Tion and Increase of Drought Conditions Over Most of on Julv 16, More Than 5 Inches of Rain at Oberlin
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Thursday, June 15, 2017 Thursday, June 15, 2017 2016 Integrated Report - Walsh County
Thursday, June 15, 2017 Thursday, June 15, 2017 2016 Integrated Report - Walsh County Thursday, June 15, 2017 Cart Creek Waterbody ID Waterbody Type Waterbody Description Date TMDL Completed ND-09020310-044-S_00 RIVER Cart Creek from its confluence with A tributary 2 miles east of Mountain, ND downstream to its confluence with North Branch Park River Size Units Beneficial Use Impaired Beneficial Use Status Cause of Impairment TMDL Priority 36.32 MILES Fish and Other Aquatic Biota Not Supporting Fishes Bioassessments L ND-09020310-044-S_00 RIVER Cart Creek from its confluence with A tributary 2 miles east of Mountain, ND downstream to its confluence with North Branch Park River Size Units Beneficial Use Impaired Beneficial Use Status Cause of Impairment TMDL Priority 36.32 MILES Fish and Other Aquatic Biota Not Supporting Benthic-Macroinvertebrate Bioassessments L Forest River Waterbody ID Waterbody Type Waterbody Description Date TMDL Completed ND-09020308-001-S_00 RIVER Forest River from Lake Ardoch, downstream to its confluence with the Red River Of The North. Size Units Beneficial Use Impaired Beneficial Use Status Cause of Impairment TMDL Priority 15.49 MILES Fish and Other Aquatic Biota Not Supporting Benthic-Macroinvertebrate Bioassessments L ND-09020308-001-S_00 RIVER Forest River from Lake Ardoch, downstream to its confluence with the Red River Of The North. Size Units Beneficial Use Impaired Beneficial Use Status Cause of Impairment TMDL Priority 15.49 MILES Fish and Other Aquatic Biota Not Supporting Fishes Bioassessments L ND-09020308-001-S_00 RIVER Forest River from Lake Ardoch, downstream to its confluence with the Red River Of The North. -
Streamflow Depletion Investigations in the Republican River Basin: Colorado, Nebraska, and Kansas
J. ENVIRONMENTAL SYSTEMS, Vol. 27(3) 251-263, 1999 STREAMFLOW DEPLETION INVESTIGATIONS IN THE REPUBLICAN RIVER BASIN: COLORADO, NEBRASKA, AND KANSAS JOZSEF SZILAGYI University of Nebraska–Lincoln ABSTRACT Water is a critical resource in the Great Plains. This study examines the changes in long-term mean annual streamflow in the Republican River basin. In the past decades this basin, shared by three states, Colorado, Nebraska, and Kansas, displayed decreased streamflow volumes as the river enters Kansas across the Nebraska-Kansas border compared to values preceding the 1950s. A recent lawsuit filed by Kansas challenges water appropriations in Nebraska. More than half of the source area for this water, however, lies outside of Nebraska. Today a higher percentage of the annual flow is generated within Nebraska (i.e., 75% of the observed mean annual stream- flow at the NE-KS border) than before the 1950s (i.e., 66% of the observed mean annual streamflow) indicating annual streamflow has decreased more dramatically outside of Nebraska than within the state in the past fifty years. INTRODUCTION The Republican River basin’s 64,796 km2 drainage area is shared by three states: Colorado, Nebraska, and Kansas (see Figure 1). Nebraska has the largest single share of the drainage area, 25,154 km2 (39% of total); Colorado can claim about 20,000 km2 (31%), while the rest, about 19,583 km2 (30%), belongs to Kansas [1], from which about 12,800 km2 (20%) lies upstream of Hardy, near the Nebraska-Kansas border. Exact figures for the contributing drainage areas (portions of the drainage areas that actually contribute water to the stream) are hard to obtain because these areas in the headwater sections of the basin have been shrinking constantly in the past fifty years. -
Fishing the Red River of the North
