Towards a Stream Classification System for the Canadian Prairie Provinces CWRA-CGU National Conference, Banff, Alberta June 5-8, 2012 Greg MacCulloch and.

Slides:



Advertisements
Similar presentations
Science to Sustain At-Risk Terminal Lakes Walker River Basin Project In Cooperation with the Bureau of Reclamation Legislative Committee on Public Lands.
Advertisements

GSA Northeastern Meeting March , 2013 Bretton Woods, NH A Comparison between Runoff Trends in a Headwater Basin and More Developed Watersheds: A.
North Saskatchewan River Planning Area Hydrology Bart Oegema, MASc, PEng Senior Hydrologist, SWA November 24-25, 2004.
Precipitation - Runoff Relations Watershed Morphology
U.S. Department of the Interior U.S. Geological Survey Streamflow conditions across North Carolina Assessment of hydrologic conditions observed through.
Bankfull / Effective / Dominant
4 th International Symposium on Flood Defence Generation of Severe Flood Scenarios by Stochastic Rainfall in Combination with a Rainfall Runoff Model U.
MARMOT CREEK RESEARCH BASIN WORKSHOP BARRIER LAKE FIELD STATION FEBRUARY 2013.
1 Assiniboine River Water Demand and Water Supply Studies Prepared by : Bob Harrison, P. Eng. and Abul Kashem, P. Eng. Surface Water Management Section.
Climate Change Impacts on the Water Cycle Emmanouil Anagnostou Department of Civil & Environmental Engineering Environmental Engineering Program UCONN.
Annual Unit Runoff in Canada Presentation at PPWB Prairie Hydrology Workshop January 29, 2013.
Alberta Rainfall-Runoff Analysis September, 2002.
2012 Southwest Wildfire Hydrology and Hazards Workshop Evan Friedman and Dr. Paul Santi Colorado School of Mines 3 April 2012.
SENSORS, CYBERINFRASTRUCTURE, AND EXAMINATION OF HYDROLOGIC AND HYDROCHEMICAL RESPONSE IN THE LITTLE BEAR RIVER OBSERVATORY TEST BED Jeffery S. Horsburgh.
IDWR Water Supply Meeting May 12, 2011 NRCS Snow Survey Measuring Lost Lake SNOTEL Site, elevation 6,110 feet, along the NF Clearwater and St Joe Divide.
Dennis P. Lettenmaier Lan Cuo Nathalie Voisin University of Washington Climate Impacts Group Climate and Water Forecasts for the 2009 Water Year October.
Hydrological Modeling FISH 513 April 10, Overview: What is wrong with simple statistical regressions of hydrologic response on impervious area?
Mark Williams, CU-Boulder Using isotopes to identify source waters: mixing models.
Alan F. Hamlet Andy Wood Seethu Babu Marketa McGuire Dennis P. Lettenmaier JISAO Climate Impacts Group and the Department of Civil Engineering University.
Analyses of Rainfall Hydrology and Water Resources RG744
Paonia/Collbran Low Flow Presentation Water Quality Work Group Meeting June 9, 2004.
Impact of Climate Change on Flow in the Upper Mississippi River Basin
WaterSmart, Reston, VA, August 1-2, 2011 Steve Markstrom and Lauren Hay National Research Program Denver, CO Jacob LaFontaine GA Water.
Overview of the Colorado River Basin Water Supply and Demand Study Urban Water Institute 19 th Annual Water Policy Conference August 22-24, 2012 San Diego.
Analysis of extreme precipitation in different time intervals using moving precipitation totals Tiina Tammets 1, Jaak Jaagus 2 1 Estonian Meteorological.
The Colorado Surface Water Supply Index (SWSI) Performance Since 1981 Nolan Doesken Colorado State Climatologist Colorado Climate Center Colorado State.
Hydrologic Change in the Lower Flint River Basin and Responses of Freshwater Mussels to Drought S.W. Golladay and D.W. Hicks J. W. Jones Ecological Research.
New Mexico Rio Grande Water Operations Modeling: Creating a synthetic flow sequence representative of regional paleo-hydrology for alternatives analysis.
Land Cover Change and Climate Change Effects on Streamflow in Puget Sound Basin, Washington Lan Cuo 1, Dennis Lettenmaier 1, Marina Alberti 2, Jeffrey.
RIVER DISCHARGE *
Agenda Project overview (brief) Modeling update (preliminary results) Next steps… Integration pathways.
CE 424 HYDROLOGY 1 Instructor: Dr. Saleh A. AlHassoun.
Snow Properties Relation to Runoff
CBRFC March Peak Flow Forecast Webinar March 11, 2014 Greg Smith & Brenda Alcorn These slides: Presentation.
HYDROELECTRIC POWER AND FERC. HYDRO 101A ”Water Runs Down Hill”
INNOVATIVE SOLUTIONS for a safer, better world Capability of passive microwave and SNODAS SWE estimates for hydrologic predictions in selected U.S. watersheds.
1 Water Resources Management - DEQ’s Role in Water Supply - State Water Commission October 1, 2002.
David Watson River Forecast Section Alberta Environment and Sustainable Resource Development.
7.2 Describing Climates Copyright © 2010 McGraw-Hill Ryerson Ltd. Distance from the equator affects both average temperature and average precipitation,
Chatfield Reservoir Phosphorus Budget Jim Saunders and Jamie Anthony WQCD, Standards Unit 13 Dec 2007.
U.S. Department of the Interior U.S. Geological Survey Montana StreamStats An overview of Montana StreamStats and methods for obtaining streamflow characteristics.
Surface Water Surface runoff - Precipitation or snowmelt which moves across the land surface ultimately channelizing into streams or rivers or discharging.
Alan F. Hamlet Andy Wood Dennis P. Lettenmaier JISAO Center for Science in the Earth System Climate Impacts Group and the Department.
L Modeling the impact of land cover change and water withdrawals on runoff and N retention in the Ipswich River, MA Hydrological Modeling Nitrogen Loading.
RHESSys and SWAT simulations for modeling of long term water yield GEOG711 December 6, 2007 Yuri Kim.
DOWNSCALING GLOBAL MEDIUM RANGE METEOROLOGICAL PREDICTIONS FOR FLOOD PREDICTION Nathalie Voisin, Andy W. Wood, Dennis P. Lettenmaier University of Washington,
EVALUATION OF A GLOBAL PREDICTION SYSTEM: THE MISSISSIPPI RIVER BASIN AS A TEST CASE Nathalie Voisin, Andy W. Wood and Dennis P. Lettenmaier Civil and.
Using Groundwater and Surface Water Models for the Marcus Hook Refinery CE 394K.2 Surface Water Hydrology Presented by Julie Kim April 29, 1999.
Colorado Basin River Forecast Center Greg Smith Senior Hydrologist National Weather Service Colorado Basin River Forecast Center January 25, 2011 Navajo.
Uncertainty or Sensitivity Analysis in Climate Change Impact Assessment? Jae-Kyoung LEE Weather Radar Center in KMA.
Sanitary Engineering Lecture 4
Trends in floods in small catchments – instantaneous vs. daily peaks
Upper Rio Grande R Basin
Estimating Changes in Flood Risk due to 20th Century Warming and Climate Variability in the Western U.S. Alan F. Hamlet Dennis P. Lettenmaier.
Precipitation-Runoff Modeling System (PRMS)
Quantitative vs. qualitative analysis of snowpack, snowmelt & runoff
CPCRW Snowmelt 2000 Image Courtesy Bob Huebert / ARSC.
Water supply Flood prediction and forecasting. Water quality
Kiran Chinnayakanahalli
Snowfall Runoff Forecasting in San Juan County, UT
Change in Flood Risk across Canada under Changing Climate
Hydrologic implications of 20th century warming in the western U.S.
GEOSTATISTICAL REGIONALIZATION OF LOW-FLOWS: TOP-KRIGING VS. PSBI
Flood Monitoring Tools 2011 OFMA Annual Conference
Modeling of land surface processes in La Plata Basin
150 years of land cover and climate change impacts on streamflow in the Puget Sound Basin, Washington Dennis P. Lettenmaier Lan Cuo Nathalie Voisin University.
DROUGHT MONITORING SYSTEM IN DHMZ
Long-Lead Streamflow Forecast for the Columbia River Basin for
Using isotopes to identify source waters: mixing models
Preciptation.
Presentation transcript:

