Transcript Slide 1
Effects of projected climate change on
energy supply and demand in the
Pacific Northwest and Washington
State
Alan F. Hamlet
Se-Yeun Lee
Kristian Mickelson
Marketa McGuire Elsner
•JISAO/CSES Climate Impacts Group
•Dept. of Civil and Environmental Engineering
University of Washington
Human Health
Infrastructure
Water Resources
Agriculture/Economics
Coasts
A comprehensive
climate change impacts
assessment for
Washington State
Forest Resources
Energy
Salmon
Adaptation
Global Climate Change Scenarios
for the PNW
Consensus Forecasts of Temperature and Precipitation Changes from IPCC AR4 GCMs
21st Century Climate Impacts for the Pacific Northwest Region
Mote, P.W. and E. P. Salathe Jr., 2009: Future climate in the Pacific Northwest
Overview of the WA Energy Assessment:
Part I: Changes in Energy Supply from the
Columbia River Hydro System
Part II: Changes in Energy Demand for
Space Heating and Cooling Needs
Part I: The Columbia River
Hydro System
•Supplies 70% of the Region’s Electricity
•Is primarily responsible for the relatively low
cost of energy in the PNW
•Strongly affects local energy supplies in WA
•Strongly influenced by climate
Snapshot of Snohomish Co. PUD
Overview of Methods
Temperature
Changes
Hydrologic
Changes
Precipitation
Changes
Changes in
Hydropower
Production
Schematic of VIC Hydrologic Model and
Energy Balance Snow Model
Snow Model
Columbia River Hydro System
Changes in Modified Flow in the Columbia River at The Dalles, OR
14,000
Streamflow (cms)
12,000
10,000
Historic
2020_A1B
2040_A1B
2080_A1B
8,000
6,000
4,000
2,000
0
Oct Nov Dec Jan Feb Mar Apr May Jun
Jul
Aug Sep
18
16
14
12
10
8
6
4
2
0
Hamlet et al., 2009: Effects of Projected Climate Change on Energy
Supply and Demand in the Pacific Northwest and Washington State
S ep
Aug
J ul
J un
May
Apr
Mar
F eb
J an
D ec
Nov
His toric
E nergy_2020_A 1B
E nergy_2040_A 1B
E nergy_2080_A 1B
O ct
S ys tem Wide E nerg y
P roduc tion
(million MW-hrs )
Streamflow Timing Shifts in the Columbia River Will Impact
Regional Electrical Energy Production
Conclusions:
•2020s: regional hydropower production is projected to
increase by 0.5-4% in winter, decrease by 9-11% in
summer, with annual reductions of 1-4%. By the
•2040s: hydropower production is projected to increase by
4.0-4.2% in winter, decrease by about 13-16% in summer,
with annual reductions of about 2.5-4.0%.
•2080s: hydropower production is projected to increase by
7-10% in winter, decrease by about 18-21% in summer, with
annual reductions of 3.0-3.5%.
•The largest and most robust changes in hydropower
production are projected to occur from June-Sept, during
the peak air conditioning season.
Outflow from Priest Rapids Dam
(Hanford Reach) (cms)
Changes in Simulated Regulated Flow
6000
5500
5000
4500
4000
3500
3000
2500
2000
1500
1000
500
0
Historic
2020_B1
2040_B1
2080_B1
2020_A1B
2040_A1B
2080_A1B
0.01 0.12 0.23 0.34 0.45 0.56 0.67 0.78 0.89
Probability of Exceedance
Important Adaptation Considerations:
Climate change will increasingly disrupt the existing balance
between hydropower, flood control, and instream flow
augmentation in the basin, requiring adjustments in reservoir
operating policies.
Transboundary relationships between ID, WA, OR and
between Canada and the U.S. will be impacted, requiring
potential adjustments in transboundary agreements such as
the Columbia River Treaty.
Losses of summer energy production may have important
inter-regional impacts because of loss of local capacity and
reduced ability to provide energy transfers to CA and the
southwest in summer.
Part II: Changes in Primary Energy Demand for
Space Heating and Cooling Needs
•Is a fundamental driver of residential and light
commercial energy demand
•Strongly influenced by climate via temperature
(heating and cooling degree days)
•Has important implications for individuals,
utilities, and high-level planning at the regional
and state level
End-Use Energy Consumption by Sector (1970-2001)
1,600
1,400
1,200
Trillion Btu
Transportation
1,000
800
600
Industrial
400
Commercial
200
Residential
0
1970
1975
1980
1985
1990
http://www.cted.wa.gov/site/533/default.aspx
1995
2000
Source: EIA SEDS
Overview of Methods
Monthly
Temp.
Changes
Heating
Degree
Days
Population
Growth
Heating
Energy
Demand
Overview of Methods
Monthly
Temp.
Changes
Cooling
Degree
Days
Population
Growth
A/C Use
Cooling
Energy
Demand
Heating and Cooling Degree Days
t max t min
HDD max 0,18.33
2
(65 ˚F)
t max t min
CDD max 0,
23.89
2
(75 ˚F)
Relationship Between CDD and A/C_Pen
Gridded Heating and Cooling Energy
Demand Indices
Heating Energy Demand Index (HEDI)
HEDI = Population * (Annual HDD)
Cooling Energy Demand Index (CEDI)
CEDI = A/C_Pen * Population * (Annual CDD)
Combined Growth Management Act
and Gridded Pop of the World v3 Data Sets
Changes in Heating Energy Demand in WA
Avg Heating Energy Demand
(million person-HDD)
8.0
Population growth alone
7.0
6.0
Warming alone (A1B)
Warming with pop growth (A1B)
5.0
4.0
+22%
+56%
+35%
3.0
2.0
1.0
0.0
2000
2020
2040
2080
Changes in Residential Cooling Energy Demand in WA
Avg Cooling Energy Demand
(million person-CDD)
0.7
Population growth alone
0.6
0.5
Warming alone (A1B)
Warming with pop growth (A1B)
+1845%
0.4
0.3
0.2
0.1
+550%
+200%
0.0
2000
2020
2040
2080
Comparison of Peak Demand in the
PNW and N. CA
Westerling A, Barnett T, Gershunov A, Hamlet AF, Lettenmaier DP, Lu N, Rosenberg E, Steinemann AC
(2008) Climate forecasts for improving management of energy and hydropower resources in the
western U.S., California Energy Commission, PIER Energy-Related Environmental Research Program.
CEC-500-2008-XXX
Conclusions
•Despite decreasing heating degree days with
projected warming, annual heating energy demand
is projected to increase due to population growth.
•Residential cooling energy demand is projected to
increase rapidly due to increasing population,
increasing cooling degree days, and increasing
use of air conditioning.
•Peak electrical demands in summer will likely
increase due to increased population, CDD, and
A/C penetration in the PNW.
Important Adaptation Considerations:
•Individual consumers and some businesses will likely
see overall reductions in annual heating and cooling
energy needs (especially in western WA).
•Utilities, by comparison, will face rising demand
across the board, and especially in summer when
CDD and A/C use are projected to increase
dramatically. Reductions in regional energy sources
from hydropower will intensify impacts to utilities in
summer, and may increase prices to consumers.
Overview of Adaptation Strategies:
•Increase energy capacity using renewable and
conventional resources to meet projected
increases in demand.
•Reduce per capita demand via changes in enduse technology, building standards, solar energy
installations on residential and commercial
buildings, conservation, etc.
•Change water management policy governing
the Columbia River hydro system.