Statistical Summaries of Streamflow in Oklahoma Through 1999

Total Page:16

File Type:pdf, Size:1020Kb

Statistical Summaries of Streamflow in Oklahoma Through 1999 U.S. Department of the Interior U.S. Geological Survey Statistical Summaries of Streamflow in Oklahoma Through 1999 By Robert L. Tortorelli Water-Resources Investigations Report 02–4025 Prepared in cooperation with the OKLAHOMA DEPARTMENT OF ENVIRONMENTAL QUALITY On Cover: Baron Fork at Eldon, Oklahoma. Low-flow photograph was taken September 1998. High-flow photograph was taken June 2000. Photographers: John A. Schmidt, senior hydrologist, and Michael D. Pierce, senior hydrologist, National Weather Service, Arkansas-Red Basin Forecast Center, Tulsa, Oklahoma. U.S. Department of the Interior GALE A. NORTON, Secretary U.S. Geological Survey CHARLES G. GROAT, Director The use of firm, trade, and brand names in this report is for identification purposes only and does not constitute endorsement by the U.S. Geological Survey. UNITED STATES GOVERNMENT PRINTING OFFICE: OKLAHOMA CITY 2002 For additional information write to: Copies of this report can be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Information Services Water-Resources Division Box 25286 202 NW 66 St., Bldg. 7 Federal Center Oklahoma City, OK 73116 Denver, CO 80225 CONTENTS Abstract ..................................................................................................................................................................................... 1 Introduction................................................................................................................................................................................ 1 Purpose and scope ........................................................................................................................................................... 2 Acknowledgments .......................................................................................................................................................... 2 Statistical Summaries ................................................................................................................................................................ 2 Site selection ................................................................................................................................................................... 2 Description of streamflow statistics tables ...................................................................................................................... 2 Station descriptions ............................................................................................................................................. 13 Mean annual discharges ...................................................................................................................................... 13 Annual high-flow frequency ............................................................................................................................... 14 Annual instantaneous peak-flow frequency ........................................................................................................ 14 Flow duration ...................................................................................................................................................... 15 Annual and seasonal low-flow frequencies ......................................................................................................... 15 Summary.................................................................................................................................................................................. 16 Selected references ................................................................................................................................................................. 17 Statistical summaries of streamflow ........................................................................................................................................ 19 Streamflow tables........................................................................................................................................................... 20 Index ............................................................................................................................................................................ 505 ILLUSTRATIONS Figure 1. Map showing location of streamflow-gaging stations with at least 10 years of streamflow data used in study. ............................................................................................................................... 3 TABLES 1. Summary of streamflow period of record used in study for selected continuous-record streamflow-gaging stations with at least 10 years of streamflow data from unregulated, regulated, and urban basins within and near Oklahoma ................................................................................................................................................................... 5 2. Summary of drainage area distribution of streamflow statistics analyses for streamflow-gaging sites .............................. 