Jasna Plavsic. WATER-FOOD-ENERGY-ECOSYSTEMS NEXUS ASSESSMENT IN THE SAVA RIVER BASIN Zagreb, 6 March 2014

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WATER-FOOD-ENERGY-ECOSYSTEMS NEXUS ASSESSMENT IN Zagreb, 6 March 214 Water and Climate Adaptation Plan (WATCAP) for the Sava River Basin: Climate Change Predictions for the Sava River Basin Jasna Plavsic 1

Water and Climate Adaptation Plan (WATCAP) for the Sava River Basin Task 3: Development of the hydrologic model and simulations with future climate scenarios Scope of work: Model development define an appropriate model structure collect necessary data perform model calibration and verification Characterisation of future hydrologic regime perform hydrologic simulations with climate scenarios for 211-24 and 241-27 2

Hydrologic Model Development Sava River Basin: ~ 95, km 2 No previous models of the whole basin 3

Hydrologic Model Development Choice of the model: HEC-HMS used initially by USACE as a link to the hydraulic model developed for ISRBC easily obtainable by future users on the SRB (free of charge) Main pros and cons moderate data requirements (depending on calculation methods) not completely suitable for continuous simulation 4

Data Requirements Input data daily precipitation time series daily temperature time series monthly potential evapotranspiration (seasonal distribution) Hydrologic data for calibration and verification daily flows time series Geographic data sub-basin areas met station elevations elevation distribution within the basin (elevation bands) 5

Data Collection Data collection by riparian experts lasted for 5 months (from 5 June to 24 October 212) delivered: hydrologic data at selected stations and in selected periods daily flow rates precipitation and air temperature data at selected meteo station daily data potential evapotranspiration data at selected stations monthly data basic information on water control facilities Precipitation and temperature data from Montenegro additional data needed for the Drina Basin model obtained via ISRBC made available in February 213 6

Model setup and data availability Choice of sub-basins, calibration and verification periods, modelling methods and data collection is an iterative process not all relevant data is readily available short calibration and verification periods due to poor data availability select subbasins select time period Calibration 1979-1984 Verification 1969-1974 ask for data select modelling method 7

Hydro and meteo stations Input Data Precipitation stations (5) Temperature stations (27) Hydrologic stations (35) 8

Record extension Filling gaps and extending P and T records Records reconstructed using a regional climate model with 1 km horizontal resolution Poorer results for precipitation in Montenegro (improper boundary conditions) of stations Number 7 6 5 4 3 2 1 16 19 1961-199 29 13 3 23 Incomplete record Complete record 9

Sub-basin division Basin subdivision with respect to daily time step and to data availability and quality sub-basin sizes 2-5 km 2 14 major sub-basins modelled separately 44 sub-basins in total 35 sub-basins controlled by hydrologic stations 1

Calibration and validation Mean monthly flows 1 Sava @ Zagreb simulation observed 1 Sava @ Zagreb simulation observed Flow (m3/s) 5 5 4 Sava @ Slavonski Brod 4 Sava @ Slavonski Brod Flow (m3/s) 2 2 5 Sava @ Sremska Mitrovica 5 Sava @ Sremska Mitrovica Flow (m3/s) 25 25 lis 1979 lis 198 lis 1981 lis 1982 lis 1983 lis 1984 lis 1969 lis 197 lis 1971 lis 1972 lis 1973 lis 1974

Model performance: bias (error in mean annual flow) 25% 2 15% 1 PBIAS 5% -5% -1-15% -2-25% calibration verification ext. record 12

Model performance: Nash-Sutcliffe Efficiency NSE for mon nthly data 1,9,8,7,6,5,4,3,2,1 calibration verification ext. record 13

Model application with future climate: Methodology Hydrologic simulations of future regime using future climate scenarios as input GCM/RCMs Baseline: 1961-199 Near future: 211-24 Distant future: 241-27 Climate scenarios (future P, T, PET) Hydrologic model 14 Hydrologic projections