FISHING THE RED RIVER OF THE NORTH The Red River boasts more than 70 species of fish. Channel catfish in the Red River can attain weights of more than 30 pounds, walleye as big as 13 pounds, and northern pike can grow as long as 45 inches. Includes access maps, fishing tips, local tourism contacts and more. TABLE OF CONTENTS YOUR GUIDE TO FISHING THE RED RIVER OF THE NORTH 3 FISHERIES MANAGEMENT 4 RIVER STEWARDSHIP 4 FISH OF THE RED RIVER 5 PUBLIC ACCESS MAP 6 PUBLIC ACCESS CHART 7 AREA MAPS 8 FISHING THE RED 9 TIP AND RAP 9 EATING FISH FROM THE RED RIVER 11 CATCH-AND-RELEASE 11 FISH RECIPES 11 LOCAL TOURISM CONTACTS 12 BE AWARE OF THE DANGERS OF DAMS 12 ©2017, State of Minnesota, Department of Natural Resources FAW-471-17 The Minnesota DNR prohibits discrimination in its programs and services based on race, color, creed, religion, national origin, sex, public assistance status, age, sexual orientation or disability. Persons with disabilities may request reasonable modifications to access or participate in DNR programs and services by contacting the DNR ADA Title II Coordinator at [email protected] or 651-259-5488. Discrimination inquiries should be sent to Minnesota DNR, 500 Lafayette Road, St. Paul, MN 55155-4049; or Office of Civil Rights, U.S. Department of the Interior, 1849 C. Street NW, Washington, D.C. 20240. This brochure was produced by the Minnesota Department of Natural Resources, Division of Fish and Wildlife with technical assistance provided by the North Dakota Department of Game and Fish. -
Republican River Valley and Adjacent Areas, Nebraska
A, Economic Geology, 97 B, Descriptive Geology 119 M, General Hydrograpmc investigations, 26 (0, Underground Waters, 72 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES I>. WALOOTT, DIKECTOR GEOLOGY AND WATER RESOURCES OF THE REPUBLICAN RIVER VALLEY AND ADJACENT AREAS, NEBRASKA G. E. CONDRA -FERTY OF -LOGICAL Sl'». WASHINGTON (GOVERNMENT PRINTING OFFICE 1907 CONTENTS. Page. Introduction __'___________________________________ 7 Geography _____________________________________ 8 Topography______________________.._ 8 Drainage _____________________________.____ 8 Climate "_________________________ _ _________ ._..__ 9 Temperature_______l_____________________ 9 Rainfall _____________________________________ 9 Winds_____________________________________ 10 Descriptive geology ________________________________ 10 General relations _____ _________ ___ ________ 10 Structure____________________________ 11 Description of the rocks____ ______________________ 11 Carboniferous system_______________________ 11 Cretaceous system.__________________________ 12 Dakota formation_________________________ 12 Character and thickness______________ 12 Distribution_________________ 13 Benton group________________________ 13 Members represented________________ 13 Graneros shale_ ________________________ 14 Character and thickness_________________ 14 Exposures,_________ _______ _-_________ 14 Greenhorn limestone_____________________ 14 Character and thickness___________________ 14 Fossils_________________________ 16 Carlile shale______.___________________ -
Approaches to Setting Nutrient Targets in the Red River of the North
APPROACHES TO SETTING NUTRIENT TARGETS IN THE RED RIVER OF THE NORTH Topical Report RSI-2328 prepared for International Joint Commission 1250 23rd St. NW, Room 100 Washington, DC 20440 March 2013 APPROACHES TO SETTING NUTRIENT TARGETS IN THE RED RIVER OF THE NORTH Topical Report RSI-2328 by Andrea B. Plevan Julie A. Blackburn RESPEC 1935 West County Road B2, Suite 320 Roseville, MN 55113 prepared for International Joint Commission 1250 23rd St. NW, Room 100 Washington, DC 20440 March 2013 EXECUTIVE SUMMARY The International Joint Commission, through its International Red River Board (IRRB), has developed a proposed approach for a basinwide nutrient management strategy for the international Red River Watershed. One component of the nutrient management strategy involves developing nitrogen and phosphorus targets along the Red River including sites at the outlet of the Red River into Lake Winnipeg, the international boundary at Emerson, and subwatershed discharge points in the watershed. These nutrient objectives will be coordinated with developing nutrient objectives for Lake Winnipeg. As a first step in developing the nutrient targets, the IRRB contracted RESPEC to conduct a literature review of the available scientific methods for setting nitrogen and