Lakes of Missouri Volunteer Program

Slides:



Advertisements
Similar presentations
Lakes of Missouri Volunteer Program University of Missouri-Columbia The Missouri’s Lakes and Reservoirs The Missouri Department of Natural Resources Region.
Advertisements

Prioritization Workgroup Summary. Workgroup Topics Nutrient results What is a watershed? What is a TMDL? Prioritization methods Basin framework and management.
Limnology 101 Dan Obrecht MU Limnology
Missouri’s Oxbow Lakes Georganne Bowman Water Protection Program DNR January 24, 2006.
Wastewater Storage Pond Design
1 Overview of Water Law and Policy University of San Francisco School of Law Water Law Class 1 January 13, 2010 David Sandino Chief Counsel California.
Developing Nutrient Criteria – Divide and Conquer! Dan Obrecht, MU Limnology.
Investigation of Seasonal Hydrology and Variable Source Areas within Regions of Ontario Ramesh Rudra (R.P. Rudra, B. Gharabaghi, S, Gregori, W.T. Dickinson)
Engineering Hydrology Discussion Ch. #1
4 th International Symposium on Flood Defence, 6 th – 8 th May 2008, Toronto, Canada Efficiency of distributed flood mitigation measures at watershed scale.
City of Kimball Stormwater Re-use Project Protecting our Water Resources – a Forum Series for Policy Makers March 30, 2011.
Crater Lake, Oregon -589 m deep and possibly the clearest lake in the world, Transparency up to 90 m. Thermocline very deep for its size No rooted plants.
Assignment 2 -Lake Watersheds and morphometry Elkwater lake is a small lake situated near Cypress Hills Provincial Park. The watershed is mostly forested.
The Hydrologic (Water) Cycle. Surface Water Oceans Rivers and streams Lakes and ponds Springs – groundwater becomes surface water.
Engineering Hydrology (ECIV 4323)
River Rainfall Runoff G.W.T Main objectives of the project: Designing the irrigation system for a specific area. The first step is to determine the water.
Agricultural Nonpoint Source Pollution and Water Quality as a function of Land Management Practices on Four Kansas Farms William W. Spotts Dr. Donald Huggins.
Pomme de Terre Lake Water Quality Summary Pomme de Terre Lake Water Quality Summary US Army Corps of Engineers Environmental Resources Section.
Through funds made available from a 319 grant focused on water quality issues in the Spring River Watershed, plans for a demonstration Rain Garden were.
Jefferson High School Compton Creek Research Project UCLA and Los Angeles Waterkeeper Funded by the Environmental Protection Agency.
URBAN AND NATURAL ENVIRONMENT CONSULTANTS European Commission 6 th Framework Programme for research and Technological Development Optimisation For Sustainable.
Nile Hydrology Preliminary Research Anthony Makana Paris
EEOS 350: Quantitative hydrogeology Lecture 2 Water balance.
Applying Methods for Assessing the Costs and Benefits of CCA 2 nd Regional Training Agenda, 30 September – 4 October 2013 Priyanka Dissanayake- Regional.
Northwest hydraulic consultants 2NDNATURE Geosyntec Consultants September 11, 2007 Urban Upland / Groundwater Source Category Group (UGSCG) Overview Presentation.
HOUSEHOLD WATER USE Landscaping (lawns and gardens) account for about 50% of our water use. Showers account for 18% Toilets use about 20% Central Valley.
Watershed Management Water Budget, Hydrograph Analysis
Concerns about the Current Approach to Nutrient Criteria.
Nutrient Criteria for the plains regions of Missouri.
Highlights A Study of Phosphorus Loading of Ballston Lake by Tributary Inflow Presentation to BLIA Annual Meeting June 16, 2014 Scott Miller, Bob Duncan,
Yellowtail Dam & Bighorn Lake Climate Change Billings, MT September, 2010 RECLAMATION Managing Water in the West.
Water Quality Short Course April 11, 2007 Lake and Reservoir Dynamics Dan Obrecht – UMC
Secondary Site Locations on Large Reservoirs Issue 1 – How to select tributary arms for criteria monitoring Missouri’s large reservoirs are highly dendritic.
Management of Lake Fertő H idrology and water management University of Debrecen Centre for Environmental Management and Policy 7. Lakepromo Meeting & Seminar.
Gilfillan Lake: Sustainable Lake Management Plan Meeting 1 April 22, 2009.
Lab 13 - Predicting Discharge and Soil Erosion Estimating Runoff Depth using the Curve Number method –Land use or cover type –Hydrologic condition –Soil.
Integrated Ecological Assessment February 28, 2006 Long-Term Plan Annual Update Carl Fitz Recovery Model Development and.
An Overview of Air, Water & Soil in Agriculture Barbara McCarthy, Ph.D. Environmental Health Department Colorado State University.
Reservoir and Lake Nutrient Criteria A Different Approach D.V. Obrecht, J.R. Jones & M.K. Knowlton – MU Limnology.
Missourians come from…. many countries Missouri’s legislative branch is called.
Estuaries November 10. Flushing time (or residence time): time required to replace water with “new” water. Several ways to compute: Flushing time (or.
Waterbody Classification Project A project of the Lakes and Watershed Commission, Dane County Department of Planning and Development, and the Dane County.
URBAN HYDROLOGY. URBAN FABRIC RUNOFF PROCESSES AND DRAINAGE CHANNELS.
Surface Water Surface runoff - Precipitation or snowmelt which moves across the land surface ultimately channelizing into streams or rivers or discharging.
 Areas affected by the California Water Project spread from Northern California to Southern Califronia.  750,000 acres of irrigated farmland.
WATERSHEDS Concepts and Curriculum Review LAKE MONITORING AND ANALYSIS Tony Thorpe and Dan Obrecht Lakes of Missouri Volunteer Program – Univ. of Missouri.
Nutrient Criteria for Reservoirs – A Review of Missouri’s Proposed Approach Daniel V. Obrecht Dept. of Fisheries and Wildlife Sciences University of Missouri.
Sanitary Engineering Lecture 4
Interpreting a contour map
Water Pollution Lecture by Dr. Ken Galli, Boston College EESC116301
CLIMATE CHANGE Consequences for Alpine Lakes & Management
S Curves From Mays, 2011, Ground and Surface Water Hydrology.
CEE 3430, Engineering Hydrology David Tarboton
Nutrient Benchmark Development
URBAN NON-POINT SOURCE NUTRIENT IMPACTS
INTRODUCTION TO HYDROLOGY
Surface Runoff and Hydrograph Components
SCS Dimensionless Unit Hydrograph
Review of Flood Reservoir Routing
Total Phosphorus in Large Reservoirs
SCS Dimensionless Unit Hydrograph
Hydrology CIVL341.
Hydrology CIVL341 Introduction
How are lakes and streams similar? How are they different?
What is the percentage of global precipitation falling on the land?
An Najah National University Faculty of Engineering
What is the percentage of global precipitation falling on the land?
Missouri Nutrient Criteria Development
Hydrology CIVL341 Introduction
The Impact of Water Clarity on Home prices in Manitowoc County
Presentation transcript:

Lakes of Missouri Volunteer Program Lake Morphology and Hydrology The Lakes of Missouri Volunteer Program University of Missouri-Columbia The Missouri Department of Natural Resources Region V11, US Environmental Protection Agency, through the Missouri Department of Natural Resources, has provided partial funding for this project under Section 319 of the Clean Water Act

Lake Morphology/Hydrology Surface Area Depth Volume Watershed Area Flushing Rate

Ranges from 6 to 53,814 acres in size, with a median of 103 acres. Surface Area Depth Volume Watershed Area Flushing Rate Surface Area Ranges from 6 to 53,814 acres in size, with a median of 103 acres.

Surface Area of Classified Lakes Depth Volume Watershed Area Flushing Rate Surface Area of Classified Lakes 30% of classified lakes are 20 acres or less in size. 10% are greater than 300 acres in size.

Depth (determined by dam height) Surface Area Depth Volume Watershed Area Flushing Rate Depth (determined by dam height)

Ranges from 3.7 feet to 62 feet, with a median of 11.6 feet. Surface Area Depth Volume Watershed Area Flushing Rate Average Depth Ranges from 3.7 feet to 62 feet, with a median of 11.6 feet.

Why is depth important? Shallow lakes may mix sporadically throughout the summer, leading to more internal loading of nutrients. A deeper lake has a larger volume of water, which influences hydrology.

Lake Volume (determined by area and depth) Surface Area Depth Volume Watershed Area Flushing Rate Lake Volume (determined by area and depth)

Lake Volume Ranges from 48 to 2,700,000 acre-feet, with a median of 1,675 acre-feet. 1 acre 1 foot 1 acre-foot = 325,851 gallons

Same inflow volume, different Lake Volume Surface Area Depth Volume Watershed Area Flushing Rate Same inflow volume, different Lake Volume Dam height and topography determine the lake volume

Watershed Area (catchment size) Surface Area Depth Volume Watershed Area Flushing Rate Watershed Area (catchment size)

Ranges from 83 to > 4,000,000 acres, with a median of 2,516 acres. Watershed Area Ranges from 83 to > 4,000,000 acres, with a median of 2,516 acres.

Same size lake, but with different inflow volumes Surface Area Depth Volume Watershed Area Flushing Rate Same size lake, but with different inflow volumes Inflow is determined by the watershed area and rainfall

Surface Area Depth Volume Watershed Area Flushing Rate Flushing Rate - the proportion of the total lake volume that is replaced (per year) by inflowing water. Flushing Rate = Regional Runoff Coefficient * Watershed Area / Lake Volume

Ranges from 140 to 0.1, with a median of 1.1 Surface Area Depth Volume Watershed Area Flushing Rate Flushing Rate Ranges from 140 to 0.1, with a median of 1.1

Flushing Rate = 0.5 Flushing Rate = 1 Flushing Rate = 2 Annual Inflow / Volume = Flushing Rate inflow 50 outflow 50 Volume 100 Flushing Rate = 0.5 Volume 100 outflow 100 inflow 100 Flushing Rate = 1 outflow 200 inflow 200 Volume 100 Flushing Rate = 2

Why is Flushing Rate important? Flushing Rate is used to gauge inputs relative to lake volume. A 100 acre lake with a low flushing rate has fewer inputs than a 100 acre lake with a high flushing rate.

Same lake volume, different Inflow Volume Surface Area Depth Volume Watershed Area Flushing Rate Same lake volume, different Inflow Volume High Flushing Rate Low Flushing Rate

Same inflow volume, different Lake Volume Surface Area Depth Volume Watershed Area Flushing Rate Same inflow volume, different Lake Volume High Flushing Rate Low Flushing Rate

Quick Ecoregion Overview

Missouri’s Physiographic Regions Glacial and Osage Plains Ozark Border Ozark Highlands

Average Phosphorus Values (for physiographic regions) Region Phosphorus (ug/L) Glacial Plains 44 Osage Plains 73 Ozark Border 40 Ozark Highlands 17