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Climate Risk Assessment of the
Hydropower Sector in Nepal: Issues and
Challenges of Using Climate Projections
Divas B. Basnyat
Nepal Development Research Institute (NDRI)
divas@ndri.org.np
1
30 January 2019, ICIMOD, Kathmandu, Nepal
Regional Workshop - Future Climate Projections and their Applications in South Asia
Outline
• Current and Future Climate (Projections) of
Nepal
• NDRI’s experience using climate projections
• Background- Climate Risk Assessment of the
Hydropower Sector in Nepal
• Issues and challenges in using Climate
Projections
2Regional Workshop- Future Climate Projections and their Applications in South Asia
Precipitation - variability
3
GPCC Precipitation
Observed Precipitation
Lack of reliable and long-term hydro-met data especially in higher elevations is a key
limitation to understanding current risks and future changes. Source: NDRI et al (2017)
Regional Workshop - Future Climate Projections and their Applications in South Asia
Hydrological Variability
4
High seasonal and
inter-annual variations
-Higher in rain-fed than
in snow-fed catchments
-Higher in smaller
catchments
Variability is influenced by
catchment elevation, size
and location
Source: NDRI et al (2017)
Regional Workshop - Future Climate Projections and their Applications in South Asia
Climate Projections : 2040-2059
5
• Most models project higher monsoon precipitation but winter
precipitation is more uncertain
• Warmer future but models vary in magnitude of change
Source: NDRI et al (2017)
Regional Workshop - Future Climate Projections and their Applications in South Asia
• Higher extreme precipitation means higher flood and related
sediment load
• GCM models project increase in 1-day and 5-day maximum
precipitation
Extreme Precipitation
6
Source: NDRI et al (2017)
Regional Workshop - Future Climate Projections and their Applications in South Asia
NDRI Experience on Climate
Projections
Project GCM/RCMs Used
Disaster Risk Reduction
and Climate Change
Adaptation in the Koshi
River Basin, Nepal
(2012) – START/CDKN
• Two RCMs- PRECIS – HadCM3Q0 and PRECIS – ECHAM05
(IPCC SRES A1B) - DHM Data Portal
• Bias corrected using power- transformation method for P
and simple mean and standard deviation correction for T
• Both models are wet biased over the Koshi Region
• RCMs models are cold-biases for most of the study area.
Flood inundation
analysis in lower West
Rapti Basin (2010) -
ICHARM
• Two GCMs, MRI-AGCM 3.1S and 3.2S under IPCC A1B
(ESGF portal)
• Bias Correction - Distribution mapping; APHRODITE used
• Magnitude and frequency of floods projected to increase
Adaptation to climate
change in
Hydroelectricity sector
in Nepal (2016) - CDKN
• 23 CMIP5 GCM models for scenarios, RCP4.5 and RCP8.5
(http://climatewizard.ciat.cgiar.org)
• Wide variations and uncertainty in projections
• Bottom-up CRA adopted
7Regional Workshop - Future Climate Projections and their Applications in South Asia
Climate Risk Assessment (CRA)
8
Source: García, L.E. et al., 2014; Ray & Brown, 2015
Regional Workshop- Future Climate Projections and their Applications in South Asia
Key Indicators – Water, Food and Energy
Security
Key Climate Parameters of Interest
• Water Availability (Supply) -
flow duration (reliability), daily,
seasonal, low flows (droughts),
floods, sediments, landslides
• Renewable energy – solar, wind
• Precipitation (P) variation –monsoon pattern,
intensity and frequency (shorter intervals –
hours, days), cloud bursts, rain, no-rain days …
• Temperature – temporal and spatial variation
• Solar radiation, cloud cover, wind
• Agriculture – crop water
requirements, cropping
patterns, yield ..