Model application with future climate: Methodology Change in hydrologic regime is evaluated by comparing simulated future regime against simulations with baseline climate Relative change evaluated rather than the absolute values Q FUT Q Q BASE BASE 1 annual change () winter: December, January and February () spring: March, April and May () summer: June, July and August () autumn: September, October and November () 15

Climate scenarios Ensemble of 5 GCM/RCM outputs for A1B IPCC/SRES scenario Climate model GCM RCM CM1 ECHAM5r3 RACMO CM2 ECHAM5r3 REMO CM3 HadCM3Q CLM CM4 HadCM3Q HadRM3Q CM5 ECHAM5r3 RegCM3 16

5 4,5 4 3,5 3 2,5 2 1,5 1,5 Temperature scenarios CM1 5 4,5 4 3,5 3 2,5 2 1,5 1,5 CM2 5 4,5 4 3,5 3 2,5 2 1,5 1,5 CM3 temperature change (deg C) temperature change (deg C) temperature change (deg C) 5 4,5 4 3,5 3 2,5 2 1,5 1,5 Ensemble median temperature change (deg C) 5 4,5 4 3,5 3 2,5 2 1,5 1,5 CM4 5 4,5 4 3,5 3 2,5 2 1,5 1,5 temperature change (deg C) temperature change (deg C) CM5

Precipitation scenarios -5-4 -3-2 -1 1 2 3 4 5 precipitation change CM1-5 -4-3 -2-1 1 2 3 4 5 precipitation change CM2-5 -4-3 -2-1 1 2 3 4 5 precipitation change CM3-5 211-24 241-27 -5 211-24 241-27 211-24 241-27 -5-4 -3-2 -1 1 2 3 4 5 211-24 241-27 precipitation change CM4-5 -4-3 -2-1 1 2 3 4 5 211-24 241-27 precipitation change CM5-5 -4-3 -2-1 1 2 3 4 5 211-24 241-27 precipitation change Ensemble median

Scenarios for potential evapotranspiration Based on temperature scenarios and the Hargreaves equation for PET PET.5 =.23 R TD ( TC + 17.8) a PET_1 with baseline CM temperatures PET_2 with future CM temperatures Relative change c = PET_2/PET_1 19 PET_ used in model calibration Future PET = c * PET_

Simulations with future climate scenarios Change in ensemble median values of mean seasonal and annual runoff, averaged over 5 locations in the basin change in mean flo ow (%) 5 4 3 2 1-1 -2-3 -4 11, 13, -9, -5,1%,4% -1,4% -3,3%-4,7% -11,4% -15,1% 2 211-24 241-27 error bars indicate range of changes across the locations

Simulations with future climate scenarios Change in mean seasonal runoff at selected locations for five climate scenarios 5 4 3 2 1-1 211-24 5 4 3 2 1-1 Sava @ Čatež Sava @ Zagreb Kupa mouth Sava @ Crnac Una mouth Sava @ Čatež Sava @ Zagreb Kupa mouth Sava @ Crnac Una mouth Sava @ Mačkovac Vrbas mouth Savaa @ Slav. Brod Bosna mouth Sava @ Županja Drina mouth @ S. Mitrovica Sava @ Beograd change in mean flow (%) Sava @ Mačkovac Vrbas mouth Savaa @ Slav. Brod Bosna mouth Sava @ Županja Drina mouth change in mean flow (%) @ S. Mitrovica Sava @ Beograd 241-27 Sava CM1 CM2 CM3 CM4 CM5 21 1-1 -2-3 -4 211-24 Sava @ Čatež Sava @ Zagreb Kupa mouth Sava @ Crnac Una mouth Sava @ Mačkovac Vrbas mouth Sava @ Slav. Brod Bosna mouth Sava @ Županja Drina mouth Sava @ S. Mitrovica Sava @ Beograd change in mean flow (%) Sava CM1 CM2 CM3 CM4 CM5 1-1 -2-3 -4 Sava @ Čatež Sava @ Zagreb Kupa mouth Sava @ Crnac Una mouth Sava @ Mačkovac Vrbas mouth Sava @ Slav. Brod Bosna mouth Sava @ Županja Drina mouth Sava @ S. Mitrovica Sava @ Beograd 241-27 change in mean flow (%) CM1 CM2 CM3 CM4 CM5 CM1 CM2 CM3 CM4 CM5