13 CONVERSION FACTORS, ABBREVIATIONS, AND VERTICAL DATUM Multiply By To obtain inch (in.) 25.4 millimeter mile (mi) 1.609 kilometer square mile (mi2) 2.590 square kilometer cubic foot per second (ft3/s) 0.02832 cubic meter per second Sea level: In this report “sea level” refers to the National Geodetic Vertical Datum of 1929 (NGVD of 1929)—a geodetic datum derived from a general adjustment of the first-order level nets of both the United States and Canada, formerly called Sea Level Datum of 1929. CONTENTS I Statistical Summaries of Streamflow in Oklahoma through 1999 By Robert L. Tortorelli ABSTRACT ronmental Quality, conducted an investigation to update streamflow statistics in Oklahoma. Statistical summaries of streamflow records At least 10 years of daily streamflow data exist through 1999 for gaging stations in Oklahoma for 174 streamflow gaging stations in Oklahoma and and parts of adjacent states are presented for 188 14 in nearby parts of adjacent states. Since 1984 there stations with at least 10 years of streamflow have been several streamflow sites: 1) with additional record. Streamflow at 113 of the stations is regu- years of record, or 2) not previously analyzed that are lated for specific periods. Data for these periods included because they now have 10 years or more of were analyzed separately to account for changes data, or 3) that are now regulated. Useful summaries in streamflow due to regulation by dams or other for streamflow data represent mean annual flow, low- human modification of streamflow. and high-flow frequency statistics, peak-flow statistics, A brief description of the location, drainage and flow-duration statistics. Information about mean area, and period of record is given for each gaging annual flow, low-flow and high-flow characteristics, station. A brief regulation history also is given for and flow-duration statistics is essential to water-man- stations with a regulated streamflow record. This agement agencies dealing with problems related to descriptive information is followed by tables of irrigation, municipal and industrial water supplies, and mean annual discharges, magnitude and proba- fish and wildlife conservation. bility of exceedance of annual high flows, magni- Low-flow statistics are particularly important to tude and probability of exceedance of annual in- assess the capability of a stream to receive and assimi- stantaneous peak flows, durations of daily mean late treated wastewater. Low-flow statistics are used in flow, magnitude and probability of non-exceed- developing wastewater permits and determining total ance of annual low flows, and magnitude and maximum daily loads of streams. Annual and seasonal probability of non-exceedance of seasonal low 7-day, 2-year low-flow streamflows are used as part of flows. the criteria for developing wasteload allocations for permit purposes and is specifically cited in State stat- utes. Other low-flow durations (1, 3, 10, 30, and 60 days) and frequencies (5, 10, and 20 years) also are INTRODUCTION useful to characterize streamflow at a site. Streamflow statistics are used by individuals and Knowledge of high-flow and peak-flow statistics organizations involved in the planning of projects with is required for the safe and economical design of high- surface-water resources. The last report that published way bridges, culverts, dams, levees, and other struc- summaries of streamflow statistics in Oklahoma used tures on or near streams and for disaster planning. streamflow data through 1984 (Heimann and Tortor- Flood plain management programs and flood-insur- elli, 1988). The U. S. Geological Survey (USGS), in ance rates also are based on peak-flow magnitude and cooperation with the Oklahoma Department of Envi- frequency information. 1 Purpose and Scope flowing into Oklahoma, the nearest gaging stations in the nearby parts of adjacent states were selected for The purposes of this report are to: (1) update analysis. Fourteen stations on major rivers in adjacent mean annual flow, annual low- and high-flow statis- states and 174 streamflow-gaging stations in Okla- tics, and flow-duration statistics for each streamflow homa were selected. Only continuous-record sites with gaging station with 10 years or more of streamflow at least 10 years of unregulated or regulated data were record; (2) present seasonal low-flow statistics for selected for analysis. Streamflow at 113 of the stations these gaging stations for three Oklahoma growth is known to be affected by regulation, urbanization, or seasons: (a) spring
Recommended publications
  • Notropis Girardi) and Peppered Chub (Macrhybopsis Tetranema)
    Arkansas River Shiner and Peppered Chub SSA, October 2018 Species Status Assessment Report for the Arkansas River Shiner (Notropis girardi) and Peppered Chub (Macrhybopsis tetranema) Arkansas River shiner (bottom left) and peppered chub (top right - two fish) (Photo credit U.S. Fish and Wildlife Service) Arkansas River Shiner and Peppered Chub SSA, October 2018 Version 1.0a October 2018 U.S. Fish and Wildlife Service Region 2 Albuquerque, NM This document was prepared by Angela Anders, Jennifer Smith-Castro, Peter Burck (U.S. Fish and Wildlife Service (USFWS) – Southwest Regional Office) Robert Allen, Debra Bills, Omar Bocanegra, Sean Edwards, Valerie Morgan (USFWS –Arlington, Texas Field Office), Ken Collins, Patricia Echo-Hawk, Daniel Fenner, Jonathan Fisher, Laurence Levesque, Jonna Polk (USFWS – Oklahoma Field Office), Stephen Davenport (USFWS – New Mexico Fish and Wildlife Conservation Office), Mark Horner, Susan Millsap (USFWS – New Mexico Field Office), Jonathan JaKa (USFWS – Headquarters), Jason Luginbill, and Vernon Tabor (Kansas Field Office). Suggested reference: U.S. Fish and Wildlife Service. 2018. Species status assessment report for the Arkansas River shiner (Notropis girardi) and peppered chub (Macrhybopsis tetranema), version 1.0, with appendices. October 2018. Albuquerque, NM. 172 pp. Arkansas River Shiner and Peppered Chub SSA, October 2018 EXECUTIVE SUMMARY ES.1 INTRODUCTION (CHAPTER 1) The Arkansas River shiner (Notropis girardi) and peppered chub (Macrhybopsis tetranema) are restricted primarily to the contiguous river segments of the South Canadian River basin spanning eastern New Mexico downstream to eastern Oklahoma (although the peppered chub is less widespread). Both species have experienced substantial declines in distribution and abundance due to habitat destruction and modification from stream dewatering or depletion from diversion of surface water and groundwater pumping, construction of impoundments, and water quality degradation.
