DOCSLIB.ORG

Gypsey Race Driffield Show Another Small Winterbourne Stream There Is No Angling Interest on This Rising Near Kirkby Grindalythe and Flows Stream

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

EAST YORKSHIRE CHALK RIVERS TRUST Newsletter No 2 - April 2008 Educational Trustees New appointment Package Due to boundary changes within the At the AGM in January 2007 the Environment Agency we have reluctantly board elected Simon Johnson as its As part of a Leader+ grant, David Croft had to accept the resignation of Karen Tait Chairman. Simon originally worked has researched and produced an from the Trust Board. Karen has been a for the Environment Agency (EA) in Education Package for the Trust. useful contact with the EA and greatly Norfolk. He has worked as a private Since the Education Package was assisted in the provision of data for use in consultant before gaining his launched at the Driffield Agricultural Show drawing up our Catchment Overview. present post with the Wild Trout it has received great interest among local Trust (WTT) as Director. and regional schools and colleges. His experience in the aquatic Sample CD Rom copies have been environmental field will be of great provided and feedback has been benefit to the Trust in his new role requested. Contact the Trust if you are as Chairman. involved in education and a trial copy will be provided. East Yorkshire Chalk Rivers Trust 1 Newsletter 02.pmd 1 08/07/2008, 11:12 Elmswell Beck A weir was removed from this small stream in January. The weir was becoming unsafe and was causing erosion to the banks of this stream and was a barrier to migrating fish. This work was undertaken in partnership with the EA providing plant and machinery. The East Yorkshire Chalk Rivers Trust (EYCRT) reinstated the bank and created important habitat from much of the woody debris found on site. Cinderella Chalk Stream Projects Kings Mill The Wild Trout Trust sponsored a visit to a Public use of this popular local footpath alongside the Elmswell Beck is causing section of West Beck where the East concern and the gross erosion of the bank is resulting in soil entering the stream. Yorkshire Chalk Rivers Trust had identified The Trust gave a presentation to the Driffield Town Council discussing the various habitat problems. These were due to options for the repair and maintenance of the river bank. previous maintenance and stock grazing The Council are to investigate the possibility of claiming the land as the present that had caused over widening of the river. owner cannot be found. A report has been received from Vaughan Lewis of Windrush AEC Ltd. highlighting remedial action and suggesting various Water Forlorns long-term solutions to the problems. The Rivers Trust has decided to take up the We have also received a WTT report concerning this small stream that runs through recommendations in the report and is in Driffield town centre. The proposals are to enhance the natural features of the stream by the process of consultation with the the use of soft engineering techniques. Environment Agency (EA). The report has been presented to the Town Council and if accepted, the Trust will Natural England (NE) is broadly in bid for the necessary funding and involve the local community in the improvements. support of the scheme and the fine detail is being discussed at the present moment. An application is being made for funding Foston Beck & of the scheme. Mires Beck This small chalk-fed stream rises in West Beck Newbald and flows south towards A proposal is being developed to set back Ellerker before joining the Humber at several areas of floodbank. Brough. Discussions are taking place between Bishop Burton College are the Trust, EA, NE and the riparian owners continuing to work on this stream in a bid to create a wider flood channel. under the guidance of the Trust. This This will enable the creation of reed bed ongoing partnership is providing a and wet woodland along these major vast amount of field work opportunity chalk streams. for the Countryside Management A 200mtr. section of the Foston Beck students at this agricultural college. has been improved in partnership with the EA. This project involved the creation of a meandering channel and enhancement of 2007 Projects the bankside habitat. Gypsey Race Driffield Show Another small winterbourne stream There is no angling interest on this rising near Kirkby Grindalythe and flows stream. However, it has the potential of & Wolds east to the resort of Bridlington. providing an important aquatic interest The stream has been subject to a to this most northerly of Yorkshire chalk planning application by a major gas streams. Country Fair storage company. The public enquiry determined that several thousand The Trust once again attended the Show pounds should be put towards on the Driffield Showground. Also this improvements to the stream and year a display was undertaken at a new surrounding habitat in mitigation for the event at Sledmere House. damage that may be caused by the A lot of interest was shown by the proposed works on this small stream. An public in the work of the Trust. electro-fishing survey has been carried out by the Environment Agency to determine the status of the fish population. Only sticklebacks, eels and minnows were found during the surveys. 