Forgotten Legacies: Understanding and Mitigating Historical Human Alterations of River Corridors
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Geomorphic Classification of Rivers
9.36 Geomorphic Classification of Rivers JM Buffington, U.S. Forest Service, Boise, ID, USA DR Montgomery, University of Washington, Seattle, WA, USA Published by Elsevier Inc. 9.36.1 Introduction 730 9.36.2 Purpose of Classification 730 9.36.3 Types of Channel Classification 731 9.36.3.1 Stream Order 731 9.36.3.2 Process Domains 732 9.36.3.3 Channel Pattern 732 9.36.3.4 Channel–Floodplain Interactions 735 9.36.3.5 Bed Material and Mobility 737 9.36.3.6 Channel Units 739 9.36.3.7 Hierarchical Classifications 739 9.36.3.8 Statistical Classifications 745 9.36.4 Use and Compatibility of Channel Classifications 745 9.36.5 The Rise and Fall of Classifications: Why Are Some Channel Classifications More Used Than Others? 747 9.36.6 Future Needs and Directions 753 9.36.6.1 Standardization and Sample Size 753 9.36.6.2 Remote Sensing 754 9.36.7 Conclusion 755 Acknowledgements 756 References 756 Appendix 762 9.36.1 Introduction 9.36.2 Purpose of Classification Over the last several decades, environmental legislation and a A basic tenet in geomorphology is that ‘form implies process.’As growing awareness of historical human disturbance to rivers such, numerous geomorphic classifications have been de- worldwide (Schumm, 1977; Collins et al., 2003; Surian and veloped for landscapes (Davis, 1899), hillslopes (Varnes, 1958), Rinaldi, 2003; Nilsson et al., 2005; Chin, 2006; Walter and and rivers (Section 9.36.3). The form–process paradigm is a Merritts, 2008) have fostered unprecedented collaboration potentially powerful tool for conducting quantitative geo- among scientists, land managers, and stakeholders to better morphic investigations. -
Seasonal Flooding Affects Habitat and Landscape Dynamics of a Gravel
Seasonal flooding affects habitat and landscape dynamics of a gravel-bed river floodplain Katelyn P. Driscoll1,2,5 and F. Richard Hauer1,3,4,6 1Systems Ecology Graduate Program, University of Montana, Missoula, Montana 59812 USA 2Rocky Mountain Research Station, Albuquerque, New Mexico 87102 USA 3Flathead Lake Biological Station, University of Montana, Polson, Montana 59806 USA 4Montana Institute on Ecosystems, University of Montana, Missoula, Montana 59812 USA Abstract: Floodplains are comprised of aquatic and terrestrial habitats that are reshaped frequently by hydrologic processes that operate at multiple spatial and temporal scales. It is well established that hydrologic and geomorphic dynamics are the primary drivers of habitat change in river floodplains over extended time periods. However, the effect of fluctuating discharge on floodplain habitat structure during seasonal flooding is less well understood. We collected ultra-high resolution digital multispectral imagery of a gravel-bed river floodplain in western Montana on 6 dates during a typical seasonal flood pulse and used it to quantify changes in habitat abundance and diversity as- sociated with annual flooding. We observed significant changes in areal abundance of many habitat types, such as riffles, runs, shallow shorelines, and overbank flow. However, the relative abundance of some habitats, such as back- waters, springbrooks, pools, and ponds, changed very little. We also examined habitat transition patterns through- out the flood pulse. Few habitat transitions occurred in the main channel, which was dominated by riffle and run habitat. In contrast, in the near-channel, scoured habitats of the floodplain were dominated by cobble bars at low flows but transitioned to isolated flood channels at moderate discharge. -
Natural Character, Riverscape & Visual Amenity Assessments