phosphorus water-quality targets. Based on the findings of the literature review, RESPEC was asked to provide recommendations on the method(s) most appropriate for the Red River. This report includes the findings of the literature review and the recommended scientific approaches for developing nitrogen and phosphorus targets in the Red River. Multiple technical approaches were reviewed. One category of approaches uses the reference condition and includes techniques such as using data from reference sites, modeling the reference condition, estimating the reference condition from all sites within a class, and paleolimnological techniques to reconstruct the reference condition through historical data. -
NWSI 10-903, Geographic Areas Of
Department of Commerce • National Oceanic & Atmospheric Administration • National Weather Service NATIONAL WEATHER SERVICE INSTRUCTION 10-903 JULY 26, 2019 Operations and Services Water Resources Services Program, NWSPD 10-9 GEOGRAPHIC AREAS OF RESPONSIBILITY NOTICE: This publication is available at: http://www.nws.noaa.gov/directives/ OPR: W/AFS25 (K. Abshire) Certified by: W/AFS25 (M. Mullusky) Type of Issuance: Routine. SUMMARY OF REVISIONS: This directive supersedes NWS Instruction 10-903, “Geographic Areas of Responsibility,” dated February 16, 2017. The following revisions were made to this instruction: 1) In Section 2, updated the link to the RFC boundary shapefiles from the NWS geographic information system (GIS) Portal. 2) In Section 2, updated the location of the Northeast RFC (NERFC) from Taunton to Norton, Massachusetts. 3) In Section 3, updated Figure 2 to show correct Hydrologic Service Area (HSA) boundaries and Weather Forecast Office three-letter identifiers. 4) In Section 3, updated the link to the national Hydrologic Service Area (HSA) map from the NWS geographic information system (GIS) Portal. 5) In Section 3, modified wording to describe the Boston/Norton, MA (BOX), Gray/Portland, ME (GYX), Nashville, TN (OHX) service areas and updated the office names of the New York, NY (OKX) and Philadelphia/Mt. Holly, PA (PHI) offices. Signed 7/12/2019 Andrew D. Stern Date Director Analyze, Forecast, and Support Office NWSI 10-903 JULY 26, 2019 Geographic Areas of Responsibility Table of Contents: Page 1. Introduction ................................................................................................................................1 -
Lateral Migration of the Red River, in the Vicinity of Grand Forks, North Dakota Dylan Babiracki
University of North Dakota UND Scholarly Commons Undergraduate Theses and Senior Projects Theses, Dissertations, and Senior Projects 2015 Lateral Migration of the Red River, in the Vicinity of Grand Forks, North Dakota Dylan Babiracki Follow this and additional works at: https://commons.und.edu/senior-projects Recommended Citation Babiracki, Dylan, "Lateral Migration of the Red River, in the Vicinity of Grand Forks, North Dakota" (2015). Undergraduate Theses and Senior Projects. 114. https://commons.und.edu/senior-projects/114 This Thesis is brought to you for free and open access by the Theses, Dissertations, and Senior Projects at UND Scholarly Commons. It has been accepted for inclusion in Undergraduate Theses and Senior Projects by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. | 1 Lateral migration of the Red River, in the vicinity of Grand Forks, North Dakota Dylan Babiracki Harold Hamm School of Geology and Geologic Engineering, University of North Dakota, 81 Cornell St., Grand Forks, ND 58202-8358 1. Abstract River channels are dynamic landforms that play an important role in understanding the alluvial changes occurring within this area. The evolution of the Red River of the North within the shallow alluvial valley was investigated within a 60 river mile area north and south of Grand Forks, North Dakota. Despite considerable research along the Red River of the North, near St. Jean Baptiste, Manitoba, little is known about the historical channel dynamics within the defined study area. A series of 31 measurements were taken using three separate methods to document the path of lateral channel migration along areas of this highly sinuous, low- gradient river. -
