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Ecological Issues in Floodplains and Riparian Corridors
Final White Paper Research Project T1803 Task 29 Riparian Corridor ECOLOGICAL ISSUES IN FLOODPLAINS AND RIPARIAN CORRIDORS by Susan M. Bolton Jeff Shellberg Associate Professor and Director Research Assistant Center for Streamside Studies University of Washington, Bx 352100 Seattle, Washington 98195 Washington State Transportation Center (TRAC) University of Washington, Box 354802 University District Building 1107 NE 45th Street, Suite 535 Seattle, Washington 98105-4631 Washington State Department of Transportation Technical Monitor Patricia Lynch Environmental Affairs Prepared for Washington State Transportation Commission Department of Transportation and in cooperation with U.S. Department of Transportation Federal Highway Administration July 2001 TECHNICAL REPORT STANDARD TITLE PAGE 1. REPORT NO. 2. GOVERNMENT ACCESSION NO. 3. RECIPIENT'S CATALOG NO. WA-RD 524.1 4. TITLE AND SUBTITLE 5. REPORT DATE Ecological Issues in Floodplains and Riparian Corridors July 2001 6. PERFORMING ORGANIZATION CODE 7. AUTHOR(S) 8. PERFORMING ORGANIZATION REPORT NO. Susan M. Bolton and Jeff Shellberg 9. PERFORMING ORGANIZATION NAME AND ADDRESS 10. WORK UNIT NO. Washington State Transportation Center (TRAC) University of Washington, Box 354802 11. CONTRACT OR GRANT NO. University District Building; 1107 NE 45th Street, Suite 535 Agreement T1803, Task 29 Seattle, Washington 98105-4631 12. SPONSORING AGENCY NAME AND ADDRESS 13. TYPE OF REPORT AND PERIOD COVERED Research Office Washington State Department of Transportation Final white paper Transportation Building, MS 47370 Olympia, Washington 98504-7370 14. SPONSORING AGENCY CODE James Toohey, Project Manager, 360-705-0885 15. SUPPLEMENTARY NOTES This study was conducted in cooperation with the U.S. Department of Transportation, Federal Highway Administration. 16. ABSTRACT This white paper examines and synthesizes the literature pertaining to the current state of knowledge on the physical and biological effects of alluvial river channelization, channel confinement, and various channel and floodplain modifications. -
Biological Impacts of the Elwha River Dams and Potential Salmonid Responses to Dam Removal
George R. Pess1, NOAA Fisheries, Northwest Fisheries Science Center, 2725 Montlake Boulevard East, Seattle, Washington 98112 Michael L. McHenry, Lower Elwha Klallam Tribe, 2851 Lower Elwha Road, Port Angeles, Washington 98363 Timothy J. Beechie, and Jeremy Davies, NOAA Fisheries, Northwest Fisheries Science Center, 2725 Montlake Boulevard East, Seattle, Washington 98112 Biological Impacts of the Elwha River Dams and Potential Salmonid Responses to Dam Removal Abstract The Elwha River dams have disconnected the upper and lower Elwha watershed for over 94 years. This has disrupted salmon migration and reduced salmon habitat by 90%. Several historical salmonid populations have been extirpated, and remaining popu- lations are dramatically smaller than estimated historical population size. Dam removal will reconnect upstream habitats which will increase salmonid carrying capacity, and allow the downstream movement of sediment and wood leading to long-term aquatic habitat improvements. We hypothesize that salmonids will respond to the dam removal by establishing persistent, self-sustaining populations above the dams within one to two generations. We collected data on the impacts of the Elwha River dams on salmonid populations and developed predictions of species-specific response dam removal. Coho (Oncorhynchus kisutch), Chinook (O. tshawytscha), and steelhead (O. mykiss) will exhibit the greatest spatial extent due to their initial population size, timing, ability to maneuver past natural barriers, and propensity to utilize the reopened alluvial valleys. Populations of pink (O. gorbuscha), chum (O. keta), and sockeye (O. nerka) salmon will follow in extent and timing because of smaller extant populations below the dams. The initially high sediment loads will increase stray rates from the Elwha and cause deleterious effects in the egg to outmigrant fry stage for all species. -
