Kakadu National Park Landscape Symposium 4: Climate Change
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New Emission Factors for Australian Vegetation Fires Measured Using
Atmos. Chem. Phys., 14, 11335–11352, 2014 www.atmos-chem-phys.net/14/11335/2014/ doi:10.5194/acp-14-11335-2014 © Author(s) 2014. CC Attribution 3.0 License. New emission factors for Australian vegetation fires measured using open-path Fourier transform infrared spectroscopy – Part 2: Australian tropical savanna fires T. E. L. Smith1, C. Paton-Walsh2, C. P. Meyer3, G. D. Cook4, S. W. Maier5, J. Russell-Smith5, M. J. Wooster1, and C. P. Yates5 1King’s College London, Earth and Environmental Dynamics Research Group, Department of Geography, London, UK 2Centre for Atmospheric Chemistry, School of Chemistry, University of Wollongong, Wollongong, New South Wales, Australia 3CSIRO Marine and Atmospheric Sciences, PMB 1, Aspendale, Victoria, Australia 4CSIRO Ecosystem Sciences Sustainable Agriculture Flagship, PMB 44, Winnellie, Northern Territory, Australia 5Charles Darwin University, Research Institute for the Environment and Livelihoods, Darwin, Northern Territory, Australia Correspondence to: T. E. L. Smith ([email protected]) Received: 30 December 2013 – Published in Atmos. Chem. Phys. Discuss.: 11 March 2014 Revised: 16 September 2014 – Accepted: 17 September 2014 – Published: 29 October 2014 Abstract. Savanna fires contribute approximately 40–50 % stantially between different savanna vegetation assemblages; of total global annual biomass burning carbon emissions. Re- with a majority of this variation being mirrored by variations cent comparisons of emission factors from different savanna in the modified combustion efficiency (MCE) of different regions have highlighted the need for a regional approach to vegetation classes. We conclude that a significant majority emission factor development, and better assessment of the of the variation in the emission factor for trace gases can be drivers of the temporal and spatial variation in emission fac- explained by MCE, irrespective of vegetation class, as illus- tors. -
Known Impacts of Tropical Cyclones, East Coast, 1858 – 2008 by Mr Jeff Callaghan Retired Senior Severe Weather Forecaster, Bureau of Meteorology, Brisbane
ARCHIVE: Known Impacts of Tropical Cyclones, East Coast, 1858 – 2008 By Mr Jeff Callaghan Retired Senior Severe Weather Forecaster, Bureau of Meteorology, Brisbane The date of the cyclone refers to the day of landfall or the day of the major impact if it is not a cyclone making landfall from the Coral Sea. The first number after the date is the Southern Oscillation Index (SOI) for that month followed by the three month running mean of the SOI centred on that month. This is followed by information on the equatorial eastern Pacific sea surface temperatures where: W means a warm episode i.e. sea surface temperature (SST) was above normal; C means a cool episode and Av means average SST Date Impact January 1858 From the Sydney Morning Herald 26/2/1866: an article featuring a cruise inside the Barrier Reef describes an expedition’s stay at Green Island near Cairns. “The wind throughout our stay was principally from the south-east, but in January we had two or three hard blows from the N to NW with rain; one gale uprooted some of the trees and wrung the heads off others. The sea also rose one night very high, nearly covering the island, leaving but a small spot of about twenty feet square free of water.” Middle to late Feb A tropical cyclone (TC) brought damaging winds and seas to region between Rockhampton and 1863 Hervey Bay. Houses unroofed in several centres with many trees blown down. Ketch driven onto rocks near Rockhampton. Severe erosion along shores of Hervey Bay with 10 metres lost to sea along a 32 km stretch of the coast. -
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. -
Fishing the Tiwi Islands Welcome to Our Islands
