Environment Canterbury
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Wrybill <I>Anarhynchus Frontalis</I>: a Brief Review of Status, Threats and Work in Progress
The Wrybill Anarhynchus frontalis: a brief review of status, threats and work in progress ADRIAN C. RIEGEN '1 & JOHN E. DOWDING 2 •231 ForestHill Road, Waiatarua, Auckland 8, NewZealand, e-maih riegen @xtra.co. nz; 2p.o. BOX36-274, Merivale, Christchurch 8030, New Zealand, e-maih [email protected]. nz Riegen,A.C. & Dowding, J.E. 2003. The Wrybill Anarhynchusfrontalis:a brief review of status,threats and work in progress.Wader Study Group Bull. 100: 20-24. The Wrybill is a threatenedplover endemic to New Zealandand unique in havinga bill curvedto the right.It is specializedfor breedingon bareshingle in thebraided riverbeds of Canterburyand Otago in the SouthIsland. After breeding,almost the entirepopulation migrates north and wintersin the harboursaround Auckland. The speciesis classifiedas Vulnerable. Based on countsof winteringflocks, the population currently appears to number4,500-5,000 individuals.However, countingproblems mean that trendsare difficult to determine. The mainthreats to theWrybill arebelieved to be predationon thebreeding grounds, degradation of breeding habitat,and floodingof nests.In a recentstudy in the MackenzieBasin, predation by introducedmammals (mainly stoats,cats and possibly ferrets) had a substantialimpact on Wrybill survivaland productivity. Prey- switchingby predatorsfollowing the introductionof rabbithaemorrhagic disease in 1997 probablyincreased predationrates on breedingwaders. A recentstudy of stoatsin the TasmanRiver showedthat 11% of stoat densexamined contained Wrybill remains.Breeding habitat is beinglost in somerivers and degraded in oth- ers,mainly by waterabstraction and flow manipulation,invasion of weeds,and human recreational use. Flood- ing causessome loss of nestsbut is alsobeneficial, keeping nesting areas weed-free. The breedingrange of the speciesappears to be contractingand fragmenting, with the bulk of the popula- tion now breedingin three large catchments. -
Basemap Using the NZ Digital River Network
Building a Hydrologic Base Map Prepared by David R. Maidment Waterways Centre for Freshwater Research University of Canterbury 14 March 2018 Goals of the Exercise This exercise shows how to develop a hydrologic base map for a catchment showing the catchment boundary and the rivers and streams within it. This is done in two ways – for the Rakaia river in Canterbury using the NZ Digital River Network, and for the Puriri river catchment in Papua-New Guinea using ArcGIS Online ready to use Hydro Services. Computer and Data Requirements To carry out this exercise, you need to have a computer, which runs ArcGIS Desktop version 10.5. This exercise will also work with version 10.4.1 if you do not have access to Version 10.5. You will need a login and password for the University of Canterbury Organizational Account for ArcGIS Online. Part One: Basemap using the NZ Digital River Network Check out information about the New Zealand Digital River Network, or REC (River Environment Classification) at https://www.niwa.co.nz/freshwater-and-estuaries/management- tools/river-environment-classification-0 You can download a copy of the dataset for all of New Zealand at: https://www.niwa.co.nz/static/web/nzRec2_v4.gdb.zip This is a 487 MB file, so you need a good Wifi connection or wired internet connection to do this. When you uncompress this file, it looks like this The nzRec2_V4.gdb is a 2.2 GB geodatabase covering all of New Zealand. If you have the full REC database and you open ArcMap and look at the REC Geodatabase, below is what you see. -
Station to Station Station to Station