    [Show full text]
  • October 2002 Local/ Length Width Persons Damage Location Date Standard (Miles) (Yards) Killed Injured Property Crops Character of Storm
    Time Path Path Number of Estimated October 2002 Local/ Length Width Persons Damage Location Date Standard (Miles) (Yards) Killed Injured Property Crops Character of Storm OKLAHOMA, Western, Central and Southeast Alfalfa County 2 S Cherokee02 1135CST 0 0 Thunderstorm Wind (G52) Grant County Pond Creek02 1730CST 0 0 Hail(0.75) Garfield County 1 W Kremlin02 1745CST 0 0 20K Thunderstorm Wind Severe straight-line winds downed several large tree limbs and blew a boat and trailer about 100 yards. In addition, several house windows were broken; a cattle feeder was blown onto a nearby road; numerous wooden fences were blown over, and the westward-facing wall of a storage shed was pushed in three to five inches. Kay County Ponca City02 1835CST 0 0 Hail(0.88) Hail was reported on the northwest side of the city. Alfalfa County 1 N Cherokee03 0000CST 0 0 60K Flash Flood Four homes received minor damage from high water. Two vehicles were pulled out of high water, and State Highway 8 was closed due to high water. Woodward County 2 SW Mutual03 0200CST 0 0 20K Flash Flood 0800CST A paved road was washed away. Alfalfa County 2 SE Helena03 0300CST 0 0 0 Flash Flood State Highway 45 was closed due to high water. OKZ005-007>008- Woods - Grant - Kay - Woodward - Major - Dewey - Blaine - Kingfisher 010>011-015-017>018 03 0700CST 0 0 25K Flood 06 1430CST Two days of periodic heavy rain fell across much of northwest Oklahoma with some areas receiving nearly seven inches. Large amounts of runoff caused many rivers to rise above flood stage, including the Salt Fork Arkansas River at Tonkawa, the Chikaskia River near Braman and Blackwell, the Cimarron River near Waynoka, Okeene, and Dover, and the North Canadian River near Seiling.
    [Show full text]
  • Drought of Water Year 2006 Compared with Four Major Drought Periods of the 20Th Century in Oklahoma
    Prepared in cooperation with the Oklahoma Water Resources Board Hydrologic Drought of Water Year 2006 Compared with Four Major Drought Periods of the 20th Century in Oklahoma • .... Canadian River near Norman February 1952 -,. Canadian River downstream from State Highway. 99" or' near Ada August 16, 2006.. Scientific Investigations Report 2008-5199 U.S. Department of the Interior U.S. Geological Survey Front Cover: Picture One shows wind ripples and river silts, Canadian River near Norman, Cleveland County, Okla- homa, taken February 1952. Photographer: W.B. Hamilton, from U.S. Geological Survey Photographic Library. Picture Two shows the dry Canadian River near Ada, Pontotoc County, Oklahoma, downstream from State High- way 99, taken August 16, 2006. Photographer: Daniel Fenner, U.S. Fish and Wildlife Service. Hydrologic Drought of Water Year 2006 Compared with Four Major Drought Periods Of the 20th Century in Oklahoma By Robert L. Tortorelli Prepared in cooperation with the Oklahoma Water Resources Board Scientific Investigations Report 2008–5199 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2008 This and other USGS information products are available at: http://store.usgs.gov/ U.S. Geological Survey Box 25286, Denver Federal Center Denver, CO 80225 To learn about the USGS and its information products visit http://www.usgs.gov/ 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government.