Republican River Basin-Wide Plan
Republican River Basin-Wide Plan Jointly developed by the Upper Republican, Middle Republican, Lower-Republican, and Tri-Basin Natural Resources Districts and the Nebraska Department of Natural Resources 2019 Republican River Basin-Wide Plan Table of Contents 1. Introduction ............................................................................................................................. 4 Effective Date and Time Frame of the Plan ............................................................................................................... 4 Authority ................................................................................................................................................................................. 4 Background, Purpose, and Intent .................................................................................................................................. 5 Vision Statement for the Plan ........................................................................................................................ 5 Mission Statement for the Plan ..................................................................................................................... 5 Integrated Management Plans and Basin-Wide Plan in the Basin ................................................................... 6 Planning Process .................................................................................................................................................................. 9 Responsibilities and Authorities -
History of North Dakota Chapter 6
The Beginnings of Settlements 109 CHAPTER 6 The Beginnings of Settlement THE FIRST PORTION OF NORTH DAKOTA to be settled was the valley of the Red River of the North. Except for the Selkirk colonists and the metis about Pembina, agricultural settlement came with the advance of the American frontier. When restless farmers, seeking cheap land, had taken over southern Minnesota, they turned next to the fertile lands of the Red River Valley. Their coming was stimulated by the opening of a new transportation system. Remoteness was a crucial problem at the Selkirk settlement. Its people, métis and white, wanted easy access to outside markets. At first they were supplied by way of Hudson Bay, but that was costly and the Hudson's Bay Company itself sought a cheaper route. St. Paul, more accessible than the Bay, wanted to make the Selkirk colony its commercial hinterland. When the cheaper route to the Selkirk settlement by way of St. Paul won out over the more costly one by way of the Bay, the valley of the Red River became a trade route. Cart trails, the steamboat line, and then the railroad ran through it. These opened the portion of the valley south of the international boundary and brought in settlers. The process advanced in three steps. The first as the growth of the metis settlement at Pembina and St. Joseph. There the metis had freer access both to St. Paul and to the buffalo herds on the American side of the boundary. The Pembina-St. Joseph settlement was also an American 110 History of North Dakota gateway to the Selkirk colony to the north. -
Red River Trails
Red River Trails by Grace Flandrau ------... ----,. I' , I 1 /7 Red River Trails by Grace Flandrau Compliments of the Great Northern Railway The Red River of the North Red River Trails by Grace Flandrau Foreword There is a certain hay meadow in southwestern Minnesota; curiously enough this low-lying bit of prairie, often entirely submerged, happens to be an important height of land dividing the great water sheds of Hudson's Bay and Mississippi riv,er. I t lies between two lakes: One of these, the Big Stone, gives rise to the Minnesota river, whose waters slide down the long tobog gan of the Mississippi Valley to the Gulf of Mexico; from the other, Lake Traverse, flows the Bois de Sioux, a main tributary of the Red River of the North, which descends for over five. hundred miles through one of the richest valleys in the world to Lake Winnipeg and eventually to