Harper Road, Lake Coleridge R.D.2 Darfield, Canterbury PH: 03 318 5818 FAX: 03 318 5819 FREEPHONE: 0800 XCOUNTRY (0800 926 868) GLENTHORNE GLENTHORNE STATION STATION EMAIL: [email protected] WEBSITE: www.glenthorne.co.nz STATION TO STATION GLENTHORNE STATION STATION TO STATION SELF DRIVE 4WD ADVENTURES CHRISTCHURCH SELF DRIVE 4WD ADVENTURES THE ULTIMATE HIGH COUNTRY EXPERIENCE LAKE COLERIDGE NEW ZEALAND 5 days and 6 nights Tracks can be varied to suit experience levels TOUR START OXFORD AMBERLEY and part trips are available. GLENTHORNE STATION 1 Accommodation is provided along with LAKE COLERIDGE dinner and breakfast. KAIAPOI Plenty of time for walking, fishing, mountain biking, DARFIELD MT HUTT 77 CHRISTCHURCH swimming and photography. METHVEN Daily route book supplied on arrival. Season runs from January to March. 1 LINCOLN Tracks are weather dependant however there are RAKAIA alternative routes, if a section is not available. Traverse the high country from “Station to Station” ASHBURTON CONTACT US FOR A FREE INFORMATION PACK through some of the South Islands remotest areas 0800 XCOUNTRY [0800 926 868] in your own 4WD. PH: 03 318 5818 Starting north of the Rakaia River at FAX: 03 318 5819 Glenthorne Station on the shores of Lake Coleridge, the trail winds its way via formed station tracks EMAIL: [email protected] interlinked by back country roads and finishing in WEBSITE: www.glenthorne.co.nz Otago’s lake district. Harper Road, Lake Coleridge R.D.2 Darfield, Canterbury PH: 03 318 5818 FAX: 03 318 5819 GLENTHORNE FREEPHONE: 0800 XCOUNTRY (0800 926 868) STATION EMAIL: [email protected] LAKE COLERIDGE NEW ZEALAND WEBSITE: www.glenthorne.co.nz GLENTHORNE STATION STATION TO STATION SELF DRIVE 4WD ADVENTURES Starting north of the Rakaia at Lake Coleridge the trail winds Your Station to Station adventure begins at Glenthorne Station, THE ULTIMATE HIGH COUNTRY EXPERIENCE its way via formed station tracks and back country roads. -
Modeling Regional Coastal Evolution in the Bight Of
MODELING REGIONAL COASTAL EVOLUTION IN THE BIGHT OF BENIN, GULF OF GUINEA, WEST AFRICA Ondoa Gregoire Abessolo, Magnus Larson, Rafael Almar, Bruno Castelle, Edward Anthony, Johan Reyns To cite this version: Ondoa Gregoire Abessolo, Magnus Larson, Rafael Almar, Bruno Castelle, Edward Anthony, et al.. MODELING REGIONAL COASTAL EVOLUTION IN THE BIGHT OF BENIN, GULF OF GUINEA, WEST AFRICA. Coastal Sediments’19, May 2019, Tampa, United States. 10.1142/9789811204487_0178. hal-02394959 HAL Id: hal-02394959 https://hal.archives-ouvertes.fr/hal-02394959 Submitted on 11 Dec 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. MODELING REGIONAL COASTAL EVOLUTION IN THE BIGHT OF BENIN, GULF OF GUINEA, WEST AFRICA ONDOA GREGOIRE ABESSOLO1,2, MAGNUS LARSON3, RAFAEL ALMAR1, BRUNO CASTELLE4, EDWARD J. ANTHONY5, J. REYNS6,7 1. LEGOS, OMP, UMR 5566 (CNRS/CNES/IRD/Université de Toulouse), 14 Avenue Edouard Belin, 31400, Toulouse, France. [email protected], [email protected]. 2. Ecosystems and Fisheries Resources Laboratory, University of Douala, BP 2701, Douala, Cameroun. 3. Department of Water Resources Engineering, Lund University, Box 118, S-221 00, Lund, Sweden. [email protected]. 4. EPOC, OASU, UMR 5805 (CNRS - Université de Bordeaux), Allée Geoffroy Saint- Hilaire – CS 50023 – 33615, Pessac Cedex, France. -
Island Wakes in the Southern California Bight R
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 110, C11012, doi:10.1029/2004JC002675, 2005 Island wakes in the Southern California Bight R. M. A. Caldeira,1,2 P. Marchesiello,3 N. P. Nezlin,4 P. M. DiGiacomo,5 and J. C. McWilliams3 Received 19 August 2004; revised 21 February 2005; accepted 14 June 2005; published 18 November 2005. [1] Wind- and current-induced island wakes were investigated using a multiplatform approach of in situ, remote sensing, and numerical model simulations for the Southern California Bight (SCB). Island wind wakes are a result of sheltering from the wind, with weak wind mixing, strong heat storage, and consequent high sea surface temperature (SST). Wind wakes around Santa Catalina Island are most persistent during spring and summer months. Current wakes, caused by the disruption of the poleward traveling California Countercurrent, induce eddies to form off the north end of Catalina Island, and these move poleward every 9–12 days. Current wake eddies induce strong mixing, with low SST and high-density sea surface signatures, whereas wind wakes induce high sea surface temperature signatures associated with the