the reliability challenge
TRANSCRIPT
BOSTON CHICAGO DALLAS DENVER LOS ANGELES MENLO PARK MONTREAL NEW YORK SAN FRANCISCO WASHINGTON
The Reliability Challenge(aka, “resilience,” “fuel security”)
NEPOOL 2018 Summer MeetingPaul J. HibbardJuly 27, 2018
Page 2NEPOOL SUMMER MEETING 2018
Setting the stage for our two presentations
Key factors related to the fuel security challenge
Implications for competition, reliability, climate
Dr. Seth Climate change – science and regional implicationsDr. Yoshida Lessons from a similarly fuel-constrained energy sector in Japan,
following the Great Earthquake/Tsunami
Discussion following the presentations
Reminder: we are not in Westborough
No agenda items, no votes, no positions being taken
High-level consideration of risks underlying - and stemming from -the challenge
Overview of Discussion
Page 3NEPOOL SUMMER MEETING 2018
Why are we here? For the better part of a decade…
The electric system operator has warned us of reliability challenges during winter conditions
Market incentives have largely worked, and may continue to
But the pace of change increases; the challenge is getting harder, not easier
What is FS/R/R generally, and in this NE context?
Keeping the lights on, getting them back on (nothing new, though added emphasis to resilience of system to storms and other events)
System security and resilience risk in NE: questionable resource availability under certain severe winter conditions (i.e., a system based primarily on variable resources and on-demand fuel transport, with little or no economic storage capability)
What options are available to the region?
Non-electric (i.e., gas) infrastructure investments
Market incentives for actions, investments, fuel contracts
Out of market payments for actions, investments, fuel contracts
Fuel Security/Resilience/Reliability…
Page 4NEPOOL SUMMER MEETING 2018
Existing and recent past efforts
Forward capacity market pay-for-performance (not fully implemented for a few years)
Winter reliability program
Wide range of energy/ancillary services market changes
Job is not done - continued FS/R/R challenges
Little incremental gas supply infrastructure; uncertainty in seasonal delivery resources (i.e., oil, LNG)
Sustained, depressed energy market revenues pushing retirements
Continued susceptibility to severe winters (though demand in decline)
Lack of faith in PFP to address the challenge
New efforts
Market redesign focused on “fuel security” - TBD
New “fuel security” basis for reliability review of resource delists (i.e., notbased on transmission security) – stacking-order calculations given load, resource and fuel inventory assumptions
Current Context
Page 5NEPOOL SUMMER MEETING 2018
Causes: Carbon Policy
Over the past 7-10 years, from “pilot” or marginal, to market significance
Energy efficiency, distributed solar accelerating due to regulatory policies on EE spending, net metering, solar RPS
Major increases in state RPS requirements
Successful renewable LTK procurements
Ongoing procurements in multiple states potentially netting an additional 1-2 GW
Overall potential market impact could approach a third to half of energy needs (generation and BPS load reduction) over next ten years, and more beyond
No let up - state carbon policies expanding rapidly
RGGI – continued reductions to 2030, 2/3 reduction from start of program
Multiple states setting goals, mandates to achieve near carbon-free generation over next couple decades (MA power plant regs – near phase out of fossil gen by 2050)
MA Senate bill – additional procurements, 100% renewables (others to follow?)
Infrastructure challenges
Pipeline siting not easy, to say the least – interstate/intrastate
Gas-fired power plants, oil firing capability face heightened review
Transmission to baseload hydro – recent setbacks
Part traditional local opposition, part campaign to end fossil fuel combustion
Page 6NEPOOL SUMMER MEETING 2018
Causes: Markets Factors
Shale gas upends relative fuel pricing, creates sustained periods of low energy prices
Renewable procurements, EE, and distributed solar extend and amplify price suppression in energy markets, largely due to state policy, not market outcomes
Aging coal, oil, natural gas, nuclear assets: insufficient market revenues to remain operational
Growing reliance on and need for FCM revenues, and shift in market incentives towards capacity payments
Under any structure (including PFP), little sense for developers to reserve new interstate pipeline capacity
Retirement of units heavily relied on for winter reliability pending (Mystic, old oil, nuclear)
Page 7NEPOOL SUMMER MEETING 2018
Where Are We Headed?