Plants for Riparian Buffers
Website: Aberdeen Plant Materials Center http://plant-materials.nrcs.usda.gov Plants for Riparian Buffers P.O. Box 296, Aberdeen, ID 83210 Phone:(208) 397-4133 Fax:(208) 397-3104 What is a Riparian Buffer? Many farmers, ranchers and land managers have a growing concern over water quality issues. Riparian buffers are one of the most important practices that you can use to help control non- point pollution and improve water quality. Riparian buffers are the grasses, grass-like, forbs, shrubs, trees or other vegetation growing along streams. These plants control erosion and help filter and keep water clean. Cropland fields shouldn’t be planted right up to a stream’s edge where the soil is generally more fragile and subject to erosion. A healthy riparian buffer between cropland and a river system Shrubs, trees and other vegetation protect the stream from pollutants and runoff. They absorb excess nutrients such as nitrogen and phosphorus from farm and livestock operations. Plants protect the stream banks from erosion by providing a protective barrier against the water. The trunks, branches, stems and leaves intercept the water currents that can weaken and wash away bank material. In addition to protecting water and soil, riparian buffers provide important habitat for aquatic and upland wildlife and also fish habitat. The information contained in this brochure will help you select the best shrubs and trees for installing riparian buffers on your farm or ranch. The plants listed are all highly recommended for use in the Intermountain West and Rocky Mountain States. Included are tips for planning riparian buffers and areas, Aberdeen Plant Materials Center Service area. -
Draft Final Report
Draft Saddle Mountain Open Space Preserve Management Plan Initial Study and Proposed Mitigated Negative Declaration Prepared for: Sonoma County Agricultural Preservation and Open Space District 747 Mendocino Avenue Santa Rosa, CA 95401 Prepared by: Prunuske Chatham, Inc. 400 Morris St., Suite G Sebastopol, CA 95472 March 2019 This page is intentionally blank. Sonoma County Agricultural Preservation and Open Space District March 2019 Saddle Mountain Open Space Preserve Management Plan Initial Study/Proposed Mitigated Negative Declaration Table of Contents Page 1 Project Information ................................................................................................................................ 1 1.1 Introduction................................................................................................................................... 2 1.2 California Environmental Quality Act Requirements .................................................................... 3 1.2.1 Public and Agency Review ................................................................................................. 3 2 Project Description ................................................................................................................................. 4 2.1 Project Location and Setting ......................................................................................................... 4 2.2 Project Goals and Objectives ......................................................................................................... 4 -
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. -
Russian River Watershed Directory September 2012
Russian River Watershed Directory September 2012 A guide to resources and services For management and stewardship of the Russian River Watershed © www.robertjanover.com. Russian River & Big Sulphur Creek at Cloverdale, CA. Photo By Robert Janover Production of this directory was made possible through funding from the US Army Corps of Engineers and the California Department of Conservation. In addition to this version of the directory, you can find updated versions online at www.sotoyomercd.org Russian River Watershed Directory version September 2012 - 1 - Preface The Sotoyome Resource Conservation District (RCD) has updated our Russian River Watershed directory to assist