    [Show full text]
  • Oklahoma Geological Survey Open-File Report Disclaimer
    Oklahoma Geological Survey Open-File Report Disclaimer Open-File Reports are used for the dissemination of information that fills a public need and are intended to make the results of research available at the earliest possible date. Because of their nature and possibility of being superseded, an Open-File Report is intended as a preliminary report not as a final publication. Analyses presented in this article are based on information available to the author, and do not necessarily represent the views of the Oklahoma Geological Survey, the University of Oklahoma, their employees, or the State of Oklahoma. The accuracy of the information contained herein is not guaranteed and any mention of trade names are not an endorsement by the author, the Oklahoma Geological Survey, or the University of Oklahoma. The Oklahoma Geological Survey is a state agency for research and public service, mandated in the State Constitution to study Oklahoma’s land, water, mineral and energy resources and to promote wise use and sound environmental practices. Preface This report is updated from one that was originally prepared for the Tulsa District Office of the U.S. Army Corps of Engineers (USACE) in 1978 to characterize the geology at and near major natural salt plains in parts of the Arkansas River Chloride Control Project (ARCCP) area in northwestern Oklahoma. The ARCCP is designed to control natural chloride-brine emissions at major source areas in northwestern Oklahoma, and thus to improve water quality for municipal, industrial, and agricultural use downstream from the salt plains. Improvements that may help control brine emissions include construction of low-flow dams, pump stations, and diversion pipelines to impoundment facilities.
    [Show full text]
  • Index of Surface-Water Records to September 30, 1955
    GEOLOGICAL SURVEY CIRCULAR 387 INDEX OF SURFACE-WATER RECORDS TO SEPTEMBER 30, 1955 PART 7.-LOWER MISSISSIPPI RIVER BASIN PftDPE1n'Y cnr U. 5. GtO ! :-:cn:Al~ SURVEY. PUBLIC ;;::..'·,:: :Cri OFFIC~ SAN nM,l-4Ci:,.;;.;o, Ci\Ltf"O~NIA UNITED STATES DEPAR'l'MENT OF THE INTERIOR Fred A. Seaton, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director GEOLOGICAL SURVEY CIRCULAR 387 INDEX OF SURFACE-WATER RECORDS TO SEPTEMBER 30,1955 PART 7.-LOWER MISSISSIPPI RIVER BASIN By J. S. Gatewood Washington, D. C., 1956 Free on application to the Geological Survey, Washington 25, D. C. INDEX OF SURFACE-WATER RECORDS TO SEPTEMBER 30,1955 PART 7.-LOWER MISSISSIPPI RIVER BASIN By J. S. Gatewood EXPLANATION This index lists th~ streamflow and reservoir stations in the Lower Mississippi River basin for which records have been or are to be published in reports of the Geological Survey for periods prior to September 30, 1955. Periods of record for the same station published by other agencies are listed only when they contain more detailed information or are for periods not reported in publications of the Geological Survey. The stations are listed in the downstream order first adopted for use in the 1951 series of water-supply papers on surface-water supply of the United States. Starting at the headwater of each stream all stations are listed in a downstream direction. Tributary streams are indicated by indention and are inserted between main-stem stations in the order in which they enter the main stream. To indicate the rank of any tributary on which a record is available and the stream to which it is immediately tributary, each indention in the listing of stations represents one rank.
    [Show full text]
  • RIVERS, STREAMS, and LAKES of OKLAHOMA Kenneth S
    Page 12, Rivers, Streams, and Lakes EDUCATIONAL PUBLICATION 9: 2008 EXPLANATION Scenic River; number corresponds to name in text Salt Plain; number corresponds to name in text Table 4. Major lakes and reservoirs in Oklahoma Lake Area Drainage Areaa Capacity Location Normal Pool Normal Pool (acres) (square miles) (acre-feet) County/Counties Eufaula 105,500 47,522 2,314,600 McIntosh; Pittsburg; Haskell Texoma 88,000 39,719 2,643,300 Love; Marshall; Bryan; Johnston Grand Lake O’ the 46,500 10,298 1,672,000 Delaware; Ottawa; Mayes Cherokees Robert S. Kerr 43,800 147,756 525,700 Haskell; Sequoyah; Le Flore Oologah 29,460 4,339 553,400 Rogers; Nowata Keystone 23,610 74,506 557,600 Osage; Pawnee; Creek; Tulsa Fort Gibson 19,900 12,492 365,200 Wagoner; Cherokee; Mayes Kaw 17,040 46,530 428,600 Kay; Osage Broken Bow 14,200 754 918,070 McCurtain Sardis 13,610 275 274,330 Pushmataha; Latimer Hugo 13,250 1,709 157,600 Choctaw Tenkiller 12,900 1,610 654,100 Cherokee; Sequoyah Webbers Falls 11,600 97,033 170,100 Muskogee Hudson 10,900 11,533 220,300 Mayes Skiatook 10,190 354 322,700 Osage Waurika 10,100 562 203,100 Jefferson; Stephens; Cotton Foss 8,880 1,496 256,220 Custer Great Salt Plains 8,690 3,200 31,420 Alfalfa Canton 7,910 12,483 111,310 Blaine; Dewey Wister 7,333 993 62,360 Le Flore aData from the Oklahoma Water Resources Board (1990). RIVERS, STREAMS, AND LAKES OF OKLAHOMA Kenneth S.
