FETWATER Pilot Training 20 24 August 2018 Water
- Slides: 67
FETWATER Pilot Training 20 - 24 August 2018 Water Resources Management From Hydrology to Yield
Contents 1. 2. 3. 4. 5. 6. 7. Hydrological Cycle Rainfall Streamflow Catchment Developments Evaporation Stochastic hydrology Yield
1. The Hydrological Cycle
Understanding catchments
Understanding catchments
Understanding catchments
Understanding catchments
2. Rainfall
One can not do water resources Management without Rainfall data Number of useable rainfall stations open over time
Why do we need rainfall data? Water resource, source of streamflow / groundwater l Can affect requirements eg. Irrigation l Intensity eg. flood management l Early warning eg. Drought cycles l Long term cyclic trends, climate change l
Where to obtain rainfall data from? DWS Management Framework Rainfall l SAWS: costs l Other l Satellite l Varying time frames: monthly, daily, hourly l
Collating Rainfall Data Raw data should be checked l Patched with surrounding rainfall gauges with available data l Individual gauges usually lumped together to obtain representative catchment rainfall l
3. Streamflow
Number of useable stramflow stations open over time
Why do we need streamflow data? To understand the volume of rainfall that produces surface flows l Natural streamflow data is known as “hydrology” l Yield analyses of water resources requires hydrology l Flow measurements important for operating systems eg. EWR & users’ requirements l
Where to obtain streamfow data from? Google Earth KMZ file
Rainfall-Runoff Relationships More rainfall = more runoff l Lag can occur l Further material under Pitman Modelling Module l
Quick Practical l What was the monthly flow out of Jericho Dam in March 1991? l What was the rainfall measured at gauge 0297159 W in January 1984?
4. Catchment developments
Afforestation Irrigation
Urbanisation Alien vegetation Dryland crops Transfers
Dams / Reservoirs
Why should they be considered? Often negative impact on streamflow l Quantifying difficult l Changes in flow over time l “Natural Streamflow” required for water resources management assessments l
Recorded vs natural vs current development level
5. Evaporation
Vaal dam surface area when full: 322. 75 km 2 = 322 750 000 m 2 2000 mm = 2 m 2 m x 322 750 000 m 2 = 645. 5 million m 3/a Storage of Vaal Dam = 2610 million m 3 therefore 25%
Required for Surface water evaporation losses from Dams, rivers l Crop evapotranspiration in determining crop water requirements l Types Lake l S-Pan l A-Pan l Crop l
Obtained from Water Resources studies l Usually constant per year, monthly distribution l
6. Stochastic Hydrology
What are stochastics? Alternative to Natural hydrology sequence l Only 1 change: rainfall, not dependant on landuse/catchment development changes l Eg. of Vaal Rainfall l Cumulative Avg: 648 mm
Sequence 1 ? Avg: 648 mm Sequence 2 Sequence 3
Sequence 1 ? Avg: 648 mm Avg: 645 mm Sequence 2 Sequence 3 Avg: 637 mm Avg: 665 mm
Why use stochastics? Eliminates the need to plan according to historic events only l Can provide results in terms of assurance of supply, probability of failure (more later) l Use STOMSA to produce stochastic flow sequences from natural historic sequence l
7. Yield and Modelling
What is yield? Available water from a water resource system l Volume of water that can be abstracted over a specific time period l Varying types: l – Historic firm – Long term at various assurance levels – Short term
Critical period Spill Recovery Full Supply Volume (FSV) Storage volume t. C Dead Storage Volume (DSV) Time Failure
Definition of Modelling “… a simplified mathematical description of a system or process, used to assist calculations and predictions…” – Oxford English Dictionary
Benefits of modelling l Allows representation of real world, subject to various human activities / interventions l Can predict behaviour prior to actual experience l Provides testing environment to assess best options for application in real world l Allows “mistakes” without applying incorrect or inappropriate options l Guides design of corrective measures