landowners, residents, professionals, educators, organizations and agencies interested in the many resources available for natural resource management and stewardship throughout the Russian River watershed. In 1997, The Sotoyome RCD compiled the first known resource directory of agencies and organization working in the Russian River Watershed. The directory was an example of an emerging Coordinated Resource Management and Planning (CRMP) effort to encourage community-based solutions for natural resource management. Since that Photo courtesy of Sonoma County Water Agency time the directory has gone through several updates with our most recent edition being released electronically and re-formatting for ease of use. For more information or to include your organization in the Directory, please contact the Sotoyome Resource Conservation District Sotoyome Resource Conservation -
Ludwigia Control in the Laguna De Santa Rosa, California
Ludwigia Control in the Laguna de Santa Rosa, California California Invasive Plant Council 15th Annual Symposium Thomas J. McNabb, Clean Lakes, Inc. Julian Meisler, Laguna de Santa Rosa Foundation Ludwigia Control in the Laguna de Santa Rosa, California CDFA Project Site SCWA Project Site Ludwigia Control in the Laguna de Santa Rosa, California Ludwigia Control in the Laguna de Santa Rosa, California The Laguna de Santa Rosa Foundation (Laguna Foundation) contracted with Clean Lakes, Inc. to carry out Year One of a three-year control effort aimed at reducing the area and density of the non-native invasive weed Ludwigia hexapetala within selected areas of the Laguna de Santa Rosa The infestation harbors mosquito vectors of West Nile Virus (WNV) that poses a health threat to humans and wildlife; out-competes native wetland species, severely degrading habitat; and is believed to impair both the water quality and the flood-control functions of the Laguna. On April 28, 2005 the California Department of Fish and Game, Central Coast Region, and the Sonoma County Water Agency, each filed a Notice of Intent (NOI) and an Aquatic Pesticide Application Plan (APAP) to comply with the terms of the General National Pollution Discharge Elimination System Permit for the Discharge of Aquatic Pesticides for Aquatic Weed Control (General Permit) On July 1, 2005, the California Department of Fish and Game filed form FG 880, Application No. 05-361, Pesticide Use Recommendation for the work to be performed on the Department of Fish and Game property (Site II). Ludwigia Control in the Laguna de Santa Rosa, California On July 14, 2005, the California Regional Water Quality Control Board, North Coast Region, issued project approvals via a letter of “Applicability of General NPDES Permit for the Discharge of Aquatic Pesticides for Aquatic Weed Control in Waters of the United States and a Notice of Coverage, Waiver of Waste Discharge Requirements for the Laguna de Santa Rosa, Sonoma County” to the Sonoma County Water Agency, Ludwigia Control Project (WDID No. -
Sonoma County Rainfall Map (1.81MB)
128 OAT VALLEY CREEK ALDER CREEK Mendocino County CREEK BIG SULPHUR CREEK CLOVERDALE 40 Cloverdale 29 60 CREEK OSSER CREEK PORTERFIELD SONOMA COUNTY WATER AGENCY 45 40 LITTLE SULPHUR CREEK BUCKEYE CREEK 40 Lake County FLAT RIDGE CREEK 45 GUALALA RIVER 50 55 60 70 GRASSHOPPER CREEK 55 Sea Ranch 60 65 75 70 RANCHERIA CREEK LITTLE CREEK 55 50 GILL CREEK Annapolis 4 A SAUSAL CREEK 55 45 Lake STRAWBERRY CREEK Sonoma MILLER CREEK BURNS CREEK 50 TOMBS CREEK 45 65 WHEATFIELD Geyserville INGALLS CREEK FORK GUALALA-SALMON GUALALA-SALMON WOOD CREEK 1 GEORGE YOUNG CREEK BOYD CREEK MILL STREAM SOUTH FORK GUALALA BEAR CREEK FULLER CREEK COON CREEK 40 LITTLE BRIGGS CREEK RIVER 50 GIRD CREEK BRIGGS CREEK 7 A MAACAMA CREEK Jimtown WINE CREEK 6 A KELLOGG CREEK GRAIN CREEK HOUSE CREEK 60 CEDAR CREEK INDIANCREEK LANCASTER CREEK DANFIELD CREEK FALL CREEK OWL CREEK 40 Stewarts Point HOOT WOODS CREEK CRANE CREEK HAUPT CREEK YELLOWJACKET CREEK FOOTE CREEK REDWOOD CREEK GUALALA RIVER WALLACE CREEK 60 128 Lake JIM CREEK Berryessa ANGEL CREEK Healdsburg RUSSIAN RIVER SPROULE CREEK MILL CREEK DEVIL CREEK AUSTIN CREEK RUSSIAN RIVER