Towards a Stream Classification System for the Canadian Prairie Provinces CWRA-CGU National Conference, Banff, Alberta June 5-8, 2012 Greg MacCulloch and Paul Whitfield

Page 2 – Introduction 1. A step toward the goal of establishing a classification system for streams that is based on observed variability in flowrates. 2. To gain insight into anticipated stream response that will aid in: –Improved design and operation of hydrometric networks –The prediction of streamflow response at ungauged or poorly gauged locations.

Page 3 – Data Set Sites on the Canadian Prairies south of 54 o N Reference Hydrometric Basin Network (RHBN) (Brimley et al., 1999). The sites that populate this network where chosen to be: – characterized by pristine or stable hydrological conditions, –unaffected by developments within the basin, –and having good quality data for at least 20 years. –continuous record –“having less than 10% of the surface area of the basin modified in some fashion” – “basins with structures controlling less than 5% of the area of a basin” –27 sites met the criteria

Page 4 – Parameters Reviewed Average Annual Yield (mm) Range in Annual Yield (mm) Ratio Range to Average Duration of Peak Yield Proportion daily Q to Annual Total Q: Q>= 0.05% Q> 1% Annual Q > 2% Annual Proportion of record with completely dry years Average March to October zero flow days Last Quartile Ratios (monthly) –Avg May to October –Range May to October –Non Zero Minimum –Maximum monthly

Page 5 –

Page 6 –

Page 7 –

Page 8 –

Page 9 – A basic classification for streams on the Canadian Prairies should be separated into two broad categories: 1.Native Prairie Streams: streams that respond to localized water sources i.e., precipitation and snowmelt, proportionally throughout the basin and can be dry from time to time. 2.Exotic Prairie Streams: Streamflow is predominately conveyed from the headwaters and these streams do not experience dry conditions. They respond to localized water sources disproportionally throughout the basin.

Page 10 –

Page 11 –

Page 12 –

Page 13 –

Page 14 –

Page 15 –

Page 16 –

Page 17 –

Page 18 – Conclusions It is likely that there are distinct classes of streams. Stream Characteristics can be distinguished from HYDAT data set –Average Annual Yield (mm) 6 vs. 800 –Ratio of Range in Yield to Average 6 vs. 1 –Average number of days per year with flow >2% 6 vs. 1 –Maximum Monthly LQR 500 vs. 2 A reference network is a very important asset and needs to be maintained. A review of operation of the existing Prairie RHBN is warranted.