Nature 423 the Snowy River Project (S.E
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Assessment of Thermal Pollution in the Snowy River Below Jindabyne
Assessment of thermal pollution Snowy River Increased Flows Assessment of thermal pollution in the Snowy River below Jindabyne Dam Summary This study assessed water temperature in the highly regulated Snowy River below Jindabyne Dam. What did we study? • The thermal regime of rivers plays a critical role in the health of aquatic ecosystems. We monitored water temperature below Jindabyne Dam to assess the thermal regime of the regulated Snowy River. Monitoring began in 2011, following the installation of a multi-level offtake and the delivery of environmental flows. It continued until 2013. During this time we compared the regulated thermal regime with a natural thermal regime model. The model was developed using pre-dam (1962-1967) water temperature data. What did we find? • Cold water pollution in the Snowy River below Jindabyne Dam is not a significant issue. • Warm water pollution remains an issue in the regulated Snowy River, particularly between March and July. Yet water temperatures are rarely more than 2 - 4°C warmer than natural. Temperatures never exceed the expected natural temperature range of the Snowy River before Jindabyne Dam. • Water temperatures match the expected natural water temperatures at the town of Dalgety. This is approximately 20km downstream of Jindabyne Dam. What does this mean for water management? • The multi-level offtake has improved the thermal regime in this regulated river. Additional management strategies to improve the thermal regime are limited. An alternate release point in the Mowamba River may further improve water temperatures. The extent of improvements would depend on the dilution of flow volumes from the Mowamba River into the Snowy River. -
Concept Plan
Monaro Acclimatisation Society Inc 9 Thompson Drive Tathra, NSW. 2550 Sustainable future fishing for trout and native fish SNOWY HYDRO 2.0 – MAS CONCEPT PLAN On 2 July 2020 MAS Secretary Rod Whiteway and I met with senior officers from NSW Fisheries to discuss the MAS Concept Plan for a trout grow-out facility as a recreational fishing offset for Snowy Hydro 2.0. Following that meeting NSW Fisheries have asked the MAS to formally enter into “Agreed Principles” arrangement. The MAS Executive is currently discussing this Agreement; however, we indicated we have four key priorities that we are committed to. On 7 July 2020 I met with senior staff from Snowy Hydro to discuss the MAS Concept Plan. Again, we explained our key priorities and Snowy Hydro did not express any negativity to our approach. Snowy Hydro indicated they are keen for a meeting between MAS, DPI and Snowy Hydro in the not too distant future to begin working formally on the plan. THE OVERALL CONCEPT Since the announcement of Snowy Hydro 2.0 the MAS has been concerned that redfin perch would be pumped from Talbingo Dam into Tantangara Dam and beyond. To help protect the Snowy Mountains trout fishery the MAS embarked on a process to identify how larger trout could be stocked to counter the expected redfin predation and to protect our trout fishing legacy and reassure the Snowy trout community that something was being done. The MAS soon realised that it was undertaking this process in a policy vacuum, so the MAS began negotiating directly with Snowy Hydro on mitigation measures. -
To View Asset
Journal entry Restoring health to 04/11/2002 the Snowy River Why the Snowy needs restoring The construction of the Snowy Mountains Hydro-electric Scheme in the 1960s resulted in the diversion of 99% of the Snowy River’s natural flow at Jindabyne Dam. The result of this and other human activities has been a build-up of sediment in the river, weed infestation and reduced habitat for native flora and fauna. 1 Journal entry What’s so special about 04/11/2002 the Snowy River No other river in Australia flows through such diverse vegetation: alpine meadows and Snow Gum Woodlands near Mt Kosciusko, the Montane Grassy Woodlands and grassland of the MonaroTableland, tall wet mountain forests, Warm Temperate Rainforests of the lowland floodplain, wetlands and coastal scrubs and Littoral Rainforests on the coast at Marlo.% Much of the Snowy valley and its remnant vegetation and wetlands continue to be important resting, feeding and breeding areas for migratory species from tropical rainforests in south-east Asia and wetland birds from Russia, China and Japan.% The lowland floodplain of the Snowy River and its rich wetlands are the traditional land of the Krowathunkoolong clan of the Gunai (Kurnai) people. This area still retains cultural significance for these people. 2 Journal entry The History Jindabyne dam 04/11/2002 Dam Wall 1958 Outfall Snowy Mountains Hydro-electric Authority Act 1998 Snowy Water Inquiry Cobbon Dec 2000 Creek Snowy river Agreement of Victorian, New South Wales and Commonwealth Governments to increase the Mowamba aqueduct Snowy River flow by 21% within ten years of Cobbon corporatisation of Snowy Hydro-electric Authority, Weir and 28% in the longer term, as well as 70 gigalitres to the River Murray. -
Long-Term Movements and Activity Patterns of Platypus on Regulated
www.nature.com/scientificreports OPEN Long‑term movements and activity patterns of platypus on regulated rivers Tahneal Hawke1*, Gilad Bino1, Richard T. Kingsford1, Dion Iervasi2, Kylie Iervasi2 & Matthew D. Taylor1,3 The platypus is a semi‑aquatic mammal, endemic to freshwater habitats of eastern Australia. There are gaps in the understanding of platypus movement behaviour within river systems, including spatial and temporal organization of individuals. We tracked movements of 12 platypuses on the regulated Snowy and Mitta Mitta Rivers for up to 12‑months, the longest continuous tracking of platypus using acoustic telemetry. Platypuses remained relatively localized, occupying 0.73–8.45 km of river over 12 months, consistent with previous tracking studies over shorter periods. Males moved further than females, and larger males had higher cumulative movements, suggesting a possible relationship to metabolic requirements. Platypuses moved greater distances on the Mitta Mitta River, possibly associated with impacts of altered fow regimes to their macroinvertebrate diet. Increased movements and diurnal activity during winter were primarily driven by males, possibly attributable to breeding behaviours, rather than increased costs of winter foraging. Evidence for relatively small movements has implications for declining populations, given areas of localised declines are unlikely to be supplemented by migrating platypuses, especially when dispersal is restricted by dam walls. Understanding platypus movement behaviour is pertinent for their conservation, as water resource development and habitat modifcation continue to reduce connectivity between populations across their distribution. Platypuses (Ornithorhynchus anatinus) occur mainly in creeks and rivers of eastern Australia, with an intro- duced population on Kangaroo Island1. Tey are primarily dependent on rivers and other water bodies, feeding exclusively on freshwater macroinvertebrates2, and using burrows on the water’s edge for resting and nesting3. -
Snowy Hydro Water Operations Reference Report
SNOWY HYDRO WATER OPERATIONS REFERENCE REPORT Snowy Hydro Limited ABN 17 090 574 431 Level 37, AMP Centre, 50 Bridge Street, Sydney NSW 2000, GPO Box 4351 Sydney NSW 2001 Telephone: 02 9278 1888 Facsimile: 02 9278 1879, www.snowyhydro.com.au Snowy Hydro Water Operations Reference Report TABLE OF CONTENTS GLOSSARY.....................................................................................................................................................................1 INTRODUCTION...........................................................................................................................................................4 2. PURPOSE OF THIS DOCUMENT......................................................................................................................4 2.1 STATEMENT OF PURPOSE ..................................................................................................................................4 THE WATER OPERATIONS OF THE SNOWY SCHEME.....................................................................................5 3. SNOWY HYDRO ...................................................................................................................................................5 4. THE SNOWY SCHEME .......................................................................................................................................5 4.1 INTRODUCTION .................................................................................................................................................5 -
Hydrology and Scaling Relationships of Snowy Mountain Rivers
University of Wollongong Research Online University of Wollongong Thesis Collection 1954-2016 University of Wollongong Thesis Collections 2016 Hydrology and scaling relationships of Snowy Mountain Rivers Sander van Tol University of Wollongong Follow this and additional works at: https://ro.uow.edu.au/theses University of Wollongong Copyright Warning You may print or download ONE copy of this document for the purpose of your own research or study. The University does not authorise you to copy, communicate or otherwise make available electronically to any other person any copyright material contained on this site. You are reminded of the following: This work is copyright. Apart from any use permitted under the Copyright Act 1968, no part of this work may be reproduced by any process, nor may any other exclusive right be exercised, without the permission of the author. Copyright owners are entitled to take legal action against persons who infringe their copyright. A reproduction of material that is protected by copyright may be a copyright infringement. A court may impose penalties and award damages in relation to offences and infringements relating to copyright material. Higher penalties may apply, and higher damages may be awarded, for offences and infringements involving the conversion of material into digital or electronic form. Unless otherwise indicated, the views expressed in this thesis are those of the author and do not necessarily represent the views of the University of Wollongong. Recommended Citation van Tol, Sander, Hydrology and scaling relationships of Snowy Mountain Rivers, Master of Philosophy thesis, School of Earth and Environmental Sciences, University of Wollongong, 2016. -
EPBC Act Referral 2018/8217) Was Lodged with the Commonwealth Department of the Environment and Energy (DEE) and Publicly Notified from 2 June to 20 June 2018
Submission #3733 - Snowy 2.0 Main Works Title of Proposal - Snowy 2.0 Main Works Section 1 - Summary of your proposed action Provide a summary of your proposed action, including any consultations undertaken. 1.1 Project Industry Type Commonwealth Development 1.2 Provide a detailed description of the proposed action, including all proposed activities. Snowy 2.0 Snowy Hydro Limited (Snowy Hydro), the operator of the Snowy Mountains Hydro-electric Scheme (Snowy Scheme), is proposing to build and operate Snowy 2.0. Snowy 2.0 is a project that will increase the pumped hydro-electric capacity within the existing Snowy Scheme by linking the Tantangara and Talbingo reservoirs with tunnels feeding a new underground power station. The project will involve tunnelling and excavation works between the two reservoirs to depths of up to 1 kilometre (km). Snowy 2.0 has been declared Critical State Significant Infrastructure (CSSI) in accordance with the provisions of Division 5.2 of the New South Wales (NSW) Environmental Planning and Assessment Act 1979 (EP&A Act) with the declaration coming into effect on 9 March 2018. As a result, Snowy 2.0 may be carried out without obtaining development consent under Part 4 of the EP&A Act. However, Snowy 2.0 is subject to Division 5.2 of the EP&A Act, which requires the preparation of an environmental impact statement (EIS) and the approval of the NSW Minister for Planning. With respect to the provisions of the Commonwealth Environment Protection and Biodiversity Conservation Act 1999 (EPBC Act), while considerable survey work has been carried out to date, additional detailed surveys remain to be completed to determine potential impacts of Snowy 2.0 Main Works on matters of national environmental significance (MNES) and the environment generally. -
Discovering the Snowies - Tour Itineraries Tour Itineraries - Continued
Discovering the Snowies - Tour itineraries Tour itineraries - continued The Snowies are well served by a network of sealed roads boasting spectacular scenery. The Snowy Mountains Drive can DAY 4 - ALPINE WAY This stretch of Tourist Drive 1 takes A stop further along at Scammels Spur lookout is a must. be accessed from Canberra in the north, Bega on the south coast and Albury to the southwest. Take your time enjoying one of you across the natural watershed of the Australian Alps. Constructed for a visit by Queen Elizabeth in 1950s, it gives Australia’s greatest natural resources at your own pace. Below Deadhorse Gap the rivers flow east into the Snowy. the best view of the western faces of the Australian Alps. Wild brumbies gather here to exploit the sub-alpine pasture. Observe Mt Kosciuszko as it rises 1900m from the valley floor. The “Snowies” contains the nation’s highest peak, Mt Kosciuszko, the inspiring feat of the Snowy Hydro Electric Scheme, They are best seen in mornings and late afternoons, and and the state’s largest preserved natural area in Kosciuszko National Park. This physical face is given its cultural heart by the KHANCOBAN Plan a stop at the Murray 1 Power Station and there are more good walking trails here to explore. heritage preserved in the park, in the people’s literature, storytelling and folklore. Information Centre, featuring an excellent display on the Snowy Continue along the Alpine Way past Tom Groggin Station, once Scheme’s history and the people who built it. The Tourist Drive 1 claimed to be home of the "Man from Snowy River", to Geehi. -
Snowy Hydro Water Report for 2014–15
CONTENTS UNDERSTANDING WATER & OUR BUSINESS 01 THE 2014-2015 WATER YEAR – WHAT WATER CAME IN 16 OVERVIEW OF SNOWY HYDRO 03 INFLOWS 16 HOW THE SNOWY SCHEME WORKS 06 SNOWY SCHEME STORAGES 17 THE SNOWY-TUMUT DEVELOPMENT 07 LAKE LEVELS 17 THE SNOWY-MURRAY DEVELOPMENT 08 COMPLYING WITH OUR LICENCE- WHAT WATER WENT OUT 20 UNDERSTANDING WATER & THE SCHEME 09 WESTERN RIVER RELEASES 21 SHARING OF INFLOWS BETWEEN CATCHMENTS 12 ENVIRONMENTAL RELEASES 25 FLOOD OPERATIONS 13 Lake Eucumbene WATER REPORT 2014 – 2015 FOREWORD Since the Snowy Scheme’s completion in 1974, Snowy Hydro Limited has been the custodian of the water that flows through the Scheme’s complex maze of dams, tunnels, aqueducts and power stations. This report outlines how we are managing that water and steps we are taking to minimise the impact of our operations on the environment. Snowy Hydro has always operated under a strict Water Licence which governs how we can use the water that is collectively the property of the people of New South Wales and Victoria. There are also strong environmental safeguards that govern our operations and our presence in the Kosciuzko National Park. Snowy Hydro is an exemplary corporate citizen and we take our obligations to meet the conditions of our licences and any regulations applying to our business very seriously. We are privileged to operate in some of the most picturesque areas of the Snowy Mountains and we understand that locals and visitors alike are attracted to the area because of the beautiful dams and waterways. This report is an important channel to educate and inform our stakeholders about the water operations of the Snowy Scheme. -
Murray-Darling Basin Amendment Bill 2002
INFORMATION, ANALYSIS AND ADVICE FOR THE PARLIAMENT INFORMATION AND RESEARCH SERVICES Bills Digest No. 57 2002–03 Murray-Darling Basin Amendment Bill 2002 DEPARTMENT OF THE PARLIAMENTARY LIBRARY ISSN 1328-8091 Copyright Commonwealth of Australia 2002 Except to the extent of the uses permitted under the Copyright Act 1968, no part of this publication may be reproduced or transmitted in any form or by any means including information storage and retrieval systems, without the prior written consent of the Department of the Parliamentary Library, other than by Senators and Members of the Australian Parliament in the course of their official duties. This paper has been prepared for general distribution to Senators and Members of the Australian Parliament. While great care is taken to ensure that the paper is accurate and balanced, the paper is written using information publicly available at the time of production. The views expressed are those of the author and should not be attributed to the Information and Research Services (IRS). Advice on legislation or legal policy issues contained in this paper is provided for use in parliamentary debate and for related parliamentary purposes. This paper is not professional legal opinion. Readers are reminded that the paper is not an official parliamentary or Australian government document. IRS staff are available to discuss the paper's contents with Senators and Members and their staff but not with members of the public. Inquiries Members, Senators and Parliamentary staff can obtain further information from the Information and Research Services on (02) 6277 2646. Information and Research Services publications are available on the ParlInfo database. -
Proceedings of an International Year of Mountains: Full Document
PROCEEDINGS OF AN INTERNATIONAL YEAR OF MOUNTAINS Coordinated by CONFERENCE In partnership with Jindabyne - Australia November 25-28, 2002 Sponsored by As part of Acknowledgements In addition to some presenters who were unable to supply their written paper, there were a number of Aboriginal presenters from different parts of Australia who chose not to submit a written form of their presentation as this is not a traditional method of communication. © 2003. This work is copyright. Copyright in this printed edition is held by the Australian Alps Liaison Committee (AALC). Apart from any use as permitted under the Copyright Act 1968, no part may be reproduced by any process without written permission. Copyright on individual papers, photographs and graphic images is held by the author. These proceedings have been sponsored by Transgrid. Edited and produced by Janet Mackay & Associates. Copies of this publication are available from: Australian Alps Liaison Committee c/- Canprint Communications PO Box 7456 Canberra Mail Centre ACT 2610 Telephone: +61 2 6295 4422 ISBN: 0-646-42204-9 For more information on the Australian Alps national parks co-operative program, visit our website at www.australianalps.ea.gov.au. Welcome to Country My name is Rae Solomon Stewart. I was born in Orbost on the banks of the Snowy River. My family come from Dalgety and South Jindabyne areas. I come to Jindabyne to welcome all the people that are here today to celebrate the Year of the Mountain. Malarkin gungee yalarguin In Aboriginal languages one word has more than one meaning. We are all gathered here peacefully for the Year of the Mountain celebration and we welcome you to our country. -
Snowy River Below Lake Jindabyne
Australia ―7 Snowy River below Lake Jindabyne Map of River 3 Australia ―7 Table of Basic Data Name(s): Snowy River below Lake Jindabyne Serial No. : Australia-7 Location: Southeastern Australia N 36° 27' ~ 37° 50' E 148° ~ 149° 30' Area: 11,720 km2 below Lake Jindabyne Length of main stream: 350 km Origin: Lake Jindabyne Highest point: Mt Cobberas, 1,833 m Outlet: Tasman Sea Lowest point: River mouth at sea level Main geological features: Low grade metamorphic and granitic rocks Main tributaries: Maclaughlin, Delegate, Deddick and Buchan rivers Main lakes: None Main reservoirs: Jindabyne Dam (most upstream point of the catchment) Mean annual precipitation: 500 mm in the coastal region to 3,800 mm in the upper central region Mean annual runoff: 43.1 m3/s post Jindabyne Dam construction Population: approx 12,000 (2001) Main cities: Orbost Land use: Grazing, National Park, forestry, intensive cropping in lower reaches 1. General Description The Snowy River catchment extends from Kiandra in the Snowy Mountains to the river mouth at Marlo where it flows into the Tasman Sea. The total catchment area is 13,570 km2 with the area below Lake Jindabyne being 11,720 km2. The annual precipitation ranges from 500 mm to 3,800 mm with the highest precipitation occurring on the mountain peaks in the form of winter snow. Precipitation in the upper Snowy catchment is highest during late autumn and lowest during summer and is increased by orographic effects. The central portion of the catchment (below Lake Jindabyne) is in a rainshadow and experiences mean annual rainfall of about 500 mm.