Carbon: one direction - external to (at least partly) internal
1980s: quantify in resource planning and procurement
1990s: restructuring – (modest) RPS, (modest) net metering
2000s: RGGI; beginning of policy expansion
2010+s: Massive policy expansionInfrastructure activism
Out of market procurements: returning?
1980s - 1990s: vertical integration; IRP
2000s: Markets & competition; RMRs gone by end of decade
2010s: State-funded procurements; net metering; utility built grid-connected solar; storage
2018: RMRs
Page 8NEPOOL SUMMER MEETING 2018
Questions for the Region
Will the climate policy driver abate?
What does climate science point to? (Dr. Seth)
How much further (with mandates, procurements) are states likely to go? Is there a long-term solution (beyond CASPR) to the state policy-markets disconnect?
Would electrification help or exacerbate the fuel security challenge?
Is new gas infrastructure even a possibility? What would it take?
Can we manage the winter fuel delivery risk?
What does Japan’s experience with LNG tell us? (Dr. Yoshida)
Will anything but a blackout coalesce states around an infrastructure solution? (California experience)
Can a new market design put this to rest, once and for all? Given ISO’s proposed schedule, is there enough time to sort through the question?
Page 9NEPOOL SUMMER MEETING 2018
The Climate Policy Driver: Dr. Anji Seth
Professor and Director of Applied Research, Connecticut Institute for Resilience & Climate Adaptation, Department of Geography, and Chair of the Atmospheric Sciences Group, University of Connecticut. We are not in Westborough
Climate change science; state of knowledge on impacts; implications
The Local Resource Limitation Dilemma: Dr. Phyllis Yoshida
Dr. Phyllis Yoshida, Senior Fellow for Energy and Technology, Sasakawa Peace Foundation USA and former Deputy Assistant Secretary for Asia and the Americas, Office of International Affairs, U.S. Department of Energy
Impact of Fukushima on Japan’s energy systems; lessons for New England
Overview of Discussion
Page 10NEPOOL SUMMER MEETING 2018
Paul J. HibbardAnalysis Group111 Huntington Avenue, 10th Floor Boston, MA [email protected]
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o Observed & Prolected Changes in Temperatures
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o Tropical Cyclones, severe weatheç winter storms, drought
o Sea Level Rise
o Basis for Climate Policy
o Unknown unknowns: "Surprises"
o Carbon Dioxide Removal (CDR), Solar Radiation Management (SRM)
Weather Predictions v. Climate Projections
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During past warm periods over the last several millionsof years, global mean sea level was higher than it istoday.
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Pliocene (-3M years ago): COz was -400ppm (similarto today), temperatures were several degrees C higherthan today with sea levels 10-30m higher.
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Basis for Climate PolicyStabilizing global mean temperature to lessthan 3.6'F (2"C) above preindustrial levels ôrequires substantial reductions in net :íglobal COz emissions prior to 2040 Ërelative to present-day values and likely ¿requires net emissions to become zero or :possibly negative later in the century)
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Commitments that form the foundation of the ParisAgreement cover only approximately one third of the 60
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gap between the reductions needed and thenational pledges made in Paris is alarmingly high .
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Potential "Surprises"1. "Known unknowns"potential changes in correlations between extreme events that may not betheir own but together can increase the iikelihood of compound extremes, i
multiple events occur simultaneously or in rapid sequence.
2. Self-reinforcing cycles, which can give rise to "tipping etemsubcomponents of the Earth system that can be stable in multiple different
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3. "Unknown unknowns" paleoclimate record also suggests possibilityof the emergence of new types of compound events not observed in the h calrecord or predicted by model simulations. E.9., Hurricane Sandy, where sea level rise,anomalously high ocean temperatures, and high tides combined to st both thestorm and the magnitude of the associated storm surge. At the same time, blockingridge over Greenland-a feature whose strength and frequency may be rel ed to bothGreenland surface melt and reduced summer sea ice in the Arctic-red the storm
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Summary
o For next few decades, warming is expected to continue (because the climate isadjusting to GHGs already emitted), and natural variability could amplify orsuppress the warming signal regionally.
o Expect more warm temperature extremes, and fewer [but not zero] coldtemperature extremes.
o Expect more heavy precipitation events.
o Possibly more intense (windspeed, precipitation) winter storms, more intensetropical cyclones.
o Continued greenhouse gas emissions near the current level >> accelerating andlarger, unprecedented changes in extremes, with potential for "surprises".
