Gas Supply and Demand Scenarios 2012-2027
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Greenpeace Deep Sea Oil Briefing
May 2012 Out of our depth: Deep-sea oil exploration in New Zealand greenpeace.org.nz Contents A sea change in Government strategy ......... 4 Safety concerns .............................................. 5 The risks of deep-sea oil ............................... 6 International oil companies in the dock ..... 10 Where is deep-sea oil exploration taking place in New Zealand? ..................... 12 Cover: A view from an altitude of 3200 ft of the oil on the sea surface, originated by the leaking of the Deepwater Horizon wellhead disaster. The BP leased oil platform exploded April 20 and sank after burning, leaking an estimate of more than 200,000 gallons of crude oil per day from the broken pipeline into the sea. © Daniel Beltrá / Greenpeace Right: A penguin lies in oil spilt from the wreck of the Rena © GEMZ Photography 2 l Greenpeace Deep-Sea Oil Briefing l May 2012 The inability of the authorities to cope with the effects of the recent oil spill from the Rena cargo ship, despite the best efforts of Maritime New Zealand, has brought into sharp focus the environmental risks involved in the Government’s decision to open up vast swathes of the country’s coastal waters for deep-sea oil drilling. The Rena accident highlighted the devastation that can be caused by what in global terms is actually still a relatively small oil spill at 350 tonnes and shows the difficulties of mounting a clean-up operation even when the source of the leaking oil is so close to shore. It raised the spectre of the environmental catastrophe that could occur if an accident on the scale of the Deepwater Horizon disaster in the Gulf of Mexico were to occur in New Zealand’s remote waters. -
Planktonic Foraminifera As Oceanographic Proxies: Comparison of Biogeographic Classifications Using Some Southwest Pacific Core-Top Faunas
Hindawi Publishing Corporation ISRN Oceanography Volume 2013, Article ID 508184, 15 pages http://dx.doi.org/10.5402/2013/508184 Review Article Planktonic Foraminifera as Oceanographic Proxies: Comparison of Biogeographic Classifications Using Some Southwest Pacific Core-Top Faunas G. H. Scott GNS Science, 1 Fairway Drive, Lower Hutt 5010, New Zealand Correspondence should be addressed to G. H. Scott; [email protected] Received 29 April 2013; Accepted 17 June 2013 Academic Editors: M. Elskens and M. T. Maldonado Copyright © 2013 G. H. Scott. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. The distribution of planktonic foraminifera, as free-floating protists, is largely controlled by hydrography. Their death assemblages in surficial sediments provide proxy data on upper water mass properties for paleoceanography. Techniques for mapping faunal distributions for this purpose are compared in a study of 35 core-top samples that span the Subtropical Front in the Southwest Pacific. Faunas are analyzed by taxon composition, order of dominant taxa, and abundance. Taxon composition (presence-absence data) and dominant taxa (ordinal data) recognize groups of sites that approximate major water mass distributions (cool subtropical water, subantarctic water) and clearly define the location of the Subtropical Front. Quantitative data (relative abundances) more closely reflect the success of taxa in upper water mass niches. This information resolves groups of sites that reflect differences in intrawater mass hydrography. Comparisons suggest that abundance data should provide much better oceanographic resolution globally than the widely used ordinal biogeographic classification that identifies only Tropical, Subtropical Transitional, Subpolar and Polar provinces. -
Campbell Plateau: a Major Control on the SW Pacific Sector of The