2 East Yorkshire Chalk Rivers Trust Newsletter 02.pmd 2 08/07/2008, 11:12 Partnership Projects VIEW FROM THE The Trust is working with the East Riding Fisheries Consultative Association to develop fish havens on the lower River RIVERBANK Hull at Eske. Designs have been drawn up and riparian owners are being contacted by this angler-led group. The last year has certainly been a out. New temporary homes and patches We have again worked with the Bishop challenging one as far as wildlife goes. As of high ground would have been found Burton College in assisting their Fishery I write this, memories of the devastating and it is only now that they return to their Management students in gaining valuable floods come back to me. Thousands of old haunts. experience with practical field work acres of rural land was inundated for as Numbers of water voles do appear to projects. long as six weeks in some areas. The have taken a downturn and more effects on wildlife will have been immense, worryingly, we have had reports of but it is only now that we can start to look American mink turning up in areas where at those effects. they weren’t present before the floods. Just as we moved into the New Year The huge lake that formed in June last we had a second bout of flooding, which year will have provided an ideal went largely unreported, but much of the opportunity for them to simply swim into wildlife will have taken a second battering new areas preying on native wildlife as just as we were moving towards another they arrived. Mink are particularly bad breeding season. news as they will slowly decimate The wildlife of the riverbank has a numbers of water voles, waterfowl and remarkable way of recovering after such ground nesting birds as well as taking events, but it is likely to take two or three large numbers of fish from the waterways. breeding seasons to return to some sort of The year ahead is a testing time for the ‘normality’. Early signs for species like the animals along our riverbanks, but with water vole and kingfisher are that they are time and more settled, ‘normal’ summer still paddling around our waterways or weather combined with continued support whizzing along the bank top in search of from positive management by landowners favourite nesting and feeding areas. Many we will hopefully continue to see ratty and kingfisher nest holes were lost and his friends as they go about their daily similarly many water vole burrows flooded business. Jon Traill - Trustee - June 2008 Students from Bishop Burton College recently carrying out fishery work on an East Yorkshire chalk stream BAP Steering Group for Chalk Rivers – Flooded out !! West Beck flooded for a second time in January 2008 after the 2007 Meeting June 2007 floods. A presentation was made to the Biodiversity Action Plan Steering Group at their Winchester meeting. The Group is The water vole was one of many made up of a wide area of expertise within species affected by the flooding the country concerned with the events over the last year. management of chalk rivers. The EYCRT represents the most northerly system of chalk rivers in Britain at this forum. East Yorkshire Chalk Rivers Trust 3 Newsletter 02.pmd 3 08/07/2008, 11:13 Riverfly Monitoring Partnership Following a recent workshop given by the Natural History Museum, a group of interested fly fishermen have been formed into a monitoring group. The group will cover many of the chalk streams and rivers in the area. The monthly monitoring programme is being developed by the Trust and the EA’s Ecological Appraisal Officer. The group will be able to identify any water quality problems as they arise and have a contact with the EA to enable a rapid response. The group collecting live samples Examining and identifying the samples Driffield’s brown trout population to benefit from weir transformation The population of brown trout in Water material was used to narrow the stream to Forlorns in Driffield has received a boost create a bed suitable for the establishment thanks to the hard work of the East of marginal plants.” Yorkshire Chalk Rivers Trust and students “The resulting faster flow past this from Bishop Burton College. section would then remove the silt The fish, whose natural spawning deposits and improve habitat.” grounds are located just upstream from The back of the new weir was built the weir near the Exchange Street Bridge, higher than the rest and as the water flows were prevented from reaching the though the high, narrow channel that has grounds by the original construction, been created, a scour forms, which keeps which was too high and too deep for them the gravel immediately downstream of the to swim over.
Recommended publications
  • U DDBA Papers of the Barnards Family 1401-1945 of South Cave