CDR and SRM
GHG forcing has the potential to push the climate farther into unprecedented states forhuman civilization and increase the likelihood of "surprises"
Limiting the global mean temperature increase through emissions reductions or adaptingto the impacts of a greater-than-3.6"F (2'C) warmer world have been acknowledged asseverely challenging tasks by the international science and policy communities.
Consequently, there is increased interest in exploring additional measures designed toreduce net radiative forcing through other, as yet untested actions, which are oftenreferred to as geoengineering, divided into two categories: carbon dioxide removal(CDR) and solar radiation management (SRM)
IPCC AR5
CDR and SRMcarbon dioxide removal (CDR) and solar radiation management (SRM)
Require potential development of global and national governance and oversightprocedures, geopolitical relations, Iegal considerations, environmental, economic andsocietal impacts, ethical considerations, and the relationships to global climate policyand current GHG mitigation and adaptation actions.
CDR is technically possible, the prrmary challenge is achieving the required scale ofremoval in a cost-effective manner, which in part presumes a comparison to the costs ofother, more traditional GHG mitigation options, with additional ltmitation of longimplementation times.
SRM would not address damage to ocean ecosystems from increasing oceanacidification due to continued CO2 uptake. SRM could theoretically have a significantglobal impact even if implemented by a small number of nations. Even if the reduction inglobal average radiative forcing from SRM was exactly equal to the radiative forcing fromGHGs, the regional and temporal patterns of these forcings would have importantdifferences.
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00
98
1
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1900 1920 1940 1960 1980 2000 2A20
Projected mid-century changesProjected Change in Number of Days Above 90"F
M¡d 21st Century Higher Scenario (RCP8.5)Projected Change in Number of Days Below 32"F
Mid 21st Century Higher Scenario (RCP8.5)
CSSR, 2017
Weighted Multi-Model Mean Weighted Multi-Model Mean
010203040506070 -74 -60 -50 -40 -30 -2A -10 0
About 20*30 more days per year with a maximum over 90"F (32'C) and 20-30 fewer days peryear with a minimum temperature below freezing in the Northeast.
W
Global Mean Temperature Change(b)
2.5
CSSR, 2017(a)
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- CMIPS Natural.Forcing Only* GISTEMP Observed
- HadCRUï4.s Observed
- NOAA Observed
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2000 2020 1880 1900 1920 194A 1960 1980Year
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Temperatures have been increasing globally, with 95% probability due toanthropogenic forcing (i.e., burning fossil fuels,)
* CMIPS All-Forcing* GISTEMP Observed
- HadCRUT4.S Observed
- NOAA Observed
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Sea Leve Rise(c) Water Level Height (ft) above Average Highest Tide
Decade the 5-year Event Becomes a 0.2-year Event
under the lntermediate Scenario(d)
Water Level Height (feet) Decade
0 1 2 3 4 >5 2020 2030 2040 2050 2060 2070 2080 2090 210a <22AA
The extent and depth of minor-to-major coastal flooding during high-water events will continue toincrease in the future as local RSL rises. a median B-fold increase (range of 1.1- to 430-fold increase)is expected by 2050 in the annual number of floods exceeding the elevation of the current 1O0-yearflood event (measured with respect to a 1991-2009 baseline sea level). Under the same forcing, thefrequency of minor tidal flooding (with contemporary recurrence intervals generally <1 year )willincrease even more so in the coming decades , and eventually occur on a daily basis (Figure 12.5b)
i n Da i ry, 20-;"::"#ii:13i3¡rreci pitati on
Winter
Summer
Spring
Fall
The 2}-year return value of theseasonal maximum 1-dayprec¡pitation totals over the per¡od1948-2015. A mix of increasesand decreases is shown.