Ocean Sci. Discuss., doi:10.5194/os-2017-36, 2017 Manuscript under review for journal Ocean Sci. Discussion started: 15 May 2017 c Author(s) 2017. CC-BY 3.0 License. Campbell Plateau: A major control on the SW Pacific sector of the Southern Ocean circulation. Aitana Forcén-Vázquez1,2, Michael J. M. Williams1, Melissa Bowen3, Lionel Carter2, and Helen Bostock1 1NIWA 2Victoria University of Wellington 3The University of Auckland Correspondence to: Aitana ([email protected]) Abstract. New Zealand’s subantarctic region is a dynamic oceanographic zone with the Subtropical Front (STF) to the north and the Subantarctic Front (SAF) to the south. Both the fronts and their associated currents are strongly influenced by topog- raphy: the South Island of New Zealand and the Chatham Rise for the STF, and Macquarie Ridge and Campbell Plateau for the SAF. Here for the first time we present a consistent picture across the subantarctic region of the relationships between front 5 positions, bathymetry and water mass structure using eight high resolution oceanographic sections that span the region. Our results show that the northwest side of Campbell Plateau is comparatively warm due to a southward extension of the STF over the plateau. The SAF is steered south and east by Macquarie Ridge and Campbell Plateau, with waters originating in the SAF also found north of the plateau in the Bounty Trough. Subantarctic Mode Water (SAMW) formation is confirmed to exist south of the plateau on the northern side of the SAF in winter, while on Campbell Plateau a deep reservoir persists into the following 10 autumn. -
Bathymetry of the New Zealand Region
ISSN 2538-1016; 11 NEW ZEALAND DEPARTMENT OF SCIENTIFIC AND INDUSTRIAL RESEARCH BULLETIN 161 BATHYMETRY OF THE NEW ZEALAND REGION by J. W. BRODIE New Zealand Oceanographic Institute Wellington New Zealand Oceanographic Institute Memoir No. 11 1964 This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ Fromispiece: The survey ship HMS Penguin from which many soundings were obtained around the New Zealand coast and in the south-west Pacific in the decade around 1900. (Photograph by courtesy of the Trustees, National Maritime Museum, Greenwich.) This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ NEW ZEALAND DEPARTMENT OF SCIENTIFIC AND INDUSTRIAL RESEARCH BULLETIN 161 BATHYMETRY OF THE NEW ZEALAND REGION by J. W. BRODIE New Zealand Oceanographic Institute Wellington New Zealand Oceanographic Institute Memoir No. 11 1964 Price: 15s. This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ CONTENTS Page No. ABSTRACT 7 INTRODUCTION 7 Sources of Data 7 Compilation of Charts 8 EARLIER BATHYMETRIC INTERPRETATIONS 10 Carte Gen�rale Bathymetrique des Oceans 17 Discussion 19 NAMES OF OCEAN FLOOR FEATURES 22 Synonymy of Existing Names 22 Newly Named Features .. 23 FEATURES ON THE CHARTS 25 Major Morphological Units 25 Offshore Banks and Seamounts 33 STRUCTURAL POSITION OF NEW ZEALAND 35 The New Zealand Plateau 35 Rocks of the New Zealand Plateau 37 Crustal Thickness Beneath the New Zealand Plateau 38 Chatham Province Features 41 The Alpine Fault 41 Minor Irregularities on the Sea Floor 41 SEDIMENTATION IN THE NEW ZEALAND REGION . -
Determination of Critical Contingency Price in Respect of the Critical Contingency of 3Rd March 2012
Determination of Critical Contingency Price in respect of the critical contingency of 3rd March 2012 Tim Denne ([email protected]) 20th April 2012 Introduction 1. This report sets out my determination of a Critical Contingency Price as required by the Gas Governance (Critical Contingency Management) Regulations 2008 (‘the Regulations’). The Critical Contingency Price is required in respect of the critical contingency of 3rd March 2012. 2. A critical contingency is defined under the Regulations. It is triggered when the operating pressure reaches a low threshold that defines the pressure required to “maintain the supply of gas across the relevant part or parts of the transmission system and to avoid disruption of distribution systems connected to the transmission system” (Regulation 25(1)(a)(iv)). 3. A draft report and recommended price was discussed at a workshop with interested parties on 16th April 2012. There were no objections to the proposed price. 4. My determination is that the critical contingency price for 3rd March 2012 is $11.10/GJ. The explanation is given below. The Event 5. A critical contingency was declared on the Maui pipeline on 3rd March 2012 following an unplanned outage of the Pohokura Production Station. The plant shutdown initially occurred as a result of a power outage at 3.40am, but production could not restart because of a fault in the plant heating system. The outage resulted in reduced supply and a low pressure being recorded at Rotowaro that fell below the threshold that triggered a critical contingency. The sequence of events is shown in Figure 1. -