FISHING THE TIWI ISLANDS WELCOME TO OUR ISLANDS The Tiwi Islands are made up of Melville and Bathurst Islands and numerous smaller, adjacent islands. The Vernon Islands also form part of the Tiwi estate. The Tiwi Traditional Owners and custodians of the area welcome you to our islands and ask that you respect and recognise the cultural importance of our land and waters. CODE OF Conduct RESPect THE RIGHts OF TRADITIONAL OWNERS. • Understand and observe all fishing regulations and no fishing zones. Report illegal fishing activities to the FISHWATCH hotline 1800 891 136 or the Tiwi Land Council HQ at Pickataramoor - 08 8970 9373. • Take no more fish than your immediate needs and carefully return excess or unwanted fish into the water unharmed. • Be courteous to all water users and those who belong to local Tiwi communities. • Respect Tiwi cultural ceremonies. This may mean that a particular area is temporarily closed to access. • Do not land ashore without first obtaining a separate Aboriginal land permit, from the Tiwi Land Council and abide by alcohol restrictions for the area. • Respect sacred sites and do not enter any part of the waters containing identified sacred sites unless specifically permitted to do so by the Tiwi Land Council. • Do not clean or dispose of fish within the vicinity of a community. • Prevent pollution and protect wildlife by removing rubbish and dispose of correctly to avoid potentially entrapping birds and other aquatic creatures. TIWI AND VERNON ISLANDS zones PERMIT FREE access The Tiwi have agreed to provide permit free access to the intertidal waters of the Tiwi and the Vernon Islands in the areas as outlined in the attached map. -
In the Aftermath of Cyclone Yasi: AIR Damage Survey Observations
AIRCURRENTS By IN THE AFTERMATH OF CYCLONE YaSI: AIR DAMAGE SURVEY OBSERVATIONS EDITOR’S NOTE: In the days following Yasi’s landfall, AIR’s post-disaster survey team visited areas in Queensland affected by the storm. This article 03.2011 presents their findings. By Dr. Kyle Butler and Dr. Vineet Jain Edited by Virginia Foley INTRODUCTION Severe Cyclone Yasi began as a westward-moving depression In addition to the intense winds, Yasi brought 200-300 off Fiji that rapidly developed into a tropical storm before millimeters of precipitation in a 24 hour period and a storm dawn on January 30, 2011. Hours later, Yasi blew across the surge as high as five meters near Mission Beach. northern islands of Vanuatu, continuing to grow in intensity and size and prompting the evacuation of more than 30,000 residents in Queensland, Australia. By February 2 (local time), the storm had achieved Category 5 status on the Australian cyclone scale (a strong Category 4 on the Saffir-Simpson scale). At its greatest extent, the storm spanned 650 kilometers. By the next day, it became clear that Yasi would spare central Queensland, which had been devastated by heavy flooding in December. But there was little else in the way of good news. Yasi made landfall on the northeast coast of Queensland on February 3 between Innisfail and Cardwell with recorded gusts of 185 km/h. Satellite-derived sustained Figure 1. Satellite-derived 10-minute sustained wind speeds in knots just after wind speeds of 200 km/h were estimated near the center Cyclone Yasi made landfall. -
Cyclone Tracey-Key Findings.Pdf
Historical case studies of extreme events Key findings: Cyclone Tracy 22/12-15:30 The event Cyclone Tracy was a Category 4 cyclone 22/12-21:00 that laid waste to the city of Darwin in the Northern Territory early on Christmas morning 1974. 23/12- 01:30 Cyclone Tracy showed the nation just how 23/12- 09:00 devastating the impact of a cyclone could be, and awoke the engineering community, local and international, to the true risk of cyclonic wind storms. Tracy’s small size minimised the spatial 23/12- 21:00 extent of damage, but her slow forward speed meant the areas beneath her storm track were completely devastated. 24/12- 09:00 Cyclone Tracy resulted in 71 deaths and 650 injuries. Fortunately for Darwin, flooding and 24/12- 13:00 storm surge were not major issues or these 24/12- 18:30 numbers could have been far higher. 24/12- 21:00 In almost all cases wind was the dominant 25/12- 00:30 factor in the ensuing structural damage, 25/12- 03:00 which left 94% of housing uninhabitable, Darwin approximately 40,000 people homeless and 25/12- 09:00 necessitated the evacuation of 80% of the 25/12- 12:00 city’s residents. Path of Cyclone Tracy. Image: Matthew Mason Scale of the disaster Cyclone Tracy is one of the most prominent the region since European settlement. The damaging and costly natural disasters in Australia’s history. Very impacts of Cyclone Tracy were the result of a ‘direct hit’ rarely does a disaster impact an entire major city, as on Darwin. -
