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Geology of the Wairarapa Area
GEOLOGY OF THE WAIRARAPA AREA J. M. LEE J.G.BEGG (COMPILERS) New International NewZOaland Age International New Zealand 248 (Ma) .............. 8~:~~~~~~~~ 16 il~ M.- L. Pleistocene !~ Castlecliffian We £§ Sellnuntian .~ Ozhulflanl Makarewan YOm 1.8 100 Wuehlaplngien i ~ Gelaslan Cl Nukumaruan Wn ~ ;g '"~ l!! ~~ Mangapanlan Ql -' TatarianiMidian Ql Piacenzlan ~ ~;: ~ u Wai i ian 200 Ian w 3.6 ,g~ J: Kazanlan a.~ Zanetaan Opoitian Wo c:: 300 '"E Braxtonisn .!!! .~ YAb 256 5.3 E Kunaurian Messinian Kapitean Tk Ql ~ Mangapirian YAm 400 a. Arlinskian :;; ~ l!!'" 500 Sakmarian ~ Tortonisn ,!!! Tongaporutuan Tt w'" pre-Telfordian Ypt ~ Asselian 600 '" 290 11.2 ~ 700 'lii Serravallian Waiauan 5w Ql ." i'l () c:: ~ 600 J!l - fl~ '§ ~ 0'" 0 0 ~~ !II Lillburnian 51 N 900 Langhian 0 ~ Clifdenian 5e 16.4 ca '1000 1 323 !II Z'E e'" W~ A1tonian PI oS! ~ Burdigalian i '2 F () 0- w'" '" Dtaian Po ~ OS Waitakian Lw U 23.8 UI nlan ~S § "t: ." Duntroonian Ld '" Chattian ~ W'" 28.5 P .Sll~ -''" Whalngaroan Lwh O~ Rupelian 33.7 Late Priabonian ." AC 37.0 n n 0 I ~~ ~ Bortonian Ab g; Lutetisn Paranaen Do W Heretauncan Oh 49.0 354 ~ Mangaorapan Om i Ypreslan .;;: w WalD8wsn Ow ~ JU 54.8 ~ Thanetlan § 370 t-- §~ 0'" ~ Selandian laurien Dt ." 61.0 ;g JM ~"t: c:::::;; a.os'"w Danian 391 () os t-- 65.0 '2 Maastrichtian 0 - Emslsn Jzl 0 a; -m Haumurian Mh :::;; N 0 t-- Campanian ~ Santonian 0 Pragian Jpr ~ Piripauan Mp W w'" -' t-- Coniacian 1ij Teratan Rt ...J Lochovlan Jlo Turonian Mannaotanean Rm <C !II j Arowhanan Ra 417 0- Cenomanian '" Ngaterian Cn Prldoli -
Ecohydrological Characterisation of Whangamarino Wetland
http://researchcommons.waikato.ac.nz/ Research Commons at the University of Waikato Copyright Statement: The digital copy of this thesis is protected by the Copyright Act 1994 (New Zealand). The thesis may be consulted by you, provided you comply with the provisions of the Act and the following conditions of use: Any use you make of these documents or images must be for research or private study purposes only, and you may not make them available to any other person. Authors control the copyright of their thesis. You will recognise the author’s right to be identified as the author of the thesis, and due acknowledgement will be made to the author where appropriate. You will obtain the author’s permission before publishing any material from the thesis. ECOHYDROLOGICAL CHARACTERISATION OF WHANGAMARINO WETLAND A thesis submitted in partial fulfilment of the requirements for the degree of Masters of Science in Earth Sciences at The University of Waikato By JAMES MITCHELL BLYTH The University of Waikato 2011 Abstract The Whangamarino wetland is internationally recognised and one of the most important lowland wetland ecosystems in the Waikato Region. The wetland‟s hydrology has been altered by reduced river base levels, the installation of a weir to raise minimum water levels and the Lower Waikato Waipa Flood Control Scheme, which is linked via the (hypertrophic) Lake Waikare and affected by varying catchment land use practices. When water levels exceed capacity, the overflow is released into the Whangamarino wetland, which also receives flood waters from Whangamarino River. Water levels in the wetland are also affected at high stage, by a control structure near Meremere at the confluence of Waikato and Whangamarino Rivers, and at low stage by a weir a short distance upstream. -
Stakeholder Study: Resource Management of Wairarapa Moana
Natalie Diltz Jena Mazzucco Austin Scott Jeffrey Sirocki March 2, 2016 STAKEHOLDER STUDY: RESOURCE MANAGEMENT OF WAIRARAPA MOANA Identification and Analysis of Wairarapa Moana Stakeholder Opinions Regarding the Management of the Blundell Barrage Gates Abstract This project aided the Greater Wellington Regional Council (GWRC) in collecting opinions from five stakeholder groups concerning management of the naturally flooding Lake Wairarapa in New Zealand. Our team conducted a total of twenty-nine interviews with the Rangitāne (Māori), Department of Conservation, South Wairarapa District Council, landowners, and recreational water users regarding the Blundell Barrage Gates which