Natural Character, Riverscape & Visual Amenity Assessments Clutha/Mata-Au Water Quantity Plan Change – Stage 1 Prepared for Otago Regional Council 15 October 2018 Document Quality Assurance Bibliographic reference for citation: Boffa Miskell Limited 2018. Natural Character, Riverscape & Visual Amenity Assessments: Clutha/Mata-Au Water Quantity Plan Change- Stage 1. Report prepared by Boffa Miskell Limited for Otago Regional Council. Prepared by: Bron Faulkner Senior Principal/ Landscape Architect Boffa Miskell Limited Sue McManaway Landscape Architect Landwriters Reviewed by: Yvonne Pfluger Senior Principal / Landscape Planner Boffa Miskell Limited Status: Final Revision / version: B Issue date: 15 October 2018 Use and Reliance This report has been prepared by Boffa Miskell Limited on the specific instructions of our Client. It is solely for our Client’s use for the purpose for which it is intended in accordance with the agreed scope of work. Boffa Miskell does not accept any liability or responsibility in relation to the use of this report contrary to the above, or to any person other than the Client. Any use or reliance by a third party is at that party's own risk. Where information has been supplied by the Client or obtained from other external sources, it has been assumed that it is accurate, without independent verification, unless otherwise indicated. No liability or responsibility is accepted by Boffa Miskell Limited for any errors or omissions to the extent that they arise from inaccurate information provided by the Client or -
On the Quantitative.Invent01·Y of the Riverscape' ,I
WATER RESOURCES RESEARCH AUGUST 1968 _ On the Quantitative .Invent01·y of the Riverscape' LPNA B. LEOPOLD AND MAURA O'BRIEN MARCHAND U. S. Geological Survey W""hinglon, D. C.IIO!!42 ,I Ab8tract. In the vicinity of Berkeley. California, 24 minor "alleys were described in terms of factors chosen to represent aspects of the river landscape. A total of 28 factors were evalu ated at eaeh site. Some were directly measurable. others were estimated, but each obsen'atioll was assigned to ODe of five categories for tha.t factor. Each factor for each site was then expressed as a uniqueness ratio, which depended on the number of sites being in Ute same category. The uniqueness ratio is believed to represent one way the scarcity of a given river &CRpe can be ranked quantitatively without bias based 011 notions of good or bad, and without assigning monetary value. GENERAL STATEMENT differently. depending upon individual back ground, interest, desires, and thus one's objec On property we grow pigs or peanulll. On tives. we grow suburbs or sunJlowers. On land The present paper presents a tcntntiye nod pe we grow feelings or frustrations. The modest attempt to record the presence or ab 'ty of a landscape may be an asset to sence of chosen factors that contribute to iety, or it may be a 'scarlet letter' that should aesthetic worth. Observations were made in a . d us of wbat we have thrown away. All restricted range of exnmples in one locality, empts to preserve the environment must ne- Alameda and Contra Costa count.ics near San ily rewesent a compromise between the Francisco Bay. -
Rainfall Thresholds for Flow Generation in Desert Ephemeral
Water Resources Research RESEARCH ARTICLE Rainfall Thresholds for Flow Generation 10.1029/2018WR023714 in Desert Ephemeral Streams 1 1 2 1 Key Points: Stephanie K. Kampf G!), Joshua Faulconer , Jeremy R. Shaw G!), Michael Lefsky , Rainfall thresholds predict 3 2 streamflow responses with high Joseph W. Wagenbrenner G!), and David J. Cooper G!) accuracy in small hyperarid and 1 2 semiarid watersheds Department of Ecosystem Science and Sustainability, Colorado State University, Fort Collins, Colorado, USA, Department 3 Using insufficient rain data usually of Forest and Rangeland Stewardship, Colorado State University, FortCollins, Colorado, USA, USDA Forest Service, Pacific increases threshold values for larger Southwest Research Station, Arcata, California,USA watersheds, leading to apparent scale dependence in thresholds Declines in flow frequency and Rainfall thresholds for streamflow generation are commonly mentioned in the literature, but increases in thresholds with drainage Abstract area are steeper in hyperarid than in studies rarely include methods for quantifying and comparing thresholds. This paper quantifies thresholds semiarid watersheds in ephemeral streams and evaluates how they are affected by rainfall and watershed properties. The study sites are in southern Arizona, USA; one is hyperarid and the other is semiarid. At both sites rainfall and 3 2 2 Supporting Information: streamflow were monitored in watersheds ranging from 10- to 10 km . Streams flowed an average of 0-5 • Supporting Information 51 times per year in hyperarid watersheds and 3-11 times per year in semiarid watersheds. Although hyperarid sites had fewer flow events, their flow frequency (fraction of rain events causing flow) was higher than in Correspondence to: 2 semiarid sites for small ( < 1 km ) watersheds. -