SLOUGHWEST MARTIN CREEK BIG AUSTIN CREEK GILLIAM CREEK THOMPSON CREEK PALMER CREEK FELTA CREEK FRANZ CREEK BLUE JAY CREEK MCKENZIE CREEK BARNES CREEK BIG OAT CREEK Windsor MARK WEST CREEK COVE 75 WARD CREEK POOL CREEK PORTER CREEKMILL CREEK Fort Ross 80 HUMBUG CREEK TIMBER Cazadero STAR FIFE CREEK CREEK 55 PRUITT 45 HOBSON CREEK CREEK 50 NEAL CREEK 1 A 60 Hacienda REDWOOD CREEK RUSSIAN WIKIUP KIDD CREEK Guerneville CREEK VAN BUREN CREEK 101 RINCON CREEK RIVER 70 35 WEEKS CREEK 50 FULTON CREEK 65 BRUSH CREEK DUCKER CREEK GREEN COFFEYCREEK PINER CREEK 5 A VALLEY Forestville 60 CREEK CREEK RUSSELL BRUSH CREEK LAGUNA 55 Monte Rio CREEK AUSTIN BEAR CREEK RIVER CREEK GREEN FORESTVILLECREEK PAULIN CREEK DUTCH PINER CREEK Santa Rosa DE PETERSONCREEKFORESTVIEW SANTA ROSA CREEK OAKMONT STEELE VALLEY WENDELL CREEK CREEK BILL SANTA CREEK 45 SONOMA CREEK RUSSIAN GRUB CREEK SPRING CREEK LAWNDALECREEK 40 Napa County STATE HWY 116 COLLEGE CREEK CREEK HOOD MT. -
Logistic Analysis of Channel Pattern Thresholds: Meandering, Braiding, and Incising
Geomorphology 38Ž. 2001 281–300 www.elsevier.nlrlocatergeomorph Logistic analysis of channel pattern thresholds: meandering, braiding, and incising Brian P. Bledsoe), Chester C. Watson 1 Department of CiÕil Engineering, Colorado State UniÕersity, Fort Collins, CO 80523, USA Received 22 April 2000; received in revised form 10 October 2000; accepted 8 November 2000 Abstract A large and geographically diverse data set consisting of meandering, braiding, incising, and post-incision equilibrium streams was used in conjunction with logistic regression analysis to develop a probabilistic approach to predicting thresholds of channel pattern and instability. An energy-based index was developed for estimating the risk of channel instability associated with specific stream power relative to sedimentary characteristics. The strong significance of the 74 statistical models examined suggests that logistic regression analysis is an appropriate and effective technique for associating basic hydraulic data with various channel forms. The probabilistic diagrams resulting from these analyses depict a more realistic assessment of the uncertainty associated with previously identified thresholds of channel form and instability and provide a means of gauging channel sensitivity to changes in controlling variables. q 2001 Elsevier Science B.V. All rights reserved. Keywords: Channel stability; Braiding; Incision; Stream power; Logistic regression 1. Introduction loads, loss of riparian habitat because of stream bank erosion, and changes in the predictability and vari- Excess stream power may result in a transition ability of flow and sediment transport characteristics from a meandering channel to a braiding or incising relative to aquatic life cyclesŽ. Waters, 1995 . In channel that is characteristically unstableŽ Schumm, addition, braiding and incising channels frequently 1977; Werritty, 1997. -
HISTORICAL CHANGES in CHANNEL ALIGNMENT Along Lower Laguna De Santa Rosa and Mark West Creek
HISTORICAL CHANGES IN CHANNEL ALIGNMENT along Lower Laguna de Santa Rosa and Mark West Creek PREPARED FOR SONOMA COUNTY WATER AGENCY JUNE 2014 Prepared by: Sean Baumgarten1 Erin Beller1 Robin Grossinger1 Chuck Striplen1 Contributors: Hattie Brown2 Scott Dusterhoff1 Micha Salomon1 Design: Ruth Askevold1 1 San Francisco Estuary Institute 2 Laguna de Santa Rosa Foundation San Francisco Estuary Institute Publication #715 Suggested Citation: Baumgarten S, EE Beller, RM Grossinger, CS Striplen, H Brown, S Dusterhoff, M Salomon, RA Askevold. 2014. Historical Changes in Channel Alignment along Lower Laguna de Santa Rosa and Mark West Creek. SFEI Publication #715, San Francisco Estuary Institute, Richmond, CA. Report and GIS layers are available on SFEI’s website, at http://www.sfei.org/ MarkWestHE Permissions rights for images used in this publication have been specifically acquired for one-time use in this publication only. Further use or reproduction is prohibited without express written permission from the responsible source institution. For permissions and reproductions inquiries, please contact the responsible source institution directly. CONTENTS 1. Introduction .....................................................................................1 a. Environmental Setting..........................................................................2 b. Study Area ................................................................................................2 2. Methods ............................................................................................4 -