Simulations with future climate scenarios Change in mean seasonal runoff at selected locations for five climate scenarios 3 2 1-1 -2-3 -4-5 211-24 3 2 1-1 -2-3 -4-5 Sava @ Čatež Sava @ Zagreb Kupa mouth Sava @ Crnac Una mouth Sava @ Čatež Sava @ Zagreb Kupa mouth Sava @ Crnac Una mouth Sava @ Mačkovac Vrbas mouth Sava @ Slav. Brod Bosna mouth Sava @ Županja Drina mouth Savaa @ S. Mitrovica Sava @ Beograd change in mean flow (%) Sava @ Mačkovac Vrbas mouth Sava @ Slav. Brod Bosna mouth Sava @ Županja Drina mouth change in mean flow (%) Savaa @ S. Mitrovica Sava @ Beograd 241-27 CM1 CM2 CM3 CM4 CM5 CM1 CM2 CM3 CM4 CM5 22 3 2 1-1 -2-3 211-24 3 2 1-1 -2-3 Sava @ Čatež Sava @ Zagreb Kupa mouth Sava @ Crnac Una mouth Sava @ Čatež Sava @ Zagreb Kupa mouth Sava @ Crnac Una mouth Sava @ Mačkovac Vrbas mouth Sava @ Slav. Brod Bosna mouth Sava @ Županja Drina mouth Sava @ S. Mitrovica Sava @ Beograd change in mean flow (%) Sava @ Mačkovac Vrbas mouth Sava @ Slav. Brod Bosna mouth Sava @ Županja Drina mouth Sava @ S. Mitrovica Sava @ Beograd 241-27 change in mean flow (%) CM1 CM2 CM3 CM4 CM5 CM1 CM2 CM3 CM4 CM5

Simulations with future climate scenarios Change in mean annual runoff at selected locations for five climate scenarios 2 1-1 -2 Sava @ Čatež Sava @ Zagreb Kupa mouth Sava @ Crnac Una mouth Sava @ Mačkovac Vrbas mouth Sava @ Slav. Brod Bosna mouth Sava @ Županja Drina mouth change in mean flow (%) Sava @ S. Mitrovica Sava @ Beograd 241-27 2 1-1 -2 211-24 Sava @ Čatež Sava @ Zagreb Kupa mouth Sava @ Crnac Una mouth Sava @ Mačkovac Vrbas mouth Sava @ Slav. Brod Bosna mouth Sava @ Županja Drina mouth Sava @ S. Mitrovica Sava @ Beograd change in mean flow (%) CM1 CM2 CM3 CM4 CM5 CM1 CM2 CM3 CM4 CM5 23

Sources of uncertainty Definition of greenhouse gas emission scenarios (unpredictability of future economic and societal development) Climate model structural uncertainty (different GCMs produce different projections for the same emission scenario) Downscaling and bias correction of GCM outputs Hydrological model structure and parameters uncertainty Record extension 24

Essentially, all models are wrong, but some are useful. Box, G. E. P., and Draper, N. R. (1987) Empirical Model Building and Response Surfaces, Wiley, New York, p. 424. 6 Sava @ Sremska Mitrovica Flow (m3/s) 5 4 3 2 simulation observed 25 1 lis 1961 lis 1966 lis 1971 lis 1976 lis 1981 lis 1986 lis 1991