Floodplain Geomorphic Processes and Environmental Impacts of Human Alteration Along Coastal Plain Rivers, Usa
WETLANDS, Vol. 29, No. 2, June 2009, pp. 413–429 ’ 2009, The Society of Wetland Scientists FLOODPLAIN GEOMORPHIC PROCESSES AND ENVIRONMENTAL IMPACTS OF HUMAN ALTERATION ALONG COASTAL PLAIN RIVERS, USA Cliff R. Hupp1, Aaron R. Pierce2, and Gregory B. Noe1 1U.S. Geological Survey 430 National Center, Reston, Virginia, USA 20192 E-mail: [email protected] 2Department of Biological Sciences, Nicholls State University Thibodaux, Louisiana, USA 70310 Abstract: Human alterations along stream channels and within catchments have affected fluvial geomorphic processes worldwide. Typically these alterations reduce the ecosystem services that functioning floodplains provide; in this paper we are concerned with the sediment and associated material trapping service. Similarly, these alterations may negatively impact the natural ecology of floodplains through reductions in suitable habitats, biodiversity, and nutrient cycling. Dams, stream channelization, and levee/canal construction are common human alterations along Coastal Plain fluvial systems. We use three case studies to illustrate these alterations and their impacts on floodplain geomorphic and ecological processes. They include: 1) dams along the lower Roanoke River, North Carolina, 2) stream channelization in west Tennessee, and 3) multiple impacts including canal and artificial levee construction in the central Atchafalaya Basin, Louisiana. Human alterations typically shift affected streams away from natural dynamic equilibrium where net sediment deposition is, approximately, in balance with net -
Coastal Erosion in Cape Cod, Massachusetts: Finding Sustainable Solutions Michael D
University of Massachusetts Amherst ScholarWorks@UMass Amherst Student Showcase Sustainable UMass 2015 Coastal Erosion in Cape Cod, Massachusetts: Finding Sustainable Solutions Michael D. Roberts University of Massachusetts - Amherst, [email protected] Lauren Bullard University of Massachusetts - Amherst Shaunna Aflague University of Massachusetts - Amherst Kelsi Sleet University of Massachusetts - Amherst Follow this and additional works at: https://scholarworks.umass.edu/ sustainableumass_studentshowcase Part of the Environmental Policy Commons, and the Environmental Studies Commons Roberts, Michael D.; Bullard, Lauren; Aflague, Shaunna; and Sleet, Kelsi, "Coastal Erosion in Cape Cod, Massachusetts: indF ing Sustainable Solutions" (2015). Student Showcase. 6. Retrieved from https://scholarworks.umass.edu/sustainableumass_studentshowcase/6 This Article is brought to you for free and open access by the Sustainable UMass at ScholarWorks@UMass Amherst. It has been accepted for inclusion in Student Showcase by an authorized administrator of ScholarWorks@UMass Amherst. For more information, please contact [email protected]. Coastal Erosion in Cape Cod 1 Coastal Erosion in Cape Cod, Massachusetts: Finding Sustainable Solutions Michael Roberts, Lauren Bullard, Shaunna Aflague, and Kelsi Sleet NRC 576 Water Resources Management and Policy Fall 2014 Coastal Erosion in Cape Cod 2 ABSTRACT The Massachusetts Office of Coastal Zone Management (CZM) and the Cape Cod Planning Commission have identified coastal erosion, flooding, and shoreline change as the number one risk affecting the heavily populated 1,068 square kilometers that constitute Cape Cod (CZM, 2013 and Cape Cod Commission 2010). This paper investigates natural and anthropogenic causes for coastal erosion and their relationship with established social and economic systems. Sea level rise, climate change, and other anthropogenic changes increase the rate of coastal erosion. -
Coastal Recovery Unit Implementation Plan for Bull Trout (Salvelinus Confluentus)