Connection Plus March/April 2001
Your business newsletter from WEL Energy Group March/April 2001 24 hour faults 0800 800 WEL Threestrikes 0800 800 935 andand you’reyou’re notnot outout InternationalInternational WEL has improved its supply reliability during flavourflavour toto storms and lightning strikes thanks to a reconfigured WEL Energy lines network. contractors check BalloonsBalloons overover A two-year, $10 million programme is being completed to the network as part reduce the length of time Waikato customers suffer outages. of our reliability WaikatoWaikato Several new 33,000 and 11,000-volt cables and associated upgrade. indoor switchgear were installed in Hamilton North, and Contact Energy’s Te Rapa cogeneration plant was brought What’s that in the sky? It’s a bird? into the system. It’s a plane? No, it’s a new, huge, specially shaped Until recently the WEL’s system was operated as a radial balloon being brought to Balloons over network. Any fault on the 33,000-volt lines supplying its Waikato thanks to sponsorship from the substations resulted in a total loss of supply to that Hamilton City Council. substation. WEL is getting behind the WEL Energy WEL Contracts Manager Bill Doig says the old system looked Trust-sponsored annual hot air balloon like a tree and if any branch was affected by an outage, festival in April. Event Manager Linda Kelly everyone on that branch was cut off until repairs were says registrations have already been made. received from balloonists in Australia, The new system created a ring network so power is able America, Britain, Canada and a number of to be re-routed through another line. -
Fonterra Submission on CCM Consultation 24 July 2020
Statement of proposal for amending the Critical Contingency Management Regulations Summary Fonterra welcomes the opportunity to provide feedback on the Statement of Proposal for amending the Critical Contingency Management Regulations paper. Fonterra is a co-operative owned by around 10,000 New Zealand farmers, and as such we take a long-term view of both our industry and our country. We are New Zealand’s largest co-operative with 30 manufacturing sites spread across New Zealand with more than 10,000 staff working for the Co-operative in regional New Zealand. Natural gas is a critical energy source for 18 of our North Island manufacturing sites. Processing our farmers' milk within 12-hours of collection is vital to avoid the significant environmental damage from disposing milk on farm. The significant environmental and economic damage that results from an outage remains long after the gas has been restored. As our 18 sites are located from Whangārei in the north down to Pahiatua in the south, we are the only major gas user that is exposed to the greatest risk of a gas outage with each kilometre of pipeline to get to our sites. We have installed diesel fuel back-up at four of our sites to assist with mitigating some of the gas outage risk from various regional scenarios. This investment has been made based upon a range of factors, including how much could be utilised without jeopardising New Zealand’s diesel stocks. Fonterra considers that greater prioritisation of gas supply needs to be given to the dairy industry , especially during the peak milk months (September to December), to minimise both environmental and economic damage that would occur from a sustained gas outage. -
Paper Is Divided Into Two Parts