    [Show full text]
  • Summary of Annual Records of Chemical Quality of Water of the Arkansas River in Oklahoma and Arkansas 1945-52
    GEOLOGICAL SURVEY CIRCULAR 361 SUMMARY OF ANNUAL RECORDS OF CHEMICAL QUALITY OF WATER OF THE ARKANSAS RIVER IN OKLAHOMA AND ARKANSAS 1945-52 Prepared in cooperation with the University of Arkansas Engineering Experiment Station, Oklahoma Planning and Resources Board, Division of Water Resources, and the Oklahoma Agricultural and Mechanical College, Division of Engineering Research. UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director GEOLOGICAL SURVEY CIRCULAR 361 SUMMARY OF ANNUAL RECORDS OF CHEMICAL QUALITY OF WATER OF THE ARKANSAS RIVER IN OKLAHOMA AND ARKANSAS, 1945-52 By T. B. Dover and J. W. Geurin A PROGRESS REPORT Prepared in cooperation with the University of Arkansas Engineering Experiment Station, Oklahoma Planning and Resources Board, Division of Water Resources, and the Oklahoma Agricultural and Mechanical College, Division of Engineering Research Washington, D. C.,1955 Free on application to the Geological Survey, Washington 25, D. C. SUMMARY OF ANNUAL RECORDS OF CHEMICAL QUALITY OF WATER OF THE ARKANSAS RIVER IN OKLAHOMA AND ARKANSAS, 1945-52 A PROGRESS REPORT By T. B. Dover and J. W. Geurin CONTENTS Page Page Abstract.................................... 1 Chemical quality Continued Introduction............................... 4 Collection and examination of samples... Purpose and scope of report...... 4 Oklahoma-Kansas State line to Tulsa..... 14 Personnel and acknowledgments. 4 Influence of Salt Fork Arkansas River. 14 Arkansas River drainage basin...... 4 Influence of Cimarron River.............. 14 Location and extent.................. 4 Tulsa to Van Buren............................. 17 Physical and geologic features... 5 Influence of Verdigris, Neosho, and Oklahoma............................ 5 Illinois Rivers............................. 17 Arkansas............................. 5 Influence of Canadian River....... ....... 18 C lima te................................