Hudson's Bay. In the dim geologic past, the melting of a great glacier ground up limestone and covered this valley with fertile deposits, while the glacial Lake Agassiz subsequently levelled it to a vast flat plain. Occasionally in spring when the rivers are exceptionally high, the meadow is flooded and becomes a lake. Then a boatman, travelling southward from the semi-arctic Hudson's Bay, could float over the divide and reach the Gulf of Mexico entirely by water route. The early travellers gave, romantic names to the rive.rs of the West, none more so, it seems to me, than Red River of the North, 3 with its lonely cadence, its suggestion of evening and the cry of wild birds in far off quiet places. -
Red River of the North “A Winding Journey to History
RED RIVER OF THE NORTH “A WINDING JOURNEY TO HISTORY” Headwaters at Breckenridge, Minnesota, U.S.A. By NEOMA A. LAKEN 2010 CONTENTS WELCOME FOREWORD INTRODUCTION CHAPTER 1 General Information CHAPTER 2 Prehistoric Heritage CHAPTER 3 Converging Rivers CHAPTER 4 Steamboats, Flatboats & Barges CHAPTER 5 Graham’s Point, Pre-1819 Trading Post CHAPTER 6 Red River Oxcarts CHAPTER 7 Fort Abercrombie, Dakota Territory CHAPTER 8 Sister River Cities: Breckenridge, MN Wahpeton, ND CHAPTER 9 Red River of the North Flooding CHAPTER 10 Flora and Fauna CHAPTER 11 Renewed Vision for the Red River of the North EPILOG REFERENCES - 2 - WELCOME... Breckenridge, Wilkin County, Minnesota, United States of America, and Wahpeton, Richland County, North Dakota, United States of America, welcome you to the Red River of the North. Some of the information contained comes from the records in the office of the County Recorder, in the Wilkin County Courthouse, Breckenridge MN. Some is local historical lore passed on to generations throughout the years and told to the author. While yet other information is a meshing of historical facts. As with the telling of any history, sagas differ slightly with the various perspectives of the authors. I hope you will find your visit to the Red River of the North a pleasant one. Enjoy your visit . and come back soon! Neoma A. Laken, Author 108 North 15th Street Breckenridge, Minnesota 56520 United States of America All rights in and to this book reserved by author. No portion may be reprinted without permission. Additional copies of this book are available from River Keepers, 325 7th St South, Fargo, ND 58103, www.riverkeepers.org for a cost of $10. -
Regression Equations
NDOR Research Project Number SPR-1(2) P541 Transportation Research Studies REGRESSION EQUATIONS Branden J. Strahm and David M. Admiraal University of Nebraska – Lincoln W355 Nebraska Hall Lincoln, NE 68588-0531 Telephone (402) 472-8568 FAX (402) 472-8934 Sponsored by The Nebraska Department of Roads 1500 Nebraska Highway 2 Lincoln, Nebraska 68509-4567 Telephone (402) 479-4337 FAX (402) 479-3975 August 2005 Technical Report Documentation Page 1. Report No. 2. Government Accession No. 3. Recipient’s Catalog No. SPR-1(2) P541 4. Title and Subtitle 5. Report Date Regression Equations August 2005 6. Performing Organization Code 7. Author/s 8. Performing Organization Report No. Branden J. Strahm and David M. Admiraal 9. Performing Organization Name and Address 10. Work Unit No. (TRAIS) Department of Civil Engineering University of Nebraska – Lincoln 11. Contract or Grant No. W348 Nebraska Hall SPR-1(2) P541 Lincoln, NE 68588-0531 12. Sponsoring Organization Name and Address 13. Type of Report and Period Covered U.S. Department of Transportation Final Report Research and Special Programs Administration 400 7th Street, SW Washington, DC 20590-0001 14. Sponsoring Agency Code 15. Supplementary Notes 16. Abstract Regional regression equations were developed to estimate peak-flow magnitudes using Geographic Information systems (GIS). Peak discharges were estimated at return intervals ranging from 2- to 500-years in Nebraska. Flow data from gaging stations located in or within 50 miles of Nebraska were collected. Regional regression analysis, using weighted-least squares (WLS) regression and data from 273 gaging stations, were used to develop equations for seven hydrologic regions.