U.S. Fish & Wildlife Service Coastal Recovery Unit Implementation Plan for Bull Trout (Salvelinus confluentus) Top left: Clackamas bull trout reintroduction, Clackamas River, Oregon. David Herasimtschuk, Freshwaters Illustrated; Top, right: Glines Canyon Dam removal, Elwha River, Washington. John Gussman, Doubleclick Productions; Center: South Fork Skagit River and Skagit Bay, Washington. City of Seattle; Bottom: Riverscape surveys, East Fork Quinault River, Washington. National Park Service, Olympic National Park Coastal Recovery Unit Implementation Plan for Bull Trout (Salvelinus confluentus) September 2015 Prepared by U.S. Fish and Wildlife Service Washington Fish and Wildlife Office Lacey, Washington and Oregon Fish and Wildlife Office Portland, Oregon Table of Contents Introduction ................................................................................................................................. A-1 Current Status of Bull Trout in the Coastal Recovery Unit ........................................................ A-6 Factors Affecting Bull Trout in the Coastal Recovery Unit ....................................................... A-8 Ongoing Coastal Recovery Unit Conservation Measures (Summary) ..................................... A-33 Research, Monitoring, and Evaluation ..................................................................................... A-38 Recovery Measures Narrative ................................................................................................... A-39 Implementation Schedule for -
WATS 5150 – Fluvial Geomorphology WEEK 5: Habitat Suitability Models
Instream Geomorphic Units I. Intro → Geomorphic Units & Process-Form Associations II. Classification & Field Identification III. Your Book (River Styles) I. Sculpted, Erosional Bedrock & Boulder GUs II. Mid-Channel, Depositional GUs III. Bank-Attached, Depositional GUs IV. Sculpted, Erosional Fine-Grained GUs V. Unit & Compound GUs VI. Forced GUs IV. Continuum of GUs V. Fluvial Taxonomy GUs (Topographically Defined) I. Tier 1 – Stage II. Tier 2 – Shape / Form III. Tier 3 – Attributed VI. GUT (Geomorphic Unit Toolkit) Reminder… • In fluvial, we found over 100 different terms to describe geomorphic units, of which 68 were actually distinctive… • This is based on same units as above, but with some clarifications • Done with your Book’s Authors • The legend should include a) margins, b) geomorphic units, and c) structural elements From: Wheaton et al. (2015) – Geomorphology; DOI: 10.1016/j.geomorph.2015.07.010 Taxonomy for Mapping Fluvial Landforms • Four Tiers • Stage Height • Shape / Form • Morphology • Roughness/Vegetation • Over 100 fluvial geomorphic units found in literature, of which 68 are distinctive (3b) • Clearer, topographically based definitions From: https://riverscapes.github.io/pyGUT/ Wheaton et al. (2015) DOI: 10.1016/j.geomorph.2015.07.010 Williams et al. (2020) DOI: 10.1016/j.scitotenv.2020.136817 Instream Geomorphic Units I. Intro → Geomorphic Units & Process-Form Associations II. Classification & Field Identification III. Your Book (River Styles) I. Sculpted, Erosional Bedrock & Boulder GUs II. Mid-Channel, Depositional GUs III. Bank-Attached, Depositional GUs IV. Sculpted, Erosional Fine-Grained GUs V. Unit & Compound GUs VI. Forced GUs IV. Continuum of GUs V. Fluvial Taxonomy GUs (Topographically Defined) I. -
River Restoration and Chalk Streams
River Restoration and Chalk Streams Monday 22nd – Tuesday 23rd January 2001 University of Hertfordshire, College Lane, Hatfield AL10 9AB Organised by the River Restoration Centre in partnership with University of Hertfordshire Environment Agency, Thames Region Report compiled by: Vyv Wood-Gee Countryside Management Consultant Scabgill, Braehead, Lanark ML11 8HA Tel: 01555 870530 Fax: 01555 870050 E-mail: [email protected] Mobile: 07711 307980 ____________________________________________________________________________ River Restoration and Chalk Streams Page 1 Seminar Proceedings CONTENTS Page no. Introduction 3 Discussion Session 1: Flow Restoration 4 Discussion Session 2: Habitat Restoration 7 Discussion Session 3: Scheme Selection 9 Discussion Session 4: Post Project Appraisal 15 Discussion Session 5: Project Practicalities 17 Discussion Session 6: BAPs, Research and Development 21 Discussion Session 7: Resource Management 23 Discussion Session 8: Chalk streams