    U DDBA Papers of the Barnards Family 1401-1945 of South Cave

    Hull History Centre: Papers of the Barnards Family of South Cave U DDBA Papers of the Barnards Family 1401-1945 of South Cave Historical background: The papers relate to the branch of the family headed by Leuyns Boldero Barnard who began building up a landed estate centred on South Cave in the mid-eighteenth century. His inherited ancestry can be traced back to William and Elizabeth Barnard in the late sixteenth century. Their son, William Barnard, became mayor of Hull and died in 1614. Of his seven sons, two of them also served time as mayor of Hull, including the sixth son, Henry Barnard (d.1661), through whose direct descendants Leuyns Boldero Barnard was eventually destined to succeed. Henry Barnard, married Frances Spurrier and together had a son and a daughter. His daughter, Frances, married William Thompson MP of Humbleton and his son, Edward Barnard, who lived at North Dalton, was recorder of Hull and Beverley from the early 1660s until 1686 when he died. He and his wife Margaret, who was also from the Thompson family, had at least seven children, the eldest of whom, Edward Barnard (d.1714), had five children some of whom died without issue and some had only female heirs. The second son, William Barnard (d.1718) married Mary Perrot, the daughter of a York alderman, but had no children. The third son, Henry Barnard (will at U DDBA/14/3), married Eleanor Lowther, but he also died, in 1769 at the age of 94, without issue. From the death of Henry Barnard in 1769 the family inheritance moved laterally.
  • Sea Trout Smolts in the Gypsey Race

    Sea Trout Smolts in the Gypsey Race

    EAST YORKSHIRE CHALK RIVERS TRUST Newsletter 4 - June 2010 NEW EYCRT LOGO Sea trout smolts in the Gypsey Race The Trust has adopted a new logo Prior to the annual EA Fisheries shown as follows: team electro-fishing survey in October 2009 at various sites along the Gypsey Race, a walking survey of the river(bed) and isolated pools at Boynton (the river was still dried up above and below Boynton) revealed one interesting pool which was subsequently electro-fished and found to hold 14 small trout of 1+ years indicating they hatched from migratory parent fish in the Gypsey Race. Another first for this enigmatic small northern chalk river! OPERATIOn ‘GYPSEY RAce’ In November 2009 the new YWA water water pipe was laid across the river but at done by hand the following day. The pipeline project taking water from depth using the open cut method in EYCRT has been present throughout Haisthorpe to both Filey and Irton crossed agreement with the Environment Agency. negotiations with the contractors and EA the Gypsey Race at a point just above The actual operation took just one day and to also being on site when the pipe Willow Garth SSSI. The work programme with streambed and bankside restoration was being laid. The Trust is to be was carried out by the contractor for being completed at the end of the day. consulted prior to the final bankside Yorkshire Water, Laing O’Rourke. The Fine tuning of the streambed shaping was restoration taking place in May 2010. PRESEntatION OF A CHEQUE The Trust received a cheque for £571.99 from Laing O’Rourke for assisting with negotiations with the EA in respect of the laying of the new YWA water main across the path of the Gypsey Race, and giving on-site advice especially in respect to seasonal stream flows.
  • River Hull Integrated Catchment Strategy Strategy Document

    River Hull Integrated Catchment Strategy Strategy Document

    River Hull Advisory Board River Hull Integrated Catchment Strategy April 2015 Strategy Document Draft report This Page is intentionally left blank 2 Inner Leaf TITLE PAGE 3 This page is intentionally left blank 4 Contents 1 This Document.............................................................................................................................17 2 Executive Summary ..............................................................................................................18 3 Introduction and background to the strategy ..................................20 3.1 Project Summary .................................................................................................................................... 20 3.2 Strategy Vision ........................................................................................................................................ 20 3.2.1 Links to other policies and strategies .......................................................................................21 3.3 Background .............................................................................................................................................. 22 3.3.1 Location ........................................................................................................................................... 22 3.3.2 Key characteristics and issues of the River Hull catchment ...............................................22 3.3.3 EA Draft River Hull Flood Risk Management Strategy .........................................................26
  • Allocations Document

