YIELD SERIES FOR HYDRO ELECTRIC PROJECTS IN RAINFALL VARIABILITY SCENARIO

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TECHNICAL SESSION : WATER AVAILABILTY AND ISSUES IN DEVELOPMENT OF HYDRO POWER/THERMAL POWER

YIELD SERIES FOR HYDRO ELECTRIC PROJECTS IN RAINFALL VARIABILITY SCENARIO

by N. N. Rai Director Central Water Commission


Introduction  Huge hydro power potential in Himalayas  Limited G&D data on main rivers only and huge

variability in rainfall  Most of the HE Projects on Tributaries  For power potential study of ROR projects at least 10

years water availability (yield) series is essential  The water availability series can not be computed by

catchment area proportioning  Yield correction factor along with catchment area

proportioning is essential


Objective  To develop yield series for HE Projects in rainfall

variability scenario by developing an yield model at a G&D site of the basin

Input data and data validation        

Catchment area map Hypsometric details of catchment Permanent snowline Transitional snow zone Upstream diversion/ other consumptive& non-consumptive use Catchment representative rainfall Observed Discharge at some locations Rainfall and discharge data Validation is must : Mass curve, double mass curve, concurrent plots, annual plots, multi station plots, yield comparison, runoff coefficient, rainfall runoff correlation, runoff-runoff correlation etc may be used


Case Study – Kameng Basin (Arunachal Pradesh) Data availabilty Discharge data  Bhalukpong G&D Site

(CA-10450 sq.km)  Bichom dam site G&D Site

(CA-2277 sq.km)

Rainfall data –Lower Kameng 

Bhalukpong, Kimi, Lumdung Sebu Lanka

Rainfall data (East Kameng) 

Seppa, Lamino

Rainfall data (West Kameng) 

Bichom, Jameri, Bomdila, Dirang, Dibbin


Hypsometric Curve of Bhalukpong G&D Site


Yield model at Bhalukpong G&D Site

Catchment

Catchment Area (sq.km)

Annual Rainfall (mm)

Snowmelt during six months @ 5 mm/day

Runoff from rainfall (MCM)

Snow melt runoff (MCM)

Permanent snowfed

136

SB1 and SB2 excluding permanent snowfed

3915.8

1440

5074.88

SB3 and SB4 excluding permanent snowfed

3679.2

2400

7947.07

SB5

2719

3914

9577.95

Area between EL 3000m-5000m

1778

1548

912.5

Total Average annual runoff from rainfall and snowmelt (MCM) Total Catchment Area (sq.km) Average annual yield (mm)=1000* [runoff (MCM)/CA (sq.km)]

Observed yield (mm) at Bhaluk-pong during (1993-2010)

124.1

2752.34 22599.90

2876.44

25476.34 10450 2437.90

2437.90


Hypsometric Curve of Bichom dam G&D Site


Testing of Yield model at Bichom G&D site Catchment

Catchment Area (sq.km)

Annual Rainfall (mm)

Permanent Snowfed

23.45

SB1 excluding permanent snowfed

2253.55

1515

Area between EL 3000m-5000m

766

1548

Snowmelt during six months @ 5 mm/day

Runoff from rainfall (MCM)

912.5

Snow melt runoff (MCM)

Observed yield (mm) at Bhaluk-pong during (1993-2010)

21.40

3072.72 1185.77

Total Average annual runoff from rainfall and snow melt (MCM)

3072.72

Total Catchment Area (sq.km)

2277.00

Average annual yield (mm)

1879.61

1207.17

4279.88

1878


Application of yield model to derive 10-daily discharge series at Pachuk-I HEP diversion Catchment CatchAnnual Snowmelt Runoff Snow melt site ment Area Rainfall during six from runoff (sq.km)

(mm)

Permanent Snow fed

42

SB3 excluding permanent snowfed catchment

974

2100

Area between EL 3000m5000m 296

1548

months @ 5 mm/day

rainfall (MCM)

912.5

(MCM)

38.33

1840.86 458.208

Total

1840.86

Average annual runoff (MCM)

2337.39

Total Catchment Area (sq.km)

1016.00

Average annual yield (mm)

2300.58

496.53


Yield Series for Pachuk-I  To develop 10 daily series at Pachuk-I,

discharge data of Bichom G&D site has been used  Correction factor for 10-daily Bichom series

has been calculated as follows:  10 daily series at Pachuk-I = 10 daily series at

Bichom *(1016/2277)*(2300/1878) CA Ratio

Yield correction factor


Conclusions  2 or 3 years measured discharge data at a project

site does not give appropriate idea of a catchment yield  Yield model at those G&D sites where long term

measured data is available can be prepared  The same based on the catchment hypsometry and

spatial variability of rainfall can be applied at other locations to get an estimate of yield and develop long term water availability series


Thank you


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