    [Show full text]
  • Downstream Effects of Dams on Alluvial Rivers
    Downstream Effects of Downstream Effects of Dams on Alluvial Rivers By GARNETT P. WILLIAMS and M. GORDON WOLMAN GEOLOGICAL SURVEY PROFESSIONAL PAPER 1286 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1984 UNITED STATES DEPARTMENT OF THE INTERIOR WILLIAM P. CLARK, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director First printing 1984 Second printing 1985 Library of Congress Cataloging in Publication Data Williams, Garnett P. Downstream effects of dams on alluvial rivers. (Geological Survey Professional Paper; 1286) Includes bibliographical references. Supt. of Docs. No.: I 19.16:1286 1. River channels. 2. Rivers Regulation. 3. Dams. I. Wolman, M. Gordon (Markley Gordon), 1924- II. Title. III. Title: Alluvial rivers. IV. Series. TC175.W48 1983 551.48'2 82-600318 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract ......................... 1 Downstream effects of dams continued Introduction ....................... 1 Mean bed elevation Continued Scope of study ................... 1 Longitudinal-profile changes ............. 26 Study sites and selection criteria ......... 1 Bed material and degradation ................ 29 Acknowledgments .................. 2 Theoretical expectations ................. 29 Methods of analysis and data sources ......... 2 Variations in bed-material sizes with time at a cross sec­ Water discharge .................. 2 tion ........................... 29 Sediment load .................... 2 Variations in bed-material sizes with
    [Show full text]
  • Homogenization of Fish Faunas and Concurrent Anthropogenic Impacts on Plains Streams in Western Kansas: 1854–2003 Mark E
    Fort Hays State University FHSU Scholars Repository Fort Hays Studies Series 2007 Homogenization of Fish Faunas and Concurrent Anthropogenic Impacts on Plains Streams in Western Kansas: 1854–2003 Mark E. Eberle Fort Hays State University, [email protected] Follow this and additional works at: https://scholars.fhsu.edu/fort_hays_studies_series Part of the Biology Commons Recommended Citation Eberle, Mark E., "Homogenization of Fish Faunas and Concurrent Anthropogenic Impacts on Plains Streams in Western Kansas: 1854–2003" (2007). Fort Hays Studies Series. 74. https://scholars.fhsu.edu/fort_hays_studies_series/74 This Book is brought to you for free and open access by FHSU Scholars Repository. It has been accepted for inclusion in Fort Hays Studies Series by an authorized administrator of FHSU Scholars Repository. Fort Hays Studies Fort Fort Hays Studies Fourth Series Number 4 Fall 2007 4.4 Fall 2007 4.4 Fall Homogenization of Fish Homogenizations of Fish Faunas in W Homogenizations of Fish Faunas Faunas and Concurrent Anthropogenic Impacts on Plains Streams in Western estern Kansas: 1854–2003 Kansas: 1854–2003 www.fhsu.edu Copyright © 2007 by by Fort Hays State University Mark E. Eberle Fort Hays Studies Fourth Series Number 4 Fall 2007 Homogenization of Fish Faunas and Concurrent Anthropogenic Impacts on Plains Streams in Western Kansas: 1854–2003 by Mark E. Eberle Department of Biological Sciences Fort Hays State University Fort Hays Studies Fourth Series, Number 4, Fall 2007 Series Editor: Bradley Will Department of English Fort Hays State University Design, Layout, and Cover: Bradley Will Copyright © 2007 by Fort Hays State University Hays, Kansas 67601 www.fhsu.edu Support for this volume was provided by: Steven Trout Interim Dean of Graduate Studies and Research Fort Hays State University Larry Gould Provost Fort Hays State University Fort Hays State University is a thriving liberal and applied arts, state- assisted institution with an enrollment of about 8,000 students.
    [Show full text]
  • OWRB Stream System Management
    Oklahoma Surface Water Resources OWRB Water Rights Permitting - Stream System Management Basins 2-9-4 Boise City Texas Beaver Harper Buffalo Newkirk Nowata Miami Cimarron Alva Grant Washington Guymon Kay 2-5-4 Cherokee Medford 2-9-3 2-10-1 2-14 Bartlesville Ottawa Beaver 2-10-2 Craig Woods Ponca City 2-15-2 Pawhuska Nowata Alfalfa 2-12 Vinita Osage Woodward Jay 2-5-3 Enid Noble Pawnee 2-13 2-16 Woodward Pawnee Rogers Major Pryor Arkansas River Basin Red River Basin Fairview Garfield Perry Delaware Ellis Owasso Claremore Mayes 2-1, Poteau River 1-1, Red River Mainstem (To Kiamichi River) Arnett 2-11 Sand Springs Dewey 2-9-2 Stillwater 2-2, Lower Arkansas River 1-2, Little River (McCurtain County) Taloga Tulsa 