• Precipitation (reliability, variation)
• Reference Evapotranspiration (ETo) - daily mean
global solar radiation, air temperature, humidity
and wind speed
• Energy (electricity) – heating,
cooling, lighting
• Precipitation, temperature – mean and variation
• Other uses- recreation, aquatic
life, navigation, flood control
• Precipitation, temperature variation
• Intensity and frequency of P (hourly, daily)
9Regional Workshop - Future Climate Projections and their Applications in South Asia
Precipitation
Rainfall
Infiltration
Soil
Evaporation
Lateral
Flow
Plant Uptake
and
Transpiration
Percolation
Shallow
Aquifer
Deep Aquifer
Return Flow
Surface
Runoff
Streamflow
Transmission
loss
Snowfall
Snowcover
Snowmelt
Seepage
Time delay Time delay
Threshold Temperature
Understanding Runoff response to Climate Change
using SWAT Model
10
Rainfall- Run-off - Curve Number
PET Calculation - Hargreaves
Snow melt–
Degree Day Model
Runoff response to CC-
Jammu
11
U/S Outlet D/S outlet (JAMMU)
Water Yield(mm) for Pre Monsoon
U/S
D/S
MID
Source: NDRI et al (2017)
Regional Workshop - Future Climate Projections and their Applications in South Asia
12
T-Sensitivity: Impact on Water
Balance(Jammu)
U/S
D/S
MID
Upstream Mid-stream Down-stream
Snowfall(mm)Snowmelt(mm)ET(mm)Yield(mm)
T-Sensitivity: Impact on Water Balance
• Nepal has complex, climate, hydrology and topography
• Wide differences in vulnerability, plants, locations, etc
• Future climate change is very uncertain
• Technically possible to address all risks ,
but danger too much or too little
• Trade off between costs now
versus future benefits later
Adaptation is challenging
13Regional Workshop - Future Climate Projections and their Applications in South Asia
We want to know what to do
now! not what to do in 2050
14
IRR 12%
IRR 11.2%
IRR 10.9%
IRR 11.4%
Base
CC
Adapt
in
design
Learn,
Act
later
+40
+80
Impacts of climate and non climate factors on project
economics of Hydropower Projects
%
0%
5%
10%
15%
20%
UP UP UP UP Phased Phased Phased Phased
Hewa Kabeli RG KGK Hewa Kabeli RG KGK
IRR
IRR
Base Median Scenario Worst Case + Extreme
Discount Rate
Regional Workshop - Future Climate Projections and their Applications in South Asia
Issues and Challenges
• Deep uncertainty – multiple projections, data scarcity, model limitations
• Downscaling and bias correction (scarce observations, current climate highly
variable)
• Skill to model Asian Monsoon esp. the Himalayan region (topography, micro-climate
etc.)
• Skill of Climate Models at appropriate temporal (daily/monthly) and spatial scales,
extreme events (floods and droughts) relevant to water projects
• Selection of Climate Models (envelop method) – sectoral needs
• IPCC’s 1.50C warming target- what does it mean to mountain catchments?
• Communication gaps among climate scientists, hydrologists/analysts, decision
makers – e.g. on information on basic principles and dynamics (process) of climate
models
• Conventional hydrological analysis (e.g. frequency analysis) based on “stationarity”
of the variables, climate change introduces “non-stationarity”
• Stakeholders’ perspective (private sector, government, ..) – future impacts?
• ?
16Regional Workshop - Future Climate Projections and their Applications in South Asia
17
Thank You

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Day 2 divas basnet, nepal development research institute (ndri), nepal, arrcc-carissa workshop

  • 1. Climate Risk Assessment of the Hydropower Sector in Nepal: Issues and Challenges of Using Climate Projections Divas B. Basnyat Nepal Development Research Institute (NDRI) divas@ndri.org.np 1 30 January 2019, ICIMOD, Kathmandu, Nepal Regional Workshop - Future Climate Projections and their Applications in South Asia
  • 2. Outline • Current and Future Climate (Projections) of Nepal • NDRI’s experience using climate projections • Background- Climate Risk Assessment of the Hydropower Sector in Nepal • Issues and challenges in using Climate Projections 2Regional Workshop- Future Climate Projections and their Applications in South Asia
  • 3. Precipitation - variability 3 GPCC Precipitation Observed Precipitation Lack of reliable and long-term hydro-met data especially in higher elevations is a key limitation to understanding current risks and future changes. Source: NDRI et al (2017) Regional Workshop - Future Climate Projections and their Applications in South Asia
  • 4. Hydrological Variability 4 High seasonal and inter-annual variations -Higher in rain-fed than in snow-fed catchments -Higher in smaller catchments Variability is influenced by catchment elevation, size and location Source: NDRI et al (2017) Regional Workshop - Future Climate Projections and their Applications in South Asia
  • 5. Climate Projections : 2040-2059 5 • Most models project higher monsoon precipitation but winter precipitation is more uncertain • Warmer future but models vary in magnitude of change Source: NDRI et al (2017) Regional Workshop - Future Climate Projections and their Applications in South Asia
  • 6. • Higher extreme precipitation means higher flood and related sediment load • GCM models project increase in 1-day and 5-day maximum precipitation Extreme Precipitation 6 Source: NDRI et al (2017) Regional Workshop - Future Climate Projections and their Applications in South Asia