    Allocations Document

    East Riding Local Plan 2012 - 2029 Allocations Document PPOCOC--L Adopted July 2016 “Making It Happen” PPOC-EOOC-E Contents Foreword i 1 Introduction 2 2 Locating new development 7 Site Allocations 11 3 Aldbrough 12 4 Anlaby Willerby Kirk Ella 16 5 Beeford 26 6 Beverley 30 7 Bilton 44 8 Brandesburton 45 9 Bridlington 48 10 Bubwith 60 11 Cherry Burton 63 12 Cottingham 65 13 Driffield 77 14 Dunswell 89 15 Easington 92 16 Eastrington 93 17 Elloughton-cum-Brough 95 18 Flamborough 100 19 Gilberdyke/ Newport 103 20 Goole 105 21 Goole, Capitol Park Key Employment Site 116 22 Hedon 119 23 Hedon Haven Key Employment Site 120 24 Hessle 126 25 Hessle, Humber Bridgehead Key Employment Site 133 26 Holme on Spalding Moor 135 27 Hornsea 138 East Riding Local Plan Allocations Document - Adopted July 2016 Contents 28 Howden 146 29 Hutton Cranswick 151 30 Keyingham 155 31 Kilham 157 32 Leconfield 161 33 Leven 163 34 Market Weighton 166 35 Melbourne 172 36 Melton Key Employment Site 174 37 Middleton on the Wolds 178 38 Nafferton 181 39 North Cave 184 40 North Ferriby 186 41 Patrington 190 42 Pocklington 193 43 Preston 202 44 Rawcliffe 205 45 Roos 206 46 Skirlaugh 208 47 Snaith 210 48 South Cave 213 49 Stamford Bridge 216 50 Swanland 219 51 Thorngumbald 223 52 Tickton 224 53 Walkington 225 54 Wawne 228 55 Wetwang 230 56 Wilberfoss 233 East Riding Local Plan Allocations Document - Adopted July 2016 Contents 57 Withernsea 236 58 Woodmansey 240 Appendices 242 Appendix A: Planning Policies to be replaced 242 Appendix B: Existing residential commitments and Local Plan requirement by settlement 243 Glossary of Terms 247 East Riding Local Plan Allocations Document - Adopted July 2016 Contents East Riding Local Plan Allocations Document - Adopted July 2016 Foreword It is the role of the planning system to help make development happen and respond to both the challenges and opportunities within an area.
  • Appendix A: Background Cultural Heritage Context

    Appendix A: Background Cultural Heritage Context

    Appendix A: Background Cultural Heritage Context Archaeological Sites The East Riding, and the c.980sqkm selected for the SEA Addendum study area, has been shaped by man’s activities over the past 10,000 years. As a result, the area contains a rich heritage of archaeological sites (both designated and non-designated), dating from the early prehistoric periods to the 20th century, which reflect the region’s varied social and economic history. The Prehistoric Periods (up to c.700 BC) The earliest phases of prehistoric occupation are generally characterised by an increasing exploitation of the natural landscape and its resources. Artefactual evidence suggests that there was a human presence in Holderness during the Palaeolithic period, and several sites have been identified within the River Hull corridor; one flint-working site at Brigham was excavated in 1962-63 in advance of gravel extraction. Climatic improvements after the Devensian ice age led to the re- establishment of forests, and plants and animals became available for exploitation. While Holderness saw some transient human activity in the later Mesolithic period (c.8300-4000 BC), there was also a significant population on the Wolds, centred on ‘activity areas’ associated with ponds and springs. The number and density of sites on the Wolds implies that this higher land was well-populated during the subsequent Neolithic period (c.4000-2500 BC). Although initially a pastoral society, the gradual introduction of grain crops resulted in a more widespread mixed agricultural regime. The construction of large communal burial mounds as well as other sacred or ritual sites, such as henges, cursus and mortuary enclosures, suggests that there was an organised, community-based society.
  • NRFA Peak Flow Dataset

    NRFA Peak Flow Dataset

    National River Flow Archive NERC Centre for Ecology & Hydrology WINFAP-FEH DATA FILES VERSION 6 Note on changes from v5 VERSION: 1.0 STATUS: FINAL DATE: FEBRUARY 2018 AUTHOR: KATIE MUCHAN, CATH SEFTON, STEVE TURNER, OLIVER SWAIN DOCUMENT VERSION CONTROL Version Date Author Description 1.0 FEBRUARY KATIE MUCHAN, CATH SEFTON, STEVE 2018 TURNER, OLIVER SWAIN TABLE OF CONTENTS 1 INTRODUCTION ............................................................................................................................................................. 1 2 NETWORK CHANGES ...................................................................................................................................................... 2 2.1 REMOVAL OF GAUGING STATIONS......................................................................................................................................... 2 2.2 ADDITION OF GAUGING STATIONS......................................................................................................................................... 3 2.3 CLOSURE OF GAUGING STATIONS .......................................................................................................................................... 3 2.4 COMBINED PEAK FLOW TIME SERIES FROM MULTIPLE STATIONS ................................................................................................ 3 2.5 COMPONENT STATIONS .....................................................................................................................................................
  • Scalby Beck Project the AMI Scheme Anglers Monitoring Initiative and Beyond!