Relationships Among Basin Area, Sediment Transport Mechanisms and Wood Storage in Mountain Basins of the Dolomites (Italian Alps)
Monitoring, Simulation, Prevention and Remediation of Dense Debris Flows II 163 Relationships among basin area, sediment transport mechanisms and wood storage in mountain basins of the Dolomites (Italian Alps) E. Rigon, F. Comiti, L. Mao & M. A. Lenzi Department of Land and Agro-Forest Environments, University of Padova, Legnaro, Padova, Italy Abstract The present work analyses the linkages between basin geology, shallow landslides, streambed morphology and debris flow occurrence in several small watersheds of the Dolomites (Italian Alps). Field survey and GIS analysis were carried out in order to seek correlations among basin area, basin geology, spatial frequency of landslides, in-channel wood storage, and local bed slope. Keywords: large woody debris, landslides, bed morphology, Alps. 1 Introduction Along with sediments, shallow landslides in forested basins supply channels with wood elements, which may have a strong impact on both channel morphology/stability and on debris flow dynamics. Headwater channels, which make up 60–80% of the cumulative channel length in mountainous terrain [10, 11], are characterized by a strong coupling between hillslope and channel processes, in contrast to lowland streams. The switch between different transport mechanisms (e.g., bedload transport to debris flows) in the same channel often depends on the occurrence of shallow landslides feeding sediment in otherwise sediment-limited systems. Along with sediments, shallow landslides in forested basins supply channels with wood elements, which may have a strong impact on both channel morphology/stability WIT Transactions on Engineering Sciences, Vol 60, © 2008 WIT Press www.witpress.com, ISSN 1743-3533 (on-line) doi:10.2495/DEB080171 164 Monitoring, Simulation, Prevention and Remediation of Dense Debris Flows II and on debris flow dynamics. -
Historical Glimpses of the Laguna De Santa Rosa
“Crystal Laughing Waters” – Historical Glimpses of the Laguna de Santa Rosa by John Cummings December 2003 Copyright – John Cummings, December 20 ©John Cummings, 2003 All rights reserved 2 INTRODUCTION While a visitor to Sebastopol in 1898 described the Laguna as “crystal laughing waters” in the Sebastopol Times, the description is very fanciful. The Laguna is physically a very low flow stream with a fall of at most about 40 feet in the 14 miles between Cotati and the Russian River (a drop of less than three feet per mile – less than two feet per mile north of Sebastopol). While draining a relatively large watershed of 250 square miles – about 16% of the acreage of Sonoma County, the Laguna would have always been a relatively warm stream prone to cloudy water of low water quality – certainly not “crystal”– even in the “pristine” Laguna conditions prior to European settlement of the region in the 1830s. The Laguna north of Sebastopol typically floods its banks to some extent during the winter rainy season and usually does not flow during the late summer, but forms a series of ponds and dry channels. The post-European changes in acreage of habitat types and the abundance of wildlife in the Laguna area in the pristine and the early settlement period, is well established. But from a water quality point of view, post-European settlement made the “natural” poor water conditions of the Laguna highly degraded by, for example, making the water warmer yet by agricultural clearing of the riparian forest shading the waterway or by increasing nutrification of the water with farm wastes, urban sewage and cannery wastewater, etc.