formation of a well-defined shallow thermocline. Current wake eddies vary from 1 to 30 km in diameter. From numerical solutions we predicted the frequency of occurrence of current-induced wakes off Santa Catalina Island. Wind wakes were also observed off all the other islands of the SCB as seen from the analysis of synthetic aperture radar data. Time series analysis of the island mass effect phenomenon has shown a concurrence of low SST and high sea surface chlorophyll for Santa Catalina, San Nicholas, and San Clemente islands that might be related to the seasonality of the California Current and California Countercurrent. -
Science for Solutions
Science for Solutions NOAA COASTAL OCEAN PROGRAM Decision Analysis Series No. 15 Characterization of Hypoxia Topic 1 Report for the Integrated Assessment on Hypoxia in the Gulf of Mexico Nancy N. Rabalais, R. Eugene Turner, Dubravko Justic´, Quay Dortch, and William J. Wiseman, Jr. May 1999 U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Ocean Service Coastal Ocean Program GULF OF MEXICO HYPOXIA ASSESSMENT This report is the first in a series of six reports developed as the scientific basis for an integrated assessment of the causes and consequences of hypoxia in the Gulf of Mexico, as requested by the White House Office of Science and Technology Policy and as required by Section 604a of P.L. 105-383. For more information on the assessment and the assessment process, please contact the National Centers for Coastal Ocean Science at (301) 713-3060. DECISION ANALYSIS SERIES The Decision Analysis Series has been established by NOAA's Coastal Ocean Program (COP) to present documents for coastal decision mak- ers which contain analytical treatments of major issues or topics. The is- sues, topics, and principal investigators have been selected through an extensive peer review process. To learn more about the COP or the De- cision Analysis Series, please write to: NOAA National Centers for Coastal Ocean Science Coastal Ocean Program 1315 East-West Highway, Room 9700 Silver Spring, Maryland 20910 phone: 301-713-3338 fax: 301-713-4044 web: http://www.cop.noaa.gov e-mail: [email protected] Cover image: Extent of bottom water with dissolved oxygen less than 2 mg/l for July 1996 (based on data of Rabalais, Turner, and Wiseman). -
Introduction Getting There Places to Fish Methods Regulations
3 .Cam River 10. Okana River (Little River) The Cam supports reasonable populations of brown trout in The Okana River contains populations of brown trout and can the one to four pound size range. Access is available at the provide good fishing, especially in spring. Public access is available Tuahiwi end of Bramleys Road, from Youngs Road which leads off to the lower reaches of the Okana through the gate on the right Introduction Lineside Road between Kaiapoi and Rangiora and from the Lower hand side of the road opposite the Little River Hotel. Christchurch City and its surrounds are blessed with a wealth of Camside Road bridge on the north-western side of Kaiapoi. places to fish for trout and salmon. While these may not always have the same catch rates as high country waters, they offer a 11. Lake Forsyth quick and convenient break from the stress of city life. These 4. Styx River Lake Forsyth fishes best in spring, especially if the lake has recently waters are also popular with visitors to Christchurch who do not Another small stream which fishes best in spring and autumn, been opened to the sea. One of the best places is where the Akaroa have the time to fish further afield. especially at dusk. The best access sites are off Spencerville Road, Highway first comes close to the lake just after the Birdlings Flat Lower Styx Road and Kainga Road. turn-off. Getting There 5. Kaiapoi River 12. Kaituna River All of the places described in this brochure lie within a forty The Kaiapoi River experiences good runs of salmon and is one of The area just above the confluence with Lake Ellesmere offers the five minute drive of Christchurch City. -
New York Bight
