usgs watershed model evolution – rrm(1972) to gsflow(2012) usgs watershed model evolution –...

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USGS Watershed Model USGS Watershed Model Evolution – RRM(1972) Evolution – RRM(1972) to GSFLOW(2012) to GSFLOW(2012) George Leavesley, USGS George Leavesley, USGS Retired and Steve Markstrom, Retired and Steve Markstrom, USGS, Denver USGS, Denver

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Page 1: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

USGS Watershed USGS Watershed Model Evolution – Model Evolution –

RRM(1972) to RRM(1972) to GSFLOW(2012)GSFLOW(2012)

George Leavesley, USGS George Leavesley, USGS Retired and Steve Markstrom, Retired and Steve Markstrom,

USGS, DenverUSGS, Denver

Page 2: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

RRM

DR3M Mountain

Watershed Model

GSFLOW

MODFLOW

PRMS

MMS

Developers

Model Evolution

Page 3: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Guiding Principles – Integrated Model

and System Development• Multi-disciplinary integration of models and tools

• Incorporation of new science advances

• Open source• Modular approach to model

development• Model composition is function of

problem objectives, data constrains, time-space of application

• Credit Dave Dawdy for planting the seeds of modular design during a grad level class at CSU in early 1970’s

Page 4: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Rainfall Runoff Model Rainfall Runoff Model (RRM)(RRM)

Dawdy, D.R., Lichty, R.W., and Bergmann, J.M., 1972, A rainfall- runoff simulation model for estimation of

flood peaks for small drainage basins: U.S. Geological Survey Professional Paper 506-B, 28 p.

Philip infiltration equation

Saturated-unsaturated soil moisture regimes

Clark instantaneous unit hydrograph

ANTECEDENT-MOISTURE ACCOUNTING COMPONENT

ROUTING COMPONENT

INFILTRATION COMPONENT

di/dt = K (1. + (P(m-m0) / i))

Model Components

Vars & Params Daily rainfallDaily pan evaporationInitial conditions

Vars & Params Storm rainfallInitial conditionsKsat and P

Vars & ParamsRainfall excessTime-area curveLinear reservoir coeff

Page 5: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

RRM

DR3M

Developers

Model Evolution

(Lumped)

(Distributed)

ENHANCEMENTS•Green-Ampt infiltration•Flow planes and channels•Kinematic routing

• Leclerc, Guy, and Schaake, J.C., Jr., 1973, Methodology for assessing the potential impact of urban development on urban runoff and the relative efficiency of runoff control alternatives: Ralph M. Parsons Laboratory Report no. 167, Massachusetts Institute of Technology, 257 p.

Page 6: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Distributed Routing Distributed Routing Rainfall Runoff Model Rainfall Runoff Model

(DR3M)(DR3M)

Dawdy, D.R., Schaake, J.C., Jr., and Alley, W.M., 1978, User's guide for distributed routing rainfall-runoff model: U.S. Geological Survey Water-Resources Investigations Report 78-90, 146 p.

Model Features•Pervious and impervious area rainfall excess•Green-Ampt infiltration equation for rainfall excess•Kinematic routing for flow planes and channels•Multiple solution techniques for kinematic routing•Soil moisture accounting between storms•Interflow and baseflow not simulated•Snow accumulation and melt are not simulated

Alley, W.M., and Smith, P.E., 1982, Distributed routing rainfall- runoff model--version II: U.S. Geological Survey Open-File Report 82-344, 201 p.

Page 7: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Distributed Routing Distributed Routing Rainfall Runoff Model Rainfall Runoff Model

(DR3M)(DR3M)

1

2

3 4

5

6

Watershed boundary

EXPLANATION

Stream

1 65432Hydrologic response unit

Streamflow gage at basin outlet

Direction of streamflow

1

2

3 4

5

6

Watershed boundary

EXPLANATION

Stream

1 65432Hydrologic response unit

Streamflow gage at basin outlet

Direction of streamflow

Flow Planes and Channels

Page 8: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Mountain Watershed Mountain Watershed ModelModel

Leavesley, G.H., 1973, A mountain watershed simulation model: Fort Collins, Colorado, Colorado State University, Ph. D.

dissertation, 174 p.

Model Features•Daily time step•Distributed hydrologic response unit (HRU) based•Surface runoff computed using contributing area concept•Subsurface and groundwater flows computed as nonlinear and linear reservoirs•Snow accumulation and melt computed using an energy budget approach

Page 9: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Mountain Watershed Model

Page 10: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

DR3M Mountain

Watershed Model

PRMS

Developers

Model Evolution

Page 11: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Precipitation-Runoff Precipitation-Runoff Modeling System (PRMS)Modeling System (PRMS)

Leavesley, G.H., Lichty, R.W., Troutman, B.M., and Saindon, L.G., 1983, Precipitation-runoff modeling system—User’s manual: U.S. Geological Survey Water-Resources Investigations Report 83-4238, 207 p.