Fixing the Hole in Australia's Heartland
Fixing the hole in Australia’s Heartland: How Government needs to work in remote Australia September 2012 Dr Bruce W Walker Dr Douglas J Porter Professor Ian Marsh The remoteFOCUS project is an initiative facilitated by Desert Knowledge Australia. Support to make this report possible has been provided by: Citation: Walker BW, Porter DJ, and Marsh I. 2012 Fixing the Hole in Australia’s Heartland: How Government needs to work in remote Australia, Desert Knowledge Australia, Alice Springs ISBN: 978-0-9873958-2-5 This report has been authored by: ISBN Online: 978-0-9873958-3-2 Dr Bruce W Walker, remoteFOCUS Project Director Dr Douglas J Porter, Governance Adviser, World Bank, Associated Reports: & Adjunct Professor, International Politics and Security Walker, BW, Edmunds, M and Marsh, I. 2012 Loyalty for Studies, Australian National University Regions: Governance Reform in the Pilbara, report to the Pilbara Development Commission, Desert Knowledge Australia Professor Ian Marsh, Adjunct Professor, Australian ISBN: 978-0-9873958-0-1 Innovation Research Centre, University of Tasmania Walker, BW, (Ed) Edmunds, M and Marsh, I. 2012 The With contributions by: remoteFOCUS Compendium: The Challenge, Conversation, Dr Mary Edmunds Commissioned Papers and Regional Studies of Remote Australia, Mr Simon Balderstone AM Desert Knowledge Australia. ISBN: 978-0-9873958-1-8 And review by the remoteFOCUS Reference Group: Copyright: Desert Knowledge Australia 2012 Hon Fred Chaney AO (Convenor) Licensed under the Creative Commons Dr Peter Shergold AC Attribution-Noncommercial-ShareAlike Licence Mr Neil Westbury PSM For additional information please contact: Mr Bill Gray AM Dr Bruce Walker Mr John Huigen (CEO Desert Knowledge Australia) Project Director | remoteFOCUS M: 0418 812 119 P: 08 8959 6125 The views expressed here are those of the individuals E: [email protected] and the remoteFOCUS team and should not be taken as W: www.desertknowledge.com.au/Our-Programs/remoteFOCUS representing the views of their employers. -
KUNINJKU PEOPLE, BUFFALO, and CONSERVATION in ARNHEM LAND: ‘IT’S a CONTRADICTION THAT FRUSTRATES US’ Jon Altman
3 KUNINJKU PEOPLE, BUFFALO, AND CONSERVATION IN ARNHEM LAND: ‘IT’S A CONTRADICTION THAT FRUSTRATES US’ Jon Altman On Tuesday 20 May 2014 I was escorting two philanthropists to rock art galleries at Dukaladjarranj on the edge of the Arnhem Land escarpment. I was there in a corporate capacity, as a direc- tor of the Karrkad-Kanjdji Trust, seeking to raise funds to assist the Djelk and Warddeken Indigenous Protected Areas (IPAs) in their work tackling the conservation challenges of maintain- ing the environmental and cultural values of 20,000 square kilometres of western Arnhem Land. We were flying low in a Robinson R44 helicopter over the Tomkinson River flood plains – Bulkay – wetlands renowned for their biodiversity. The experienced pilot, nicknamed ‘Batman’, flew very low, pointing out to my guests herds of wild buffalo and their highly visible criss-cross tracks etched in the landscape. He remarked over the intercom: ‘This is supposed to be an IPA but those feral buffalo are trashing this country, they should be eliminated, shot out like up at Warddeken’. His remarks were hardly helpful to me, but he had a point that I could not easily challenge mid-air; buffalo damage in an iconic wetland within an IPA looked bad. Later I tried to explain to the guests in a quieter setting that this was precisely why the Djelk Rangers needed the extra philanthropic support that the Karrkad-Kanjdji Trust was seeking to raise. * * * 3093 Unstable Relations.indd 54 5/10/2016 5:40 PM Kuninjku People, Buffalo, and Conservation in Arnhem Land This opening vignette highlights a contradiction that I want to explore from a variety of perspectives in this chapter – abundant populations of environmentally destructive wild buffalo roam widely in an Indigenous Protected Area (IPA) declared for its natural and cultural values of global significance, according to International Union for the Conservation of Nature criteria. -
Storm Surge: Know Your Risk in Queensland!