play a vital role in flood management. Interview discussions indicate that water quality, sources of pollution, water levels, flood management, and future operation of the barrage gates are controversial. We identified communication, collaboration, and education as three areas of focus for the GWRC as they continue to improve their management of the region. i Executive Summary This project is concerned with Wairarapa Moana, a water system located in the Wairarapa region, situated on the North Island of New Zealand. Wairarapa Moana consists of the three main water bodies, shown in Figure 1; the coastal lake is Lake Onoke, the inland lake is Lake Wairarapa, and the main river is the Ruamahanga. The system is dynamic, which means water can flow in both directions. Both tidal movements and rainfall affect the direction of flow. The area is low-lying and sits between two mountain ranges exposing much of the land to seasonal flooding. The Greater Wellington Regional Council, the governing body for the Wellington region, developed the Lower Wairarapa Valley Development Scheme (LWVDS), to control flooding in the 1960s. -
RUAMĀHANGA RIVER RUAMĀHANGA REACH 2: Mount Bruce X
RUAMAHANGA RIVER REACH 1: Ruamahanga Headwaters RUAMĀHANGA RIVER RUAMĀHANGA REACH 2: Mount Bruce x VOLUME 2 VOLUME REACH 3: Hidden Lakes DRAFT TE KĀURU UPPER RUAMĀHANGA UPPERRUAMĀHANGA KĀURU TE DRAFT REACH 4: Double Bridges to FLOODPLAIN MANAGEMENT PLAN MANAGEMENT FLOODPLAIN Te Ore Ore REACH 5: Te Ore Ore to Waingawa Confluence REACH 6: Waingawa Confluence to Gladstone Bridge REACH 8: Kokotau Rd Bridge to Waiohine River Confluence REACH 7: Gladstone Bridge to Kototau Rd Bridge Ruamāhanga River RUAMĀHANGA RIVER RUAMĀHANGA 1 2. Ruamāhanga River General Issues The Ruamāhanga flows from its source in the Tararua Ranges down through steep mountainous terrain and native The Ruamāhanga River is well known to the Wairarapa community for its flood flows. The relatively entrenched upper 2 VOLUME forests, running through rock-lined gorges and boulder garden rapids before leaving the foothills close to Pukaha / reaches of the Ruamāhanga River contain much of the flood water, confining it between old river terraces, and its Mount Bruce. From there, it flows through a number of steep-sided gorges where historic river terracing can be seen passage is controlled in several locations by prominent rocky outcrops. As it turns to the south at its confluence with through the fringes of patchy native and exotic vegetation, before opening out into the pastoral Wairarapa Plains. Here the Kopuaranga River it opens into a broader floodplain, and the modelled flood events show a greater extent of the it turns to a more southerly direction flowing downstream through confluences with all of the other rivers which flow adjacent land under water. -
RUAMAHANGA RIVER FISHERY ACCESS POINTS ACCESS POINTS the Ruamahanga River Is the Principal Trout Fishery in the Wairarapa
Wellington Region Wellington your left. This sign marks the turn off onto a track that runs about about runs that track a onto off turn the marks sign This left. your Photo: AndrewHarding website Game & Fish Wellington Road for 3.3km until you see a Fish & Game ‘Angler Access’ sign on on sign Access’ ‘Angler Game & Fish a see you until 3.3km for Road the from map detailed more a get to this Scan Road (this is sign posted as “Kahutara Canoes”). Follow Pahuatea Pahuatea Follow Canoes”). “Kahutara as posted sign is (this Road When travelling south along Kahutara Road, turn left onto Pahuatea Pahuatea onto left turn Road, Kahutara along south travelling When 13) Pahautea Road Access Road Pahautea 13) ACCESS POINTS ACCESS www.fishandgame.org.nz fishing is an excellent way to catch fish here. fish catch to way excellent an is fishing Telephone: 06 359 0409 359 06 Telephone: fishing in our region is found here with fish up to 2kg caught. Bait Bait caught. 2kg to up fish with here found is region our in fishing Palmerston North Palmerston when sea run brown trout move into the river. Some of the best perch perch best the of Some river. the into move trout brown run sea when P O Box 1325 Box O P Below the Tuhitarata Bridge trolling is popular, especially in autumn autumn in especially popular, is trolling Bridge Tuhitarata the Below LOWER RUAMAHANGA RIVER RUAMAHANGA LOWER on Regi gton in ll We fish the next 1km of river on the true right side of the riverbed. -