NEW YORK BIGHT RESTORATION PLAN REPORT TO CONGRESS NEW YORK BIGHT RESTORATION PLAN FINAL REPORT MARCH 1993 A PRODUCT ,.·F THE NEW YORK-NEW JERSa:'. 1j;U>\RY PROGR/,.� MANAGEMENT cu;·:�·.:RENCE TABLE OF CONTENTS EXECUTIVE SUMMARY S-1 Use Impairments and Precipitating Pollutant Factors S-1 Floatable Debris S-2 Pathogen Contamination S-2 Toxic Contamination S-3 Nutrient and Organic Enrichment S-4 Habitat Loss and Degradation S-5 Program Administration S-5 INTRODUCTION 1 General 1 Congressional Mandate 1 Prior Reports and Activities 2 Preliminary Problem Assessment 3 RESTORATION PLAN MODULES 4 Floatable Debris 5 Introduction 5 Short-term Floatables Action Plan 5 Comprehensive Floatables Plan 6 Independent Activities and Public Education 7 MARPOL Annex V 7 Recycling and Waste Reduction 8 Program Constraints 8 Program Follow-Up 9 Pathogen Contamination 9 Introduction 9 Beach/Shellfish Bed Closure Action Plan 9 Ocean Dumping Ban Act 10 Combined Sewer Overflow (CSO) Abatement Program 10 Alternative Pathogenic Indicator Study 10 Program Constraints 11 Program Follow-Up 11 3. Toxic Contamination 11 Introduction 11 Problem Characterization 12 Total Maximum Daily Load/Wasteload Allocation (TMDL/WLA) 13 Antidegradation 14 TABLE OF CONTENTS (cont.) Toxic Contamination (cont.) Dredged Material Management 14 Ecosystem Indicators 16 Other Existing Programs and Authorities 16 Program Constraints and Follow-Up 17 Nutrient and Organic Enrichment 17 Introduction 17 Problem Characterization 17 Eutrophication Modeling 18 Ecosystem Indicators 18 Program Constraints and Follow-Up 19 5. Habitat Loss and Degradation 19 Introduction 19 Habitat Inventory 19 Regulatory Programs 20 Non-Regulatory Approach 20 Geographic Targeting 20 Program Constraints 20 Program Follow-Up 21 A Comprehensive Focus 21 Program Administration 22 LIST OF FIGURES Figure 1 - The New York Bight 2 Figure 2 - The New York-New Jersey Harbor 3 Figure 3 - Management Conference Membership and Structure 5 ATTACHMENTS 1. -
Survival of Chinook Salmon, Oncorhynchus Tshawytscha, from A
812 Abstract.-To characterize the im Survival of chinook salmon, pact ofspring floods on the survival of juvenile chinook salmon in the un Oncorhynchus tshawytscha, from a stable, braided rivers on the east coast ofNew Zealand's South Island, I exam spawning tributary of the Rakaia Rivet. ined correlations between spring and summer flows in the mainstem of the New Zealand, in relation to spring and Rakaia River and fry-to-adult survival for chinook salmon spawningin a head summer mainstem flows water tributary. Flow parameters that were investigated included mean flow, maximum flow, and the ratio of mean Martin J. Unwin to median flow (an index of flow vari National Institute of Water and Atmospheric Research (NIWA) ability), calculated during peak down PO Box 8602, Christchurch, New Zealand river migration ofocean-type juveniles (August to January). Survival was E-mail address:[email protected] uncorrelated with mean or maximum flow but was positively correlated with the ratio of mean to median flow dur ing spring (October and November). The correlation suggests that pulses of suits can be derived (Kope and Bots freshwater entering the ocean during To understand the population dy floods may butTer the transition offin namics of anadromous Pacific ford, 1990). gerlings from fresh to saline waters and salmonids <Oncorhynchus spp.), it Despite the importance of in thus partly compensate for the lack of is important to isolate and charac stream habitats for rearingjuvenile an estuary on the Rakaia River. A posi terize the influence of varying en chinook salmon <0. tshawytscha), tive correlation between spring flow variability and the proportion ofocean vironmental factors on annual pro the relation betweenflow and brood type chinook in relation to stream-type duction. -
Application for Resource Consent, Upper Rangitata River
