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२०८२ मङ्सिर १९, शुक्रबार
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जलविद्युत सोलार वायु बायोग्यास पेट्रोलियम अन्तर्राष्ट्रिय जलवायु ऊर्जा दक्षता उहिलेकाे खबर हरित हाइड्रोजन ईभी सम्पादकीय बैंक पर्यटन भिडियो छापा खोज प्रोफाइल ऊर्जा विशेष ऊर्जा

Kathmandu; Under the informative weekly column "Urja Gyan" published every Friday by Urja Khabar, this week we are presenting insights on how the monsoon and seasonal river flow affect hydropower generation. In the previous edition of the same column, we had discussed "Production, Advantages and Disadvantages of Green Hydrogen."

How do monsoon and seasonal river flows affect electricity generation?

Answer:

Monsoon and the seasonal flow in rivers and streams have positive as well as negative effects on the generation of hydropower. These are elucidated point-wise as follows:

1. Positive Impacts

Increase in Water Availability

Monsoon rainfall increases the water level in rivers. More availability of water increases the generation capacity and plant load factor in hydropower.

Maximum Electricity Production

Hydropower plants run on full capacity during the monsoon months starting from June to October. The country generates maximum amount of electricity during this period.

Reduced Dependence on Expensive Energy Sources

With increased hydropower generation, reliance on more expensive energy alternatives decreases-diesel generators and thermal backup systems, for instance.

Reservoir Refill

Reservoir and semi-reservoir projects benefit most from the monsoon. Fully filled reservoirs can supply stored water during the dry season.

Improved Grid Stability

Higher production enhances operational flexibility. It stabilizes frequency, provides reserve margins, and allows the system to respond better to peak demand.

2. Negative Impacts

Floods and Excessive Flow

Sudden increases in river flow during monsoon cause various issues such as damage to hydropower structures and flooding in powerhouse areas.

Forced Shutdowns of Turbines

Many run-of-river hydropower plants have to be shut down during the monsoon due to excessive sediment load (siltation) and a high flood risk.

High sediment and debris flow

Heavy rain produces landslides along riverbanks, adding a large amount of soil, sand, and debris to the river. It causes:

  • erosion of turbine blades - runners
  • greater maintenance needs
  • frequent shutdowns
  • higher operational costs
  • Uncertainty in River Flow

Flash floods, landslides, and large boulders entering the river add more risks. Similarly, river flow patterns vary during agricultural irrigation in the monsoon.

Transmission and Distribution Problems

Line faults, tower collapses, outages, and grid instability occur due to heavy rain, lightning, windstorms, and storms.

Safety Risks

High flows in rivers create safety risks for dams, intakes, and workers around the structure. Risks of drowning, hazards during gate operation, and other accidents also increase.

3. Seasonal Impacts (Dry Season)

Decrease in River Flow

The river flow drastically shrinks during winter and pre-monsoon months from December to June. Many run-of-river plants function merely at 20–30% of their capacity.

Pressure of Load Shedding

This causes imbalance in supply and demand, hence import of electricity, load management, and possible cuts for the industrial consumers in the dry season. Rising Cost of Supply Low river flow reduces hydropower generation, thus reducing revenue for the generating companies and increasing costs. Consequently, Nepal Electricity Authority will have to import expensive electricity or resort to using backup systems. Slow Reservoir Refill Prolonged drought delays refilling of reservoirs. Long-term effects are on multi-year reservoir projects and irrigation schedules.

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