Hydrological Monitoring Technical Report
JUNE 2005 Hydrological monitoring technical report Laura Watts Resource Investigations Department Greater Wellington Regional Council Contents 1. Introduction 1 1.1 What is this report about? 1 1.2 Scope of analysis 1 1.3 Report structure 2 2. Pressures on surface water quantity in the Wellington Region 3 2.1 Climate cycles 3 2.1.1 El Nino Southern Oscillation (ENSO) 3 2.1.2 Influences of ENSO on Wellington’s water resources 4 2.1.3 Interdecadal Pacific Oscillation (IPO) 4 2.2 Climate change 6 2.3 Land use change 7 2.4 Abstractive demand 8 2.4.1 Current extent of water allocation and use 8 2.4.2 Trends in demand 13 2.5 Summary points 14 3. Monitoring surface water quantity 16 3.1 Monitoring rainfall 16 3.2 Monitoring river flows and lake levels 16 4. Surface water quantity in the region – on average 20 4.1 Variation across the region 20 4.2 Seasonal variations in water quantity 22 4.3 Summary points 25 5. Surface water quantity 1999 to 2004 26 5.1 Annual rainfall 26 5.2 Monthly rainfall and river flows 27 5.2.1 Kapiti Coast 27 5.2.2 Central Wellington Region 29 5.2.3 Wairarapa 31 5.3 Low flows 34 5.4 Minimum flows and target lake levels 37 5.5 Floods 40 5.6 Summary points 42 6. Long-term perspective 44 th 6.1 Climate patterns of the 20 century 44 6.2 Trends and variability in annual rainfall 44 6.3 Droughts and low flows 51 6.4 Extreme rainfall and floods 55 6.5 Summary points 61 7. -
Archaeology of the Wellington Conservancy: Wairarapa
Archaeology of the Wellington Conservancy: Wairarapa A study in tectonic archaeology Archaeology of the Wellington Conservancy: Wairarapa A study in tectonic archaeology Bruce McFadgen Published by Department of Conservation P.O. Box 10-420 Wellington, New Zealand To the memory of Len Bruce, 1920–1999, A tireless fieldworker and a valued critic. Cover photograph shows a view looking north along the Wairarapa coastline at Te Awaiti. (Photograph by Lloyd Homer, © Insititute of Geological and Nuclear Sciences.) This report was prepared for publication by DOC Science Publishing, Science & Research Unit; editing by Helen O’Leary and layout by Ruth Munro. Publication was approved by the Manager, Science & Research Unit, Science Technology and Information Services, Department of Conservation, Wellington. All DOC Science publications are listed in the catalogue which can be found on the departmental website http://www.doc.govt.nz © May 2003, New Zealand Department of Conservation ISBN 0–478–22401–X National Library of New Zealand Cataloguing-in-Publication Data McFadgen, B. G. Archaeology of the Wellington Conservancy : Wairarapa : a study in tectonic archaeology / Bruce McFadgen. Includes bibliographical references. ISBN 0-478-22401-X 1. Archaeological surveying—New Zealand—Wairarapa. 2. Maori (New Zealand people)—New Zealand—Wairarapa— Antiquities. 3. Wairarapa (N.Z.)—Antiquities. I. New Zealand. Dept. of Conservation. II. Title. 993.6601—dc 21 ii Contents Abstract 1 1. Introduction 3 2. Geology and geomorphology 6 3. Sources of information 8 4. Correlation and dating 9 5. Off-site stratigraphy in the coastal environment 11 5.1 Sand dunes 12 5.2 Stream alluvium and colluvial fan deposits 13 5.3 Uplifted shorelines 14 5.4 Tsunami deposits 15 5.5 Coastal lagoon deposits 15 5.6 Correlation of off-site stratigraphy and adopted ages for events 16 6. -
Valuing Wetlands Guidance for Valuing the Benefi Ts Derived from Wetland Ecosystem Services De Groot, Stuip, Finlayson, and Davidson 03
