initial evidence for self-organized criticality in blackouts ben carreras & bruce poole oak...

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Initial evidence for self-organized criticality in blackouts Ben Carreras & Bruce Poole Oak Ridge National Lab David Newman Physics, U. of Alaska Ian Dobson ECE, U. of Wisconsin

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Page 1: Initial evidence for self-organized criticality in blackouts Ben Carreras & Bruce Poole Oak Ridge National Lab David Newman Physics, U. of Alaska Ian Dobson

Initial evidence for self-organized criticality

in blackouts

Ben Carreras & Bruce Poole Oak Ridge National Lab

David NewmanPhysics, U. of Alaska

Ian DobsonECE, U. of Wisconsin

Page 2: Initial evidence for self-organized criticality in blackouts Ben Carreras & Bruce Poole Oak Ridge National Lab David Newman Physics, U. of Alaska Ian Dobson

Two approaches to blackouts:

1 Analyze specific causes and sequence of events for each blackout.

2 Try to understand global, complex system dynamics.

Page 3: Initial evidence for self-organized criticality in blackouts Ben Carreras & Bruce Poole Oak Ridge National Lab David Newman Physics, U. of Alaska Ian Dobson

Gaussian model

Uncorrelated random disturbances (eg weather) drive a linear system to produce blackouts.

Then H 0.5 for large timespdf tails are exponential

Look at time series of blackout sizes

Hurst parameter H:H=1.0 deterministic H>0.5 + correlationH=0.5 uncorrelated

Page 4: Initial evidence for self-organized criticality in blackouts Ben Carreras & Bruce Poole Oak Ridge National Lab David Newman Physics, U. of Alaska Ian Dobson

Analysis of NERC data

Then H = 0.7

pdf tails ~ (blackoutsize)^(-0.98)

Look at daily time series of blackout sizes1993-1998.

Analyze using SWV and R/S

H = 0.7 blackouts correlated with later blackouts

Consistent with SOC dynamics!

Page 5: Initial evidence for self-organized criticality in blackouts Ben Carreras & Bruce Poole Oak Ridge National Lab David Newman Physics, U. of Alaska Ian Dobson

Ingredients of SOC in idealized sandpile

• system state = local max gradients • event = sand topples (cascade of

events is an avalanche)1 addition of sand builds up sandpile2 gravity pulls down sandpile• Hence dynamic equilibrium with

avalanches of all sizes and long time correlations

Page 6: Initial evidence for self-organized criticality in blackouts Ben Carreras & Bruce Poole Oak Ridge National Lab David Newman Physics, U. of Alaska Ian Dobson

SOC dynamic equilibrium in power system transmission?

• system state = loading pattern• event = limiting or zeroing of flow

(events can cascade as flow redistributes)

• [cascadezero load] = blackout1 load demand drives loading up2 response to blackout relieves

loading specific to that blackout

Page 7: Initial evidence for self-organized criticality in blackouts Ben Carreras & Bruce Poole Oak Ridge National Lab David Newman Physics, U. of Alaska Ian Dobson

Conclusions• NERC data shows long range time

correlations and power dependent pdf tails.

• Consistent with SOC hypothesis but SOC not yet established.

• Suggest qualitative description of opposing forces which could cause SOC: load demands vs. responses to blackouts.

• Study of