Application for resource consent, Upper Rangitata River Section 95A of the Resource Management Act 1991 The Ashburton and Timaru District Councils have received the following applications for resource consent: Applicant: Braided River Jet Boating Ltd Address for Service: Ronald Clearwater, Braided River Jet Boating Ltd, 201 Geraldine – Arundel Road, RD22, Geraldine 7922 or by email at [email protected] Application number(s): LUC18/0094 & 102.2108.224 Location: Upper Rangitata River Details of proposed activity: Resource consent is sought to operate a commercial jet boat activity on the Rangitata River. The Rangitata River represents the boundary between the Ashburton and Timaru Districts and as such resource consent has been sought from both Councils. The two Councils are processing the applications as a joint process similarly to as if there was one application. It is proposed to operate a six person jet boat on the river (1 driver plus 5 guests) for up to a maximum of four trips per day with an overall cap of 480 trips per year. The activity will operate during daylight hours (up to a maximum of between 7am and 7pm), seven days a week. The activity will operate on the upper reaches of the Rangitata River and activities will be limited to from the top of the Rangitata Gorge up to the confluence of the Havelock and Clyde rivers. It is noted that the river includes various branches within this area and as part of this the activity will go up to the confluence point but will also travel up another arm of the river up to the Deep Creek area towards Mount Sunday. -
The Glacial Sequences in the Rangitata and Ashburton Valleys, South Island, New Zealand
ERRATA p. 10, 1.17 for tufts read tuffs p. 68, 1.12 insert the following: c) Meltwater Channel Deposit Member. This member has been mapped at a single locality along the western margin of the Mesopotamia basin. Remnants of seven one-sided meltwater channels are preserved " p. 80, 1.24 should read: "The exposure occurs beneath a small area of undulating ablation moraine." p. 84, 1.17-18 should rea.d: "In the valley of Boundary stream " p. 123, 1.3 insert the following: " landforms of successive ice fluctuations is not continuous over sufficiently large areas." p. 162, 1.6 for patter read pattern p. 166, 1.27 insert the following: " in chapter 11 (p. 95)." p. 175, 1.18 should read: "At 0.3 km to the north is abel t of ablation moraine " p. 194, 1.28 should read: " ... the Burnham Formation extends 2.5 km we(3twards II THE GLACIAL SEQUENCES IN THE RANGITATA AND ASHBURTON VALLEYS, SOUTH ISLAND, NEW ZEALAND A thesis submitted in fulfilment of the requirements for the Degree of Doctor of Philosophy in Geography in the University of Canterbury by M.C.G. Mabin -7 University of Canterbury 1980 i Frontispiece: "YE HORRIBYLE GLACIERS" (Butler 1862) "THE CLYDE GLACIER: Main source Alexander Turnbull Library of the River Clyde (Rangitata)". wellington, N.Z. John Gully, watercolour 44x62 cm. Painted from an ink and water colour sketch by J. von Haast. This painting shows the Clyde Glacier in March 1861. It has reached an advanced position just inside the remnant of a slightly older latero-terminal moraine ridge that is visible to the left of the small figure in the middle ground. -
Island Wakes in the Southern California Bight R.M
Island wakes in the Southern California Bight R.M. Caldeira, P. Marchesiello, N. Nezlin, P. Digiacomo, J. C. Mcwilliams To cite this version: R.M. Caldeira, P. Marchesiello, N. Nezlin, P. Digiacomo, J. C. Mcwilliams. Island wakes in the Southern California Bight. Journal of Geophysical Research. Oceans, Wiley-Blackwell, 2005, 110, pp.C11012. 10.1029/2004JC002675.. hal-00280338 HAL Id: hal-00280338 https://hal.archives-ouvertes.fr/hal-00280338 Submitted on 19 Feb 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 110, C11012, doi:10.1029/2004JC002675, 2005 Island wakes in the Southern California Bight R. M. A. Caldeira,1,2 P. Marchesiello,3 N. P. Nezlin,4 P. M. DiGiacomo,5 and J. C. McWilliams3 Received 19 August 2004; revised 21 February 2005; accepted 14 June 2005; published 18 November 2005. [1] Wind- and current-induced island wakes were investigated using a multiplatform approach of in situ, remote sensing, and numerical model simulations for the Southern California Bight (SCB). Island wind wakes are a result of sheltering from the wind, with weak wind mixing, strong heat storage, and consequent high sea surface temperature (SST).