Ramsar Technical Reports Ramsar Technical Report No. 3 CBD Technical Series No. 27 Valuing wetlands Guidance for valuing the benefi ts derived from wetland ecosystem services De Groot, Stuip, Finlayson, and Davidson 03 Ramsar Technical Report No. 3 CBD Technical Series No. 27 Valuing wetlands: Guidance for valuing the benefi ts derived from wetland ecosystem services Rudolf de Groot1, Mishka Stuip2, Max Finlayson3, and Nick Davidson4 1 Environmental Systems Analysis Group, Wageningen University, PO Box 47, 6700 AA, Wageningen, The Netherlands. [email protected] 2 Foundation for Sustainable Development FSD, P.O. Box 570, 6700AN, Wageningen, The Netherlands. [email protected] 3 International Water Management Institute, P.O. Box 2075, Colombo, Sri Lanka. m.fi [email protected] 4 Ramsar Convention Secretariat, 28 rue Mauverny, CH-1196 Gland, Switz erland. [email protected] Ramsar Convention Secretariat Gland, Switz erland November 2006 Ramsar Technical Reports Published jointly by the Secretariat of the Convention on Wetlands (Ramsar, Iran, 1971) & the Secretariat of the Convention on Biological Diversity. © Ramsar Convention Secretariat 2006; © Secretariat of the Convention on Biological Diversity 2006 This report should be cited as: De Groot, R.S., Stuip, M.A.M., Finlayson, C.M. & Davidson, N. 2006. Valuing wet- lands: guidance for valuing the benefi ts derived from wetland ecosystem services, Ramsar Technical Report No. 3/CBD Technical Series No. 27. Ramsar Convention Secretariat, Gland, Switz erland & Secretariat of the Convention on Biological Diversity, Montreal, Canada. ISBN 2-940073-31-7. Series editors: Heather MacKay (Chair of Ramsar Scientifi c & Technical Review Panel), Max Finlayson (former Chair of Ramsar Scientifi c & Technical Review Panel) & Nick Davidson (Deputy Secretary General, Ramsar Convention Secretariat). -
Freshwater Conservation Under a Changing Climate
Freshwater conservation under a changing climate Proceedings of a workshop hosted by the Department of Conservation, 10–11 December 2013, Wellington Cover: Whataroa River, south Westland. Photo: Philippe Gerbeaux, DOC. © Copyright September 2016, Department of Conservation, Christchurch. Private Bag 4715 Christchurch Mail Centre, Christchurch 8140. Report prepared by the Publishing Team, National Office, Department of Conservation, Wellington. How to cite this document: Robertson, H.; Bowie, S.; Death, R.; Collins, D. (Eds) 2016: Freshwater conservation under a changing climate. Proceedings of a workshop hosted by the Department of Conservation, 10–11 December 2013, Wellington. Department of Conservation, Christchurch. 87 p. CONTENTS Executive summary 1 1. Introduction 3 1.1 Workshop 3 1.2 References 4 2. Setting the scene 5 2.1 Evidence and projections of climate change 5 2.1.1 Background5 2.1.2 IPCC AR5 working group 1 headlines 5 2.1.3 Evidence showing the effects of anthropogenic climate change 5 2.1.4 Climate change in New Zealand 6 2.1.5 Summary 7 2.1.6 References 7 2.2 Physical changes to New Zealand’s freshwater ecosystems under climate change 9 2.2.1 Introduction 9 2.2.2 Water temperature 9 2.2.3 The water cycle 9 2.2.4 Sediment and channel morphology 11 2.2.5 Indirect effects 11 2.2.6 Uncertainties 11 2.2.7 Implications for freshwater conservation 12 2.2.8 References 12 3. Vulnerability of freshwater ecosystems due to climate change 14 3.1 River ecosystems 14 3.1.1 Background 14 3.1.2 Vulnerability of rivers to climate change -
FINAL Whangamarino Wetland and Willow Control
Review of Whangamarino Wetland vegetation response to the willow control programme (1999 – 2008) NIWA Client Report: HAM2010-010 August 2010 NIWA Project: DOC09204 Review of Whangamarino Wetland vegetation response to the willow control programme (1999 – 2008) K.A. Bodmin P.D. Champion NIWA contact/Corresponding author K.A. Bodmin Prepared for Waikato Area Office, Department of Conservation NIWA Client Report: HAM2010-010 August 2010 NIWA Project: DOC09204 National Institute of Water & Atmospheric Research Ltd Gate 10, Silverdale Road, Hamilton P O Box 11115, Hamilton, New Zealand Phone +64-7-856 7026, Fax +64-7-856 0151 www.niwa.co.nz All rights reserved. This publication may not be reproduced or copied in any form without the permission of the client. Such permission is to be given only in accordance with the terms of the client's contract with NIWA. This copyright extends to all forms of copying and any storage of material in any kind of information retrieval system. Contents Executive Summary iv 1. Introduction 1 1.1 Whangamarino Wetland 2 2. Previous reports 4 2.1 Whangamarino Wetland vegetation communities 4 2.2 Whangamarino River northern bank transects (Champion, 2006) 5 2.3 Vegetation monitoring 1993 to 2003 (Reeves, 2003) 6 2.4 Sedge restoration monitoring (Champion annual reports 1999 to 2003) 7 3. Methods 8 3.1 Time series vegetation maps 8 3.2 DOC staff interview 8 3.3 Previously collected data 8 3.4 Site visits 9 3.5 Analysis of data 9 4. Results 12 4.1 Aerial spray programme for Salix species 12 4.2 2009 site descriptions for untreated and treated areas 19 4.3 Site descriptions for helicopter accessed locations 30 4.3.1 Southern peat bog 30 4.3.2 Reao peat bog 33 4.4 Vegetation maps and willow spread from 1942 to 2008 35 4.5 Vegetation types based on PRIMER results 42 4.5.1 Willow cover included 42 4.5.2 Willow cover excluded 46 4.5.3 Influence of willow on PRIMER vegetation types 46 5. -
Economic Values of the World's Wetlands
Living Waters Conserving the source of life The Economic Values of the World’s Wetlands Prepared with support from the Swiss Agency for the Environment, Forests and Landscape (SAEFL) Gland/Amsterdam, January 2004 Kirsten Schuyt WWF-International Gland, Switzerland Luke Brander Institute for Environmental Studies Vrije Universiteit Amsterdam, The Netherlands Table of Contents 4 Summary 7 Introduction 8 Economic Values of the World’s Wetlands 8 What are Wetlands? 9 Functions and Values of Wetlands 11 Economic Values 15 Global Economic Values 19 Status Summary of Global Wetlands 19 Major Threats to Wetlands 23 Current Situation, Future Prospects and the Importance of Ramsar Convention 25 Conclusions and Recommendations 27 References 28 Appendix 1: Wetland Sites Used in the Meta-Analysis 28 List of 89 Wetland Sites 29 Map of 89 Wetland Sites 30 Appendix 2: Summary of Methodology 30 Economic Valuation of Ecosystems 30 Meta-analysis of Wetland Values and Value Transfer Left: Water lilies in the Kaw-Roura Nature Reserve, French Guyana. These wetlands were declared a nature reserve in 1998, and cover area of 100,000 hectares. Kaw-Roura is also a Ramsar site. 23 ©WWF-Canon/Roger LeGUEN Summary Wetlands are ecosystems that provide numerous goods and services that have an economic value, not only to the local population living in its periphery but also to communities living outside the wetland area. They are important sources for food, fresh water and building materials and provide valuable services such as water treatmentSum and erosion control. The estimates in this paper show, for example, that unvegetated sediment wetlands like the Dutch Wadden Sea and the Rufiji Delta in Tanzania have the highest median economic values of all wetland types at $374 per hectare per year. -
Resilient Wetlands Research Programme Update 7: July 2017 to June 2018
Resilient Wetlands Research Programme Update 7: July 2017 to June 2018 Bev Clarkson, Dave Campbell, Yvonne Taura, Chris Tanner Overview Our Resilient Wetlands research programme is funded by the Strategic Science Investment Fund (SSIF) Crown Research Institutes from the Ministry of Business, Innovation and Employment's Science and Innovation Group (previously ‘core’ funding). The following update summarises the major outputs and successes between July 2017 and June 2018. O tu Wharekai wetlands relatively resilient to N-loading in the short term. Our 3-year fertiliser (N, P) experiment in a montane fen to determine the vulnerability of natural wetlands to agricultural inputs has now been completed. Olivia Burge led the data analysis and write-up of the journal paper, which has just been submitted. The catchment, on the foothills of the Southen Alps, is largely intact, with very low atmospheric nitrogen inputs. We found little evidence of community-level change after 3 years of nutrient addition, aside from increasing dominance in cover of the most abundant canopy species and decreases in species richness, in the highest N treatment (both nitrate-N and ammonium-N) plots. Species richness decreases were due to losses of both native and exotic species. Further work is required to assess the longer-term resilience of New Zealand wetlands to agricultural losses of N and P, the impacts of which have largely gone unstudied. Final harvesting of a total of 8 replicated plots each of Schoenus (left), Carex (right), and Chionochloa (not shown) communities at O Tu Wharekai after 3 years fertilization with either nitrate-N, ammonium-N and phosphate-P alone or in combination.