  • 7. NDRI Experience on Climate Projections Project GCM/RCMs Used Disaster Risk Reduction and Climate Change Adaptation in the Koshi River Basin, Nepal (2012) – START/CDKN • Two RCMs- PRECIS – HadCM3Q0 and PRECIS – ECHAM05 (IPCC SRES A1B) - DHM Data Portal • Bias corrected using power- transformation method for P and simple mean and standard deviation correction for T • Both models are wet biased over the Koshi Region • RCMs models are cold-biases for most of the study area. Flood inundation analysis in lower West Rapti Basin (2010) - ICHARM • Two GCMs, MRI-AGCM 3.1S and 3.2S under IPCC A1B (ESGF portal) • Bias Correction - Distribution mapping; APHRODITE used • Magnitude and frequency of floods projected to increase Adaptation to climate change in Hydroelectricity sector in Nepal (2016) - CDKN • 23 CMIP5 GCM models for scenarios, RCP4.5 and RCP8.5 (http://climatewizard.ciat.cgiar.org) • Wide variations and uncertainty in projections • Bottom-up CRA adopted 7Regional Workshop - Future Climate Projections and their Applications in South Asia
  • 8. Climate Risk Assessment (CRA) 8 Source: García, L.E. et al., 2014; Ray & Brown, 2015 Regional Workshop- Future Climate Projections and their Applications in South Asia
  • 9. Key Indicators – Water, Food and Energy Security Key Climate Parameters of Interest • Water Availability (Supply) - flow duration (reliability), daily, seasonal, low flows (droughts), floods, sediments, landslides • Renewable energy – solar, wind • Precipitation (P) variation –monsoon pattern, intensity and frequency (shorter intervals – hours, days), cloud bursts, rain, no-rain days … • Temperature – temporal and spatial variation • Solar radiation, cloud cover, wind • Agriculture – crop water requirements, cropping patterns, yield .. • Precipitation (reliability, variation) • Reference Evapotranspiration (ETo) - daily mean global solar radiation, air temperature, humidity and wind speed • Energy (electricity) – heating, cooling, lighting • Precipitation, temperature – mean and variation • Other uses- recreation, aquatic life, navigation, flood control • Precipitation, temperature variation • Intensity and frequency of P (hourly, daily) 9Regional Workshop - Future Climate Projections and their Applications in South Asia
  • 10. Precipitation Rainfall Infiltration Soil Evaporation Lateral Flow Plant Uptake and Transpiration Percolation Shallow Aquifer Deep Aquifer Return Flow Surface Runoff Streamflow Transmission loss Snowfall Snowcover Snowmelt Seepage Time delay Time delay Threshold Temperature Understanding Runoff response to Climate Change using SWAT Model 10 Rainfall- Run-off - Curve Number PET Calculation - Hargreaves Snow melt– Degree Day Model
  • 11. Runoff response to CC- Jammu 11 U/S Outlet D/S outlet (JAMMU) Water Yield(mm) for Pre Monsoon U/S D/S MID Source: NDRI et al (2017) Regional Workshop - Future Climate Projections and their Applications in South Asia
  • 12. 12 T-Sensitivity: Impact on Water Balance(Jammu) U/S D/S MID Upstream Mid-stream Down-stream Snowfall(mm)Snowmelt(mm)ET(mm)Yield(mm) T-Sensitivity: Impact on Water Balance
  • 13. • Nepal has complex, climate, hydrology and topography • Wide differences in vulnerability, plants, locations, etc • Future climate change is very uncertain • Technically possible to address all risks , but danger too much or too little • Trade off between costs now versus future benefits later Adaptation is challenging 13Regional Workshop - Future Climate Projections and their Applications in South Asia
  • 14. We want to know what to do now! not what to do in 2050 14 IRR 12% IRR 11.2% IRR 10.9% IRR 11.4% Base CC Adapt in design Learn, Act later +40 +80
  • 15. Impacts of climate and non climate factors on project economics of Hydropower Projects % 0% 5% 10% 15% 20% UP UP UP UP Phased Phased Phased Phased Hewa Kabeli RG KGK Hewa Kabeli RG KGK IRR IRR Base Median Scenario Worst Case + Extreme Discount Rate Regional Workshop - Future Climate Projections and their Applications in South Asia
  • 16. Issues and Challenges • Deep uncertainty – multiple projections, data scarcity, model limitations • Downscaling and bias correction (scarce observations, current climate highly variable) • Skill to model Asian Monsoon esp. the Himalayan region (topography, micro-climate etc.) • Skill of Climate Models at appropriate temporal (daily/monthly) and spatial scales, extreme events (floods and droughts) relevant to water projects • Selection of Climate Models (envelop method) – sectoral needs • IPCC’s 1.50C warming target- what does it mean to mountain catchments? • Communication gaps among climate scientists, hydrologists/analysts, decision makers – e.g. on information on basic principles and dynamics (process) of climate models • Conventional hydrological analysis (e.g. frequency analysis) based on “stationarity” of the variables, climate change introduces “non-stationarity” • Stakeholders’ perspective (private sector, government, ..) – future impacts? • ? 16Regional Workshop - Future Climate Projections and their Applications in South Asia