Model Features•Modular design•Integrates daily and storm mode time steps•Computes surface, subsurface, and groundwater flow at all time steps•User selectable components for ET, precip and temp distribution, surface runoff, and solar radiation computations•Includes optimization and sensitivity analysis tools

Page 12: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

PRMS

Page 13: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

PRMS Modular Design•Conceptually a great idea•Implementation in PRMS, less than desirable

• Few support tools• Coding complexity• Spaghetti codingEnter the Modular Modeling

System (MMS)•Developed in collaboration with the Center for Advanced Decision Support in Water and Environemental Systems (CADSWES), Univ of Colorado, Boulder, CO

Leavesley, G.H., Restrepo, P.J., Markstrom, S.L., Dixon, M., and Stannard, L.G., 1996b, The Modular Modeling System (MMS): User’s manual: U.S. Geological Survey Open-File Report 96-151, 142 p.

Page 14: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

MMS Developed to Address s a Range of a Range of Modular Design

Levels PROCESSPROCESS MODELMODEL FULLY COUPLED MODELSFULLY COUPLED MODELS LOOSELY COUPLED MODELSLOOSELY COUPLED MODELS RESOURCE MANAGEMENT RESOURCE MANAGEMENT

DECISION SUPPORT SYSTEMSDECISION SUPPORT SYSTEMS ANALYSIS AND SUPPORT TOOLSANALYSIS AND SUPPORT TOOLS

Page 15: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Model Builder

MMS Interface

MODULAR MODELING

SYSTEM (MMS)

Object User Interface

Page 16: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Analysis and Support Analysis and Support Tools Integrated with Tools Integrated with

MMS and PRMSMMS and PRMS

• The GIS Weasel• LUCA – A Multi-step

multi-objective calibration tool

• Esemble Streamflow Prediction

• Data retrieval Downsizer

Page 17: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

GSFLOW

MODFLOW

PRMSRevise

d

Developers

Model Evolution

PRMS

Page 18: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

PRMS SOIL ZONEPRMS SOIL ZONE((Original Version)Original Version)

Recharge Zone (soil_rechr_max)

Lower Zone

excs (soil_moist > soil zone field capacity)

sroff

soil_moist_max (rooting depth)

soil2gw_maxexcs - soil_to_gw

to subsurface reservoir

to ground-water reservoir

Page 19: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

ConceptuaConceptual Revised l Revised Soil Zone Soil Zone Structure Structure and Flow and Flow

ComputatiComputation on

SequenceSequence

Page 20: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Original and Revised Soil Original and Revised Soil ZoneZone

Page 21: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Revision Revision Adds Adds

Cascading Cascading HRU Flow HRU Flow

PathsPaths1

234

5

Watershed boundary

EXPLANATION

Stream

1 21Hydrologic response unit and numerical

identification

Streamflow gage at basin outlet

Direction of streamflow

678

9

10

11

12

13

14

15

1617

18

1920

21

Direction of runoff and interflow among hydrologic response units

A

1

234

5

Watershed boundary

EXPLANATION

Stream

1 21Hydrologic response unit and numerical

identification

Streamflow gage at basin outlet

Direction of streamflow

678

9

10

11

12

13

14

15

1617

18

1920

21

Direction of runoff and interflow among hydrologic response units

1

234

5

Watershed boundary

EXPLANATION

Stream

1 21Hydrologic response unit and numerical

identification

Streamflow gage at basin outlet

Direction of streamflow

678

9

10

11

12

13

14

15

1617

18

1920

21

Direction of runoff and interflow among hydrologic response units

A

Page 22: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Original PRMS Original PRMS ConceptualizationConceptualization

SRO

Page 23: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Revised PRMS Revised PRMS ConceptualizationConceptualization

Page 24: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

GSFLOW -- Coupled GSFLOW -- Coupled PRMS, MODFLOW, SFR, PRMS, MODFLOW, SFR, and Unsaturated Zone and Unsaturated Zone

ModelsModels

Streamflow

Unsaturated Zone Model:

PRMS to UZF UZF to MODFLOW

PRMS to SFR2

PRMS to MODFLOW

MODFLOW to SFR2

Page 25: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Coupled Groundwater Coupled Groundwater Surface-Water Flow Model Surface-Water Flow Model

(GSFLOW)(GSFLOW)

Markstrom, S.L., Niswonger, R.G., Regan, R.S., Prudic, D.E., and Barlow, P.M., 2008, GSFLOW—Coupled ground-water and surface-water flow model based on the integration of the Precipitation-Runoff Modeling System (PRMS) and the Modular Ground-Water Flow Model (MODFLOW-2005): U.S. Geological Survey Techniques and Methods 6-D1, 240 p.

Model Features•Daily time step•Simultaneously simulates flow across the land surface, within subsurface saturated and unsaturated materials, and within streams and lakes•3 simulation modes (integrated, PRMS only, MODFLOW only) allow incrimental setup and calibration

Page 26: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

SummarySummary

Page 27: USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) USGS Watershed Model Evolution – RRM(1972) to GSFLOW(2012) George Leavesley, USGS Retired and

Model Developer CreditsModel Developer Credits

Alley, W.M.Barlow, P.M.Bergman, J.M.Dawdy, D.R.Dixon, M.Hay, L.E.Harbaugh, A.W.Lichty, R.W.Markstrom, S.L.

Niswonger, R.G.Prudic, D.E.Regan, R.S.Restrepo, P.J.Schaake, J.W. JrSmith, P.E.Stannard, L.G.Troutman, B.M.