Storm Surge: Know your risk in Queensland! Storm surge is a rise in sea level above the normal tide usually associated with a low pressure weather system such as a tropical cyclone. Storm surge develops due to strong winds pushing water towards the coastline as well as the low atmospheric pressure drawing up the sea surface. The Queensland coastline is highly vulnerable to storm surge. This is due to the frequency of tropical cyclones, the wide continental shelf and relatively shallow ocean floor in both the Great Barrier Reef lagoon and in the Gulf of Carpentaria, as well as the low lying nature of many coastal cities and towns. While the highest storm surges are more likely to occur in North Queensland and the Gulf of Carpentaria, they can also develop in southeast Queensland affecting the Sunshine Coast, Moreton Bay and the Gold Coast. Storm surges may reach magnitudes of 1 to 10 metres above the tide depending on the intensity of the cyclone, its size and the local characteristics of the coastline. Impacts Coral Sea Storm surge can be very dangerous and poses a critical risk Gulf of Carpentaria to human life during tropical cyclones. Great Cairns Barrier Reef The length of coastline affected by a storm surge can be Innisfail tens to hundreds of kilometres wide. The rise in sea level Cardwell Townsville can be rapid and high in velocity, inundating the ground Bowen floor of buildings, even up to the roof. Mackay Queensland Storm surge has the power to easily move cars, even Gladstone houses, can damage roads and buildings and can be Hervey Bay almost impossible to manoeuvre through. -
Cyclone Tracy Report 1975
DEPARTMENT OF HOUSING AND CONSTRUCTION REPORT ON CYCLONE “TRACY” - Effect On Buildings - DECEMBER 1974 Volume 1 BY GEORGE R WALKER SENIOR LECTURER DEPARTMENT OF ENGINEERING JAMES COOK UNIVERSITY OF NORTH QUEENSLAND MARCH 1975 CONTENTS ACKNOWLEDGEMENTS INTRODUCTION Chapter 1 SUMMARY Chapter 2 CHARACTERISTICS OF CYCLONE “TRACY” Chapter 3 GENERAL PATTERN OF DAMAGE Chapter 4 STRUCTURAL BEHAVIOUR Chapter 5 IMPLICATIONS OF DISASTER Chapter 6 BIBLIOGRAPHY 2 ACKNOWLEDGEMENTS In assembling this report the writer was helped by many people to whom he is deeply grateful. The writer would like to particularly acknowledge the support of Professor D. H. Trollope, Pro-Vice-Chancellor and Professor of Civil Engineering at the James Cook University of North Queensland whose initiative and encouragement in the development of tropical cyclone studies at this University following cyclone “Althea” in December, 1971, has been a primary factor in the writer’s own involvement in this work. The ready and willing co-operation of the Director of the Department of Housing and Construction in Darwin, Mr G. Redmond, and his staff, in particular the Principal Structural Engineer, Mr J. Gamble, is gratefully acknowledged. Much assistance was also gained from members of the Department’s Darwin Reconstruction Study Group. The willing co- operation of Mr D. Green of the Northern Territory Housing Commission was also appreciated. A great deal of assistance was gained in the actual investigation of the damage from others similarly engaged. In particular the writer would like to express his thanks for the assistance of Mr K. Baker and Mr Nicholls and other members of staff of Halpern Glick Pty. -
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.