Limitations of modelling l Cannot capture full complexities of real world l Dependent on assumptions l Data availability l Selection of appropriate model l Difficult to standardise modelling approach l Specialist configuration and interpretation l Small user group l Extensive configuration checking
l l Assessment Purpose – Resource capability – Resource assurance – Water quality Impact of interventions – Conservation – Resource development Impact of management options – Resource operation – System maintenance Monitoring of observed behaviour
The modelling process l Define objectives l Identify main physical features l Define system network l Select system operating rules l Undertake scenario analysis l Evaluate results l Implement decision
Models and utilities l Hydrological and water quality data preprocessors (various) l Data patching utilities (CLASSR, PATCHR) l Rainfall-runoff models (Pitman) l Stochastic streamflow models (STOMSA) l Water quality models (WQT) l Yield analysis models (WRYM) l Planning analysis models (WRPM) l Information management systems (WR-IMS)
Undeveloped catchment Runoff Available flow
Available flow Monthly flow volume (million m 3) 40 35 Average flow 30 25 20 15 10 5 0 0 1 2 3 4 5 Year 6 7 8 9 10
Abstraction from river Water user Abstraction Runoff Available flow
Actual supply Available flow Monthly flow volume (million m 3) 40 35 Average flow 30 Abstraction capacity 25 20 Actual supply 15 10 5 0 0 1 2 3 4 5 Year 6 7 8 9 10
Abstraction from reservoir Water user Reservoir Abstraction Runoff
Reservoir model Inflows < Outflows S ∆ S = Inflows – Outflows
Reservoir model Inflows > Outflows S ∆ S = Inflows – Outflows
Relationship between time-steps Time-step 1 Start S 1 Time-step 2 End S 1 Start S 2
Flow rate Simulation Cap Abstraction Abs Cap Abs Time Storage level FSL Start S D R S Adapted from: Basson Et. Al. 1994 D R S D R D R S D DSL
8. Stochastic yield analysis
Why bother? Historical yield analysis at Midmar Dam Period of analysis (hydrological years) Number of years Firm yield (million m 3/a) 1930 – 1934 5 81 1930 – 1939 10 69 1930 – 1949 20 69 1930 – 1969 40 69 1930 – 1989 60 36
Water resource system Assumptions: 1. Fixed reservoir capacity 2. Fixed annual abstraction volume 3. Particular inflow sequence Reservoir Runoff Abstraction
Abstraction rate and of failure risk Full Supply Volume (FSV) Storage level Failure A B Dead Storage Volume (DSV) Time A = Higher abstraction rate: higher risk of failure B = Lower abstraction rate: lower risk of failure
Abstraction rate and reliability of supply A B Reliability of supply A = Higher abstraction rate: lower reliability B = Lower abstraction rate: higher reliability
Yield results for 41 sequences Yield / target draft (million m 3/a) Target draft = 45 million m 3/a 50 40 30 20 10 0 5 10 15 20 25 Sequence number 30 35 40
Yield results sorted Yield / target draft (million m 3/a) Break point 50 Base yield line 40 30 20 19 10 0 5 10 15 20 25 Sequence number 30 35 40
Definitions l Rn = Long-term risk of failure = [Failure sequences + 1] / [Total sequences] = (19 + 1) / 41 = 0. 488 = 48. 8 % l Ep = Long-term reliability of supply = 1 – Rn = 51. 2 % l RI = Recurrence interval of failures = 1 / (1 – Ep 1/n) = 90. 18 years
Yield-reliability curve 50 40 Ep = 51. 2 % 30 RI = 1: 50 year 10 RI = 1: 100 year 20 RI = 1: 200 year Rn = 48. 8 % RI = 1: 20 year Yield / target draft (million m 3/a) n = 60 years 0 0 10 20 30 40 50 60 70 80 90 100 Reliability of supply (as % of sequences observed)
Family of yield-reliability curves 50 40 RI = 1: 50 year 10 RI = 1: 100 year 20 RI = 1: 200 year 30 RI = 1: 20 year Yield / target draft (million m 3/a) Firm yield line 0 0 10 20 30 40 50 60 70 80 90 100 Reliability of supply (as % of sequences observed)
50 47. 5 10 40 5. 5 RI = 1: 50 year 10 RI = 1: 100 year 20 RI = 1: 200 year 30 RI = 1: 20 year Yield / target draft (million m 3/a) Available resource 32 0 0 10 20 30 40 50 60 70 80 90 100 Reliability of supply (as % of sequences observed)
9. Boxplot practical
FETWATER Pilot Training 20 - 24 August 2018 Water Resources Management From Hydrology to Yield End of Module
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