2-15-1 2-9-1 Broken Arrow Adair Payne Sapulpa Cherokee 2-3, Lower Canadian River (To Lake Eufaula) 1-3, Kiamichi River Wagoner Kingfisher Tahlequah 2-6-3 Guthrie Wagoner 2-4, Middle Arkansas River 1-4-1, Muddy Boggy River Blaine Kingfisher 2-4 Tulsa 2-17 Stilwell Watonga Creek Roger Mills Logan 2-5-1, Lower North Canadian River 1-4-2, Clear Boggy Creek Muskogee Chandler 2-5-2, Middle North Canadian River 1-5, Red River Mainstem (To Blue River) 2-5-2 Canadian Edmond 1-8-4 Custer 2-7 Okmulgee Muskogee Cheyenne Arapaho Oklahoma 2-5-3, Upper North Canadian River 1-6, Blue River Weatherford El Reno Yukon Bethany Lincoln Okfuskee Sequoyah Oklahoma City Okmulgee Elk City Del City Sallisaw 2-5-4, North Canadian Headwaters 1-7, Red River Mainstem (To Washita) Okemah Midwest City Washita Mustang 2-6-1, Lower Canadian River 1-8-1, Lower Washita
    [Show full text]
  • KOARC 2017 Engg Comm
    KANSAS-OKLAHOMA ARKANSAS RIVER COMPACT COMMISSION ENGINEERING COMMITTEE REPORT July 28, 2021 Oklahoma Water Resources Board Oklahoma City, OK This report covers water year (WY) 2020: October 1, 2019 through September 30, 2020. The report contains the standard updates to streamflow data, water quality data and reservoir conservation storage capacities constructed in the Compact area. WY2020 mean flows at four of the five Oklahoma gaging stations were lower than WY2019 mean flows. At the Cimarron River gage near Waynoka, OK, the WY2020 mean flow was 115 cfs, an 81% decrease from the WY2019 mean flow of 607 cfs. Three of the other Oklahoma gaging stations reported decreases in mean flow ranging from 42% to 70% between WY2019 and WY2020. Due to a bridge reconstruction project, the fifth Oklahoma gaging station – the Chikaskia River gage near Blackwell, OK – was not in operation from April 2, 2020 through the end of the water year. The Verdigris River gage at Independence, KS reported a 51% decrease in mean flow, from 6,302 cfs in WY2019 to 3,080 cfs in WY2020. The Arkansas River gage at Arkansas City, KS reported a 76% decrease in mean flow, from 6,962 cfs in WY2019 to 1,655 cfs in WY2020. WY2020 mean flows at the gaging stations in Kansas and Oklahoma varied in relation to the historical mean flows at those gaging stations, ranging from a 57% decrease at the Cimarron River gage near Waynoka, OK to a 36% increase at the Verdigris River gage near Independence, KS. The Engineering Committee reports that there were no new water storage structures completed in the Kansas or Oklahoma Compact areas between October 1, 2019 and September 30, 2020 that exceeded the 100-acre-foot conservation storage minimum requirement as set forth in the Compact.
    [Show full text]
  • Robert Edward Pearce Date of Degree: May 23, 1965
    Name: Robert Edward Pearce Date of Degree: May 23, 1965 Institution: Oklahoma State University Location: Stillwater, Oklahoma Title of Study: ·western Distribution of Platanus occidentalis L. in Oklahoma Pages in Study: 42 Candidate for Degree of Master of Natural Science Major Field: Natural Science. Scope and Method of Study: Determine the Western Distribution of Platanus occidentalis L. in Oklahoma. This was accomplished by making trips into Love, Carter, Murray, Garvin, McClain, Cleveland, Pontotoc, Seminole, Pottawatomine, Lincol;tn, Logan, Payne, Pawnee, Kay, and Grant Counties. Collections were made to verify the location. A distribution map of plant collected and they are on deposit in the Bebb Herbarium of the University of Oklahoma. A study was made of the unpublished Paper of the Ecology of the Bottomland of Oklahoma by Rice (1962). Findings and Conclusions: P. occidentalis L. are found along most of the creeks and rivers in the eastern half of the counties above. More abundant growth is along larger and wider creeks and rivers in the counties mentioned. P. ocd.dentalis L. are found growing with other species of trees. Few young trees were found in the narrow creeks. More trees were growing on limestone soils. ~ occidentalis L. are found to be more abundant to the east of the distri­ bution found in this paper. Adviser's Approval: WESTERN DISTRIBUTION OF PLATANUS OCCIDENTALIS L. IN OKLAHOMA By ROBERT EDWARD PEARCE Bachelor of Science Oklahoma State University Stillwater, Oklahoma 1954 Submitted to the faculty of the Graduate School of the Oklahoma State University in partial fulfillment of the requirements for the degree of MASTER OF NATURAL SCIENCE May, 1965 THE WESTERN DISTRIBUTION OF THE PLATANUS OCCIDENTALIS 1.
    [Show full text]