    Scalby Beck Project the AMI Scheme Anglers Monitoring Initiative and Beyond!

    Scalby Beck Project Scalby Beck is part of the Yorkshire work themselves with the local Trust’s River Derwent. Over 100 years ago a support. All the permissions are in place, man-made channel was cut from the plans have been approved, drawings headwaters of the Derwent to Scalby passed and the club is ready to go ahead Beck to take flood water as required. as soon as low flows allow the work to Scalby Beck discharges into the North progress. The materials to be used are Sea at a point north of Scarborough. As stainless steel brackets and expanding part of the flood relief channel a number bolts – the brackets will be used secure of weirs have been built to manage the oak timbers to the weir creating several energy of the floods. These weirs are a boxes for the fish to negotiate. These barrier to upstream migration for materials are an improvement on what was salmon, sea trout, eels and lampreys. A first used and so should stand up as well to number of years ago the Scalby Beck heavy flows as the original boxes. The Angling Club along with the Agency original pass is still functioning more than built a small wooden fish pass on one 10 years later (see photograph). The of the lower weirs. This is still in place positive thing about these type of materials and has worked well in relieving some is if there is a need for maintenance then of the pressure at a pinch point which is costs can be kept to a minimal.
  • ! National Rivers Authority ! Information Centre '9Ad Office Jass N O

    ! National Rivers Authority ! Information Centre '9Ad Office Jass N O

    NATIONAL RIVERS AUTHORITY YORKSHIRE REGION RIVER FLOW & RAINFALL STATISTICS UPDATED TO 31ST DECEMBER 1992 National Rivers Authority Northumbria & Yorkshire Region Olympia House Gelderd Lane Gelderd Road Leeds LS12 6DD August 1993 ! National Rivers Authority ! Information Centre '9ad Office Jass N o ................. | accession No NATIONAL RIVERS AUTHORITY YORKSHIRE REGION RIVER FLOW AND RAINFALL STATISTICS UPDATED TO 31ST DECEMBER 1992 This publication combines the 1992 annual reports on River Flow Statistics and on Rainfall. It is in two sections:- (i) River Flow Statistics updated to 31st December 1992. (ii) Annual Rainfall Report 1992. IMPORTANT NOTICE The published d^ta are the best available in August 1993. Please consult the Resource Planning and Hydrometry Section about the accuracy of the data, and the possibility of revision, before using these records for detailed investigations. The Section would also be pleased to be notified of any errors which may be discovered. Telephone: Leeds 440191 NRA Northumbria & Yorkshire Region August 1993 RIVER FLOW STATISTICS UPDATED TO 31ST DECEMBER 1992 Introduction This publication contains summary data for 1992 and analyses of long period river flow records. The data should be used with some caution. All the published river flows are "net" or "as measured". No adjustments have been made in respect of abstractions.from, or discharges to, the river upstream of the flow measuring station, or for changes in storage of reservoirs etc. Records allowing for such adjustments are usually available from the appropriate Division of Yorkshire Water pic or from NRA Northumbria and Yorkshire Region Resource Planning and Hydrometry Section. Records have been included for some stations which were designed primarily to measure low flows.
  • English Hundred-Names

    English Hundred-Names

    l LUNDS UNIVERSITETS ARSSKRIFT. N. F. Avd. 1. Bd 30. Nr 1. ,~ ,j .11 . i ~ .l i THE jl; ENGLISH HUNDRED-NAMES BY oL 0 f S. AND ER SON , LUND PHINTED BY HAKAN DHLSSON I 934 The English Hundred-Names xvn It does not fall within the scope of the present study to enter on the details of the theories advanced; there are points that are still controversial, and some aspects of the question may repay further study. It is hoped that the etymological investigation of the hundred-names undertaken in the following pages will, Introduction. when completed, furnish a starting-point for the discussion of some of the problems connected with the origin of the hundred. 1. Scope and Aim. Terminology Discussed. The following chapters will be devoted to the discussion of some The local divisions known as hundreds though now practi­ aspects of the system as actually in existence, which have some cally obsolete played an important part in judicial administration bearing on the questions discussed in the etymological part, and in the Middle Ages. The hundredal system as a wbole is first to some general remarks on hundred-names and the like as shown in detail in Domesday - with the exception of some embodied in the material now collected. counties and smaller areas -- but is known to have existed about THE HUNDRED. a hundred and fifty years earlier. The hundred is mentioned in the laws of Edmund (940-6),' but no earlier evidence for its The hundred, it is generally admitted, is in theory at least a existence has been found.
  • Baseline Report Series: 10. the Chalk Aquifer of Yorkshire and North Humberside

