TO GO WITH THE FLOW. The importance of streamflow data for watershed management. Scott Morlock Deputy Director USGS Indiana Water Science Center

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1 TO GO WITH THE FLOW The importance of streamflow data for watershed management Scott Morlock Deputy Director USGS Indiana Water Science Center U.S. Department of the Interior U.S. Geological Survey

2 Streamflow Volume of water that passes a point on a stream per unit of time

3 Streamflow Precipitation (inches) Peak streamflow Surface runoff Lag Receding limb Rising limb Stormflow - surface runoff Base flow Time (days, hours, weeks) 1 Bigelow Laboratory for Ocean Sciences, How Our Rivers Run

4 Measuring Streamflow Q = VA A = w x d

5

6 Stage Streamgaging measurement rating curve 6 ft measurement Streamflow 700 cfs *Stage = water level referenced to a datum

7 GOES DOMSAT LRGS Field Station with Data Collection Platform (DCP) Data Access and Processing System (DAPS), Wallops Island, VA National Water Information System (NWIS) Real-time telemetry: 24/7/365

8 Wabash River at Lafayette, 1930

9 Real-time Streamflow Reservoir operations NPDES compliance Spill tracking Recreational boating Flood response Drought detection

10

11

12 WaterWatch

13

14 QUESTIONS? USGS IN real-time streamgage data - Drought monitor WaterWatch - WaterAlert -

15 Historic Streamflow Records Daily mean Q Annual runoff Peak of record 7Q 10 Q 100 Harmonic mean Flow durations Trend analyses

16 Streamflow and Watersheds Physiography Land-use Stressors Development Contaminants Water use Climate change Outflow point

17 Physiography White River Central Kankakee River North Equivalent basin size Base flow of Kankakee = 3X BF of White Peak flows of White >> Kankakee

18 Land Use Losing forests and farmland at 3 acres per minute Estimated million acres of forest land will be developed by 2050

19 Forested Watersheds Provide drinking water for 180 million Replenish ground water Decrease severity of floods

20 Wetland Reserve Program Restore and enhance wetlands/wildlife habitat Lessen stream flows due to flooding Improve water quality Specific Criteria: vegetation, soils and hydrology

21

22 Questions? Links: USGS IN real-time streamgage data - Drought monitor - USGS WaterWatch -

23 Low-flow Statistics Water Use Discharge permitting Drought determination Total Maximum Daily Loads Aquatic Ecosystems Ecological Flows

24 Ecological Flow long-term hydro-ecological research set within an adaptive management framework is needed to improve predictions of the ecological consequences of flow regulation and to inform the intensifying debates about ecosystem responses to flow modification and climate change. -Angela Arthington et al Arthington, A.H., Bunn, S.E., Poff, N.L., Naiman, R.J., 2006, The challenge of providing environmental flow rules to sustain river ecosystems, in Ecological Applications 16 (4), Ecological Society of America, pp , _EFlows.pdf

25 Climate Change - Streamflow Flow timing shifts in areas where snow has been significant Predominantly increasing low & average flows Changes in flooding, very unclear Changes in ground-water, very unclear

26

27 Streamflow and Water Quality Streamflow is one of most important ancillary variables that can be collected in stream or river quality studies. Having it allows us to remove the fluctuations in concentration data attributable only to variation in flow and helps us ascertain other effects (e.g. changes to landscape). Charles Crawford, USGS

28 Streamflow and Water Quality Load computation Concentration x Streamflow Watershed diagnostics Trend assessments BMP evaluation

29 Why is streamflow important and Flow Delivered to the Gulf of Mexico 1000 TONS TN LOAD, IN Gulf hypoxia IN 1000 CFS AVERAGE FLOW, CONC., IN mg/l FLOW-WEIGHTED TN average Lowess smooth May Mississippi River Basin Total Nitrogen Load WATER YEAR

30 Watershed Diagnostics

31 Suspended Sediment

32 BMPs?

33 Urbanization =more bankfull events = increased bank erosion =>sediment loads = changed BMP focus flow driven, in-stream process KAREN L. PRESTEGAARD Sediment Budgets (Proceedings of the Porto Alegre Symposium, December 1988). IAHS Publ. no. 174, 1988.

34 Streamflow is a driver of important hydrologic processes in a watershed Streamflow should be key in watershed monitoring plans Continuous records of streamflow are superior to discreet measurements Pairing continuous streamflow and waterquality data is powerful

35 Scott Morlock x153

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