mesoscale convective J. Marsham, S. Trier, T. 271 O system to a surface based squall line: 13th June, Weckwerth, J. Wilson, A. Blyth IHOP_2002 08/08/08: classification and simulation challenge of the A. Pucillo, A. Manzato 273 O FVG olympic storm H. Bluestein, D. Burgess, D. VORTEX2: The Second Verification of the Origins of Dowell, P. Markowski, E. 275 O Rotation in Tornadoes Experiment Rasmussen, Y. Richardson, L. Wicker, J. Wurman Observations of the initiation and development of severe A. Blyth, K. Browning, J. O convective storms during CSIP Marsham, P. Clark, L. Bennett The development of tornadic storms near a surface warm P. Groenemeijer, U. Corsmeier, 277 O front in central England during the Convective Storm C. -
Bungaroo Creek Water Reserve
Government of Western Australia Department of Water Bungaroo Creek Water Reserve Drinking water source protection plan West Pilbara water supply scheme Looking after all our water needs Water resource protection series Report WRP 135 November 2012 Bungaroo Creek Water Reserve drinking water source protection plan West Pilbara Water Supply Scheme Looking after all our water needs Department of Water Water resource protection series Report WRP 135 November 2012 Department of Water 168 St Georges Terrace Perth Western Australia 6000 Telephone +61 8 6364 7600 Facsimile +61 8 6364 7601 National relay service 13 36 77 www.water.wa.gov.au © Government of Western Australia November 2012 This work is copyright. You may download, display, print and reproduce this material in unaltered form only (retaining this notice) for your personal, non-commercial use or use within your organisation. Apart from any use as permitted under the Copyright Act 1968, all other rights are reserved. Requests and inquiries concerning reproduction and rights should be addressed to the Department of Water. ISBN 978-1-922124-47-0 (online) Acknowledgements The Department of Water would like to thank the following people for their contribution to this publication: the agency’s Clint Roberts, Natalie Leach, Chris Qiu, Stephen Watson and Nigel Mantle, Water Corporation’s Hew Merrett, Rio Tinto Iron Ore’s Ian Bell, Paul Collie, Natti Hundi and Leisa Turner, and the Traditional Owners of the land, the Kuruma Marthudunera People. For more information about this report, contact Water Source Protection Planning on +61 8 6364 7600 or [email protected]. Disclaimer This document has been published by the Department of Water. -
Legislative Council
Legislative Council Wednesday, 12 April 2006 THE PRESIDENT (Hon Nick Griffiths) took the chair at 2.00 pm, and read prayers. PAPERS TABLED Papers were tabled and ordered to lie upon the table of the house. WESTERN AUSTRALIAN GOVERNMENT’S COMMITMENT TO TRAINING Motion Resumed from 5 April on the following motion moved by Hon Graham Giffard - That this house congratulates the Western Australian government for its commitment to training and condemns the Australian government for its failure to address skills shortages. HON PETER COLLIER (North Metropolitan) [2.04 pm]: I will continue my comments on the federal government’s initiatives on training. As I said at the outset, the opposition will oppose the motion. It is a shame that we will oppose it because, as I said last week, we are very supportive of reforms and initiatives for the training sector in particular. We believe that this motion is a cheap shot on the part of the government to deal with something that is essentially a very serious matter. I have recognised the state government’s education and training initiatives, which I have stated on several occasions. The part of the motion to condemn the federal government is without merit, and that is why we cannot support the motion. I will continue my comments regarding the initiatives of the federal government. Last week I referred to the Commonwealth-State Agreement for Skilling Australia’s Workforce. This includes the provision of 20 000 additional places for new apprenticeship commencements and 26 000 additional training places for mature age people. That is a tremendous federal government initiative. -
Rainfall Distribution of Five Landfalling Tropical Cyclones in the Northwestern Australian Region
Australian Meteorological and Oceanographic Journal 63 (2013) 325–338 Rainfall distribution of five landfalling tropical cyclones in the northwestern Australian region Yubin Li1, Kevin K.W. Cheung1, Johnny C.L. Chan2, and Masami Tokuno3 1Department of Environment and Geography, Macquarie University, Sydney, Australia 2Guy Carpenter Asia-Pacific Climate Impact Centre, School of Energy and Environment, City University of Hong Kong, Hong Kong 3Meteorological Research Institute/Japan Meteorological Agency, Tsukuba, Ibaraki, Japan (Manuscript received July 2012; revised December 2012) Rain gauge data, satellite IR brightness temperature and radar-estimated rain rate for five tropical cyclones from the 2005–06 to 2009–10 seasons that made landfall along the northwestern coast of Australia are analysed. It is the first time that the spatial rainfall distribution of landfalling tropical cyclones in the southern hemi- sphere has been systematically investigated. It is found that the distributions of rainfall are more concentrated in the right side of the track of the landfall tropical cyclones, which is the offshore flow position. Potential mechanisms responsible for this observed asymmetry in rainfall distribution are discussed. These include the tropical cyclone motion direction, deep-tropospheric vertical wind shear and land-sea contrast in surface properties. Topography is considered to have less ef- fect since Western Australia is relatively flat. The rainfall maxima are found in the front and downshear quadrants for these tropical cyclones, which is consistent with previous studies. The changes in vertical wind shear when these tropical cy- clones moved to the south are largely attributed to the prevailing environmental flow. Three numerical simulations are performed; one with a realistic land surface, one with all topography removed and one with all land removed. -
Alpine Forest Drought Monitoring in South Tyrol: PCA Based Synergy Between Scpdsi Data and MODIS Derived NDVI and NDII7 Time Series
remote sensing Article Alpine Forest Drought Monitoring in South Tyrol: PCA Based Synergy between scPDSI Data and MODIS Derived NDVI and NDII7 Time Series Katarzyna Ewa Lewi ´nska 1,2, Eva Ivits 3, Mathias Schardt 1,* and Marc Zebisch 2 1 Institute of Remote Sensing and Photogrammetry, Graz Technical University, Steyrergasse 30/I, Graz 8010, Austria; [email protected] 2 Institute for Applied Remote Sensing, European Academy of Bozen/Bolzano (EURAC), Viale Druso 1, Bolzano 39100, Italy; [email protected] 3 European Environment Agency (EEA), Kongens Nytorv 6, Copenhagen K 1050, Denmark; [email protected] * Correspondence: [email protected]; Tel.: +43-316-873-6330 or +43-316-876-1754 Academic Editors: Angela Lausch, Marco Heurich, Lars T. Waser and Prasad S. Thenkabail Received: 26 April 2016; Accepted: 27 July 2016; Published: 5 August 2016 Abstract: Observed alternation of global and local meteorological patterns governs increasing drought impact, which puts at risk ecological balance and biodiversity of the alpine forest. Despite considerable attention, drought impact on forest ecosystems is still not entirely understood, and comprehensive forest drought monitoring has not been implemented. In this study, we proposed to bridge this gap exploiting a time-domain synergetic use of medium resolution MODSI NDVI (Normalized Difference Vegetation Index) and NDII7 (Normalized Difference Infrared Index band 7) time series as well as on-station temperature and precipitation measures combined in the scPDSI (self-calibrated Palmer Drought Severity Index) datasets. Analysis employed the S-mode Principal Component Analysis (PCA) examined under multiple method settings and data setups. The investigation performed for South Tyrol (2001–2012) indicated prolonged meteorological drought condition between 2003 and 2007, as well as general drying tendencies.