    Baseline Report Series: 10. the Chalk Aquifer of Yorkshire and North Humberside

    Baseline Report Series: 10. The Chalk Aquifer of Yorkshire and North Humberside Groundwater Systems and Water Quality Commissioned Report CR/04/128 Environment Agency Science Group Technical Report NC/99/74/10 The Natural Quality of Groundwater in England and Wales A joint programme of research by the British Geological Survey and the Environment Agency BRITISH GEOLOGICAL SURVEY Commissioned Report CR/04/128 ENVIRONMENT AGENCY Science Group: Air, Land & Water Technical Report NC/99/74/10 This report is the result of a study jointly funded by the British Geological Baseline Report Series: Survey’s National Groundwater Survey and the Environment Agency’s Science 10. The Chalk Aquifer of Yorkshire Group. No part of this work may be reproduced or transmitted in any form or and North Humberside by any means, or stored in a retrieval system of any nature, without the prior permission of the copyright proprietors. All rights are reserved by the copyright P L Smedley, I Neumann and R Farrell* proprietors. Disclaimer Contributors The officers, servants or agents of both R Hargreaves, C J Milne, D Chadha* and M Morton* the British Geological Survey and the Environment Agency accept no liability whatsoever for loss or damage arising from the interpretation or use of the information, or reliance on the views contained herein. Environment Agency Dissemination status Internal: Release to Regions External: Public Domain ISBN: 978-1-84432-635-8 Product code: SCHO0207BLYH-E-P ©Environment Agency, 2004 Statement of use This document forms one of a series of reports describing the baseline chemistry of selected reference aquifers in England and Wales.
  • PDF (Volume 1)

    PDF (Volume 1)

    Durham E-Theses Aspects of late iron age and Romano-British settlement in the lower Hull valley Didsbury, Michael Peter Townley How to cite: Didsbury, Michael Peter Townley (1990) Aspects of late iron age and Romano-British settlement in the lower Hull valley, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/6477/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk 2 ABSTRACT The lower Hull valley is an extensive tract of estuarine alluvium between Kingston upon Hull and Beverley, North Humberside. The thesis examines the evidence for later Iron Age and Romano-British settlement in a landscape block of £. 330 km , incorporating the valley proper and the higher glacial deposits at its margins. The discussion utilises a comprehensive and critical gazetteer of some two hundred and twenty sites and findspots, and seven detailed site-studies present the results of the author's fieldwork or analysis of previously unpublished material assemblages.
  • NRFA Peak Flow Dataset

    NRFA Peak Flow Dataset

    National River Flow Archive NERC Centre for Ecology & Hydrology WINFAP-FEH DATA FILES VERSION 5 Note on changes from v4.1 VERSION: 1.0 STATUS: FINAL DATE: APRIL 2017 AUTHOR: KATIE MUCHAN, CATH SEFTON, STEVE TURNER, OLI SWAIN, MATT FRY, NURIA BACHILLER-JARENO DOCUMENT VERSION CONTROL Version Date Author Description 1.0 APRIL 2017 KATIE MUCHAN, CATH SEFTON, STEVE TURNER, OLI SWAIN, MATT FRY, NURIA BACHILLER-JARENO TABLE OF CONTENTS 1 INTRODUCTION ............................................................................................................................................................. 1 2 NETWORK CHANGES ...................................................................................................................................................... 2 2.1 REMOVAL OF GAUGING STATIONS......................................................................................................................................... 2 2.2 ADDITION OF GAUGING STATIONS......................................................................................................................................... 2 2.3 CLOSURE OF GAUGING STATIONS .......................................................................................................................................... 2 2.4 CHANGES TO FEH INDICATIVE SUITABILITIES ........................................................................................................................... 3 2.5 COMBINED PEAK FLOW TIME SERIES FROM MULTIPLE STATIONS ...............................................................................................