and wetlands 25 Discussion Session 9: Conclusions and information dissemination 27 Site visit notes 29 Appendix I: Delegate list 35 Appendix II: Feedback 36 Appendix III: RRC Project Information Pro-forma 38 Appendix IV: Project summaries and contact details – listed 41 alphabetically by project name. ____________________________________________________________________________ River Restoration and Chalk Streams Page 2 Seminar Proceedings INTRODUCTION Workshop Objectives · To facilitate and encourage interchange of information, views and experiences between people working with projects and programmes with strong links to chalk streams and activities or research that affect this environment. · To improve the knowledge base on the practicalities and associated benefits of chalk stream restoration work in order to make future investments more cost effective. Participants The workshop was specifically targeted at individuals and organisations whose activities, research or interests include a specific practical focus on chalk streams. -
Report on the Millennium Chalk Streams Fly Trends Study
EA-South West/0fe2 s REPORT ON THE MILLENNIUM CHALK STREAMS FLY TRENDS STUDY A survey carried out in 2000 among 365 chalk stream fly fishermen, fishery owners, club secretaries and river keepers Subject: trends in aquatic fly abundance over recent decades and immediate past years, seen through the eyes of those constantly on the banks of, and caring for, the South country chalk rivers. Prepared by: Allan Frake, Environment Agency Peter Hayes, FMRS, Wiltshire Fishery Association with data available to all contributory associations and clubs. E n v ir o n m e n t A g e n c y WILTSHIRE FISHFRY ASSOCIATION I Report on the Millennium Chalk Streams Fly Trends Study Published by: Environment Agency Manley House Kestrel Way Exeter EX2 7LQ Tel: 01392 444000 Fax: 01392 444238 ISBN 1 85 705759 7 © Environment Agency 2001 All rights reserved. No part of this publication may be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, mechanical or photocopying, recording, or otherwise, without prior written permission of the Environment Agency. En v ir o n m e n t A g e n c y NATIONAL LIBRARY & INFORMATION SERVICE SOUTH WEST REGION Manley House, Kestrel Way. Exeter EX2 7LQ SW-12/01 -E-1.5k-BG|W Errt-^o-t-Hv k Io i - i Report on the Millennium Chalk Streams Fly Trends Study I CONTENTS Management Summary Falling fly numbers Introduction and Objectives Methodology Sampling method, respondent qualifications and sample achieved Observational coverage Internal tests for bias, and robustness of data Questionnaire design -
Managing Catchments for Flood Risk and Biodiversity
How river catchments can be better managed to control flood risk and provide biodiversity benefits A critical discussion of options and experience and suggestions for ways forward Adam Broadhead and Julian Jones April 2010 Water21 (Department of Vision21 Ltd) 30 St Georges Place Cheltenham GL50 3JZ 01242 224321 Managing rivers and floodplains to reduce flood risk and improve biodiversity Abstract This paper critically discusses options for farmland, river and floodplain management to resolve flood risk and provide biodiversity benefits. Focusing on the UK context, where there is a call for working more closely with nature. Restoration of natural systems provides the best opportunities for habitat creation and biodiversity, but the benefits to flood risk management can be limited, unless applied at the catchment scale. Conventional hard-engineered approaches offer proven but expensive flood resolution, and there is now a move towards more soft-engineered, multi-purpose, low cost, naturalistic schemes involving the whole landscape. The effectiveness for biodiversity improvements must be balanced by the overriding priority to protect people from flooding. Linking biodiversity and flood risk management is an important step, but does not go far enough. Contents Abstract ................................................................................................................................................... 2 Contents .................................................................................................................................................