Change (inches)
WIII
+0.22
+0.0
<0.0 0.0-0.10 0.11-0.20 0.21-0.30 0.31-0.40 >0.40
Projected Changein Daily, 2}-year Extreme Precipitation
Changes in the Z}-year return periodamount for daily precipitation showlarge percentage increases for boththe middle and late 2'l st century. Noregion in either scenario shows adecline in heavy precipitation. Theincreases in extreme precipitationtend to increase with return level, suchthat increases for the 1OO-year returnlevel are about 30% by the end of thecentury under a higher scenario.
Mid-century
Mid-century
Lower Emissions
Higher Ëmissions
Late-century
Late-century
Change (%)
14
+13+12
+10
+13
+10
+11
+12
+13
+13
+10
+12
+11
3
+21
+20
+16
+19
+20
+20
04 5-9 10-14 15+
Observed precipitation extremes
Observed large increases in measures of heavyprecipitation in the Northeast U.S.
For the continental United States there is high confidencein the detection of extreme precipitation increases, whilethere is low confidence in attributing the exiremeprecipitation changes purely to anthropogenic forcing.There is stronger evidence for a human contribution(medium confidence) when taking into account process-based understanding (increased water vapor in awarmer atmosphere), evidence from weather and climatemodels, and trends in other parts of the world.
99th Percentile Precipitation(1e58-2016)
Number of 5-yr, 2 Dary Events(1958-2016)
Change (%)
TIIffiII I<0 0-9 10-19 20-29 30-39 40+
PRo¿ecrons o¡ SuRrnce TeupeRnruRes
2020 -2029 2090 - 20992.5
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Global Average Surface Temperature Change ('C) 0 0.5 1'1.5 2 2.5 3 3.5 4 4.5 5 5.5 6 6.5 7 7.5
('c)
Tem pe ratu re Proj ecti o n sLarge dependence on emissions choices by end of century.
A2
209G2099
2020-2029
“Energy Conundrum”
How to provide an affordable and environmentally friendly energy supply resilient to the unexpected-- with insufficient domestic
resources.
The Great Eastern Japan Earthquake and Tsunami
217 Square Miles Flooded,16,000 Dead, $199 Billion in Direct Damage
“The Quadlemma”
Decreased energy self-sufficiency
A deteriorating trade balance
High electricity tariffs
Increased CO2 emissions
0
10,000
20,000
30,000
40,000
50,000
60,000
70,000
80,000
90,000
196
5
67
69
71
73
75
77
79
81
83
85
87
89
91
93
95
97
99
01
03
05
07
09
11
13
15
City Gas
Power Industry
(1,000 tonne)
Trends in Japan’s LNG Consumption
Source: IEEJ/EDMC, “Handbook of Japan’s and World Energy
and Economic Statistics”
Coking coal import expenditure
Thermal coal import expenditure
Coal’s import expenditure share in total
import expenditure (right axis)
Coal Import Expenditures and their Shares in the Total Import Expenditures
Source: METI Energy White Paper 2017
Recommendations1. Policymakers must ensure electricity and natural gas
market deregulation and reform is transparent, increases competition, and creates opportunities for new actors, and for new technologies and practices.
2. Japan must reverse its underinvestment in and underutilization of renewables as a major source of domestic supply to enhance energy security and environmental sustainability.
3. Japan must give special attention to mass transportation in smart-urban and -suburban environments, vehicle electrification, hydrogen-fuel vehicles, and autonomous-drive technologies to mitigate oil consumption.
Recommendations4. Japan must actively explore the next generation of
advanced nuclear reactors to determine how they can play a role in Japan’s energy future and energy security.
5. Adequate system flexibility, especially the expansion of transmission interconnections, must play a role in lowering energy demand and achieving Japan’s goal of cutting greenhouse gas emissions from 2013 levels by 80 percent by 2050.
6. Japan must limit investment in the fossil fuel power plants to generators with the highest operational efficiency to support environmental and climate goals for security, health, and resiliency.