Earth-Science Reviews 140 (2015) 72–107 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Geologic and kinematic constraints on Late Cretaceous to mid Eocene plate boundaries in the southwest Pacific Kara J. Matthews a,⁎, Simon E. Williams a, Joanne M. Whittaker b,R.DietmarMüllera, Maria Seton a, Geoffrey L. Clarke a a EarthByte Group, School of Geosciences, The University of Sydney, NSW 2006, Australia b Institute for Marine and Antarctic Studies, University of Tasmania, TAS 7001, Australia article info abstract Article history: Starkly contrasting tectonic reconstructions have been proposed for the Late Cretaceous to mid Eocene (~85– Received 25 November 2013 45 Ma) evolution of the southwest Pacific, reflecting sparse and ambiguous data. Furthermore, uncertainty in Accepted 30 October 2014 the timing of and motion at plate boundaries in the region has led to controversy around how to implement a Available online 7 November 2014 robust southwest Pacific plate circuit. It is agreed that the southwest Pacific comprised three spreading ridges during this time: in the Southeast Indian Ocean, Tasman Sea and Amundsen Sea. However, one and possibly Keywords: two other plate boundaries also accommodated relative plate motions: in the West Antarctic Rift System Southwest Pacific fi Lord Howe Rise (WARS) and between the Lord Howe Rise (LHR) and Paci c. Relevant geologic and kinematic data from the South Loyalty Basin region are reviewed to better constrain its plate motion history during this period, and determine the time- Late Cretaceous dependent evolution of the southwest Pacific regional plate circuit. A model of (1) west-dipping subduction Subduction and basin opening to the east of the LHR from 85–55 Ma, and (2) initiation of northeast-dipping subduction Plate circuit and basin closure east of New Caledonia at ~55 Ma is supported. -
38. Seismic Stratigraphy and Structure Adjacent to an Evolving Plate Boundary, Western Chatham Rise, New Zealand1
38. SEISMIC STRATIGRAPHY AND STRUCTURE ADJACENT TO AN EVOLVING PLATE BOUNDARY, WESTERN CHATHAM RISE, NEW ZEALAND1 K. B. Lewis, New Zealand Oceanographic Institute D. J. Bennett, Geophysics Division of the Department of Scientific and Industrial Research, New Zealand R. H. Herzer, New Zealand Geological Survey and C. C. von der Borch, Flinders University2 ABSTRACT Seismic profiles obtained from the eastern side of New Zealand, in transit to and from Site 594, illustrate the evolu- tion of the western end of the Chatham Rise and the southern extremity of the Hikurangi Trough. They show several unconformities and several major changes in tectonic and depositional regime. The unconformities represent major changes in oceanic circulation, possibly triggered by large lowerings of sea level in the late Oligocene and late Miocene. Tectonism is exemplified by a Late Cretaceous phase of block faulting, heralding the rift from Gondwanaland, and by Plio-Pleistocene normal faulting on the northern flank of the rise antithetic to the oblique-collision plate boundary in the southern Hikurangi Trough. This active normal faulting may indicate that the northwestern corner of Chatham Rise continental crust is being dragged down with the subducting slab to the north. The depositional regime has changed from Late Cretaceous infilling of fault-angle depressions, through an early Tertiary transgression and mid-Tertiary car- bonate drape, to a late Miocene-Recent sequence recording repeated glacial-interglacial events. This upper stratified unit onlaps a late Miocene erosion/phosphatization unconformity toward the crest of the rise. It is locally truncated by a slope-parallel erosion surface, with downslope buildup, which may indicate either current scour and deposition or mass movement. -
Seismic Database Airborne Database Studies and Reports Well Data
VOL. 8, NO. 2 – 2011 GEOSCIENCE & TECHNOLOGY EXPLAINED geoexpro.com EXPLORATION New Zealand’s Ida Tarbell and the Standard Underexplored Oil Company Story Potential HISTORY OF OIL Alaska: The Start of Something Big TECHNOLOGY Is Onshore Exploration Lagging Behind? GEOLOGY GEOPHYSICS RESERVOIR MANAGEMENT Explore the Arctic Seismic database Airborne database Studies and reports Well data Contact TGS for your Arctic needs TGS continues to invest in geoscientific data in the Arctic region. For more information, contact TGS at: [email protected] Geophysical Geological Imaging Products Products Services www.tgsnopec.com Previous issues: www.geoexpro.com Thomas Smith Thomas GEOSCIENCE & TECHNOLOGY EXPLAINED COLUMNS 5 Editorial 30 6 ExPro Update 14 Market Update The Canadian Atlantic basins extend over 3,000 km from southern Nova 16 A Minute to Read Scotia, around Newfoundland to northern Labrador and contain major oil 44 GEO ExPro Profile: Eldad Weiss and gas fields, but remain a true exploration frontier. 52 History of Oil: The Start of Something Big 64 Recent Advances in Technology: Fish are Big Talkers! FEATURES 74 GeoTourism: The Earth’s Oldest Fossils 78 GeoCities: Denver, USA 20 Cover Story: The Submerged Continent of New 80 Exploration Update New Zealand 82 Q&A: Peter Duncan 26 The Standard Oil Story: Part 1 84 Hot Spot: Australian Shale Gas Ida Tarbell, Pioneering Journalist 86 Global Resource Management 30 Newfoundland: The Other North Atlantic 36 SEISMIC FOLDOUT: Gulf of Mexico: The Complete Regional Perspective 42 Geoscientists Without Borders: Making a Humanitarian Difference 48 Indonesia: The Eastern Frontier Eldad Weiss has grown his 58 SEISMIC FOLDOUT: Exploration Opportunities in business from a niche provider the Bonaparte Basin of graphical imaging software to a global provider of E&P 68 Are Onshore Exploration Technologies data management solutions. -
Geomagnetism of the Bounty Region East of the South ·Island, N�W Zealand
ISSN 2538-1016; 30 NEW ZEALAND DEPARTMENT OF' SCIENTIFIC AND_ INDUSTRIALI RESEARCH BULLETIN 170 GEOLOGY AND ·GEOMAGNETISM OF THE BOUNTY REGION EAST OF THE SOUTH ·ISLAND, N�W ZEALAND ( ( by DALE C. KRAUSE .. New Zealand Oceanographic Institute Memoir No. 30 1966 GEOLOGY AND GEOMAGNETISM OF THE BOUNTY REGION EAST OF THE SOUTH ISLAND, NEW ZEALAND This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ tr - ,1. __ l ,,, . � Photo, E. J. Thorn/Pt' MV Taranui in Wellington Harbour. This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ NEW ZEALAND DEPARTMENT OF SCIENTIFIC AND INDUSTRIAL RESEARCH BULLETIN 170 GEOLOGY AND GEOMAGNETISM OF THE BOUNTY REGION EAST OF THE SOUTH ISLAND, NEW ZEALAND by DALE C. KRAUSE New Zealand Oceanographic Institute Memoir No. 30 Price: 1 s. 6d. (S1.75) 1966 This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ This publication should be referred to as: N.Z. Dep. sci. industr. Res. Bull. 170 CROWN COPYRIGHT R. E. OWEN', GOVER. "'.!ENT PRINTER, WELLINGTON, NEW ZEALAND-1966 This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ CONTENTS Paa• FOREWORD 7 ABSTRACT 9 INTRODUCTION 9 BATHYMETRY - SOURCES OF INFORMATION 11 ' '. -
Critical Contingency Management Plan
Approved 30 September 2020 Critical Contingency Management Plan Prepared in accordance with the Gas Governance (Critical Contingency Management) Regulations 2008 First Gas Limited October 2020 Plan | Critical Contingency Management Plan Version Control This document is uncontrolled Control Details Owner Ryan Phipps, Transmission Operations Manager Version 12.0 Department Transmission Operations Effective date October 2020 Review date October 2020 Preparer John Blackstock, Senior Commercial Advisor History Version Date Summary of changes Preparer 7.0 18/12/2009 First issue for publication 8.0 09/05/2012 Revised to update the CCOs contact details 9.1 11/09/2012 Revised to reflect the recommendations made in the December 2011 and April 2012 Performance Reports, and amendment to Critical Contingency Imbalance Methodology 9.0 25/02/2014 Revised to update TSO and CCO contact details with effect from 1 March 2014 Revised to reflect amendment to the Gas Governance (Critical 10.0 14/05/2014 Contingency Management) Regulations 2008, and the appointment of a new CCO Minor corrections and amendments made to ensure 10.1 17/12/2014 consistency with the CCO’s amended Communications Plan Adapted to First Gas Limited business branding with minor 10.2 23/05/2016 Rebecca Pendrigh updates in formatting Revised to reflect the sale of the Maui Pipeline asset to First 10.3 16/06/2016 Gas Limited and consequently removal of references to MDL John Blackstock and other necessary contextual amendments Revised to become sole CCMP document for all of the 11.0 20/02/2017 Transmission System and to incorporate suggested John Blackstock amendments from previous critical contingency test exercises Changes drafted in 2018/2019 to accommodate the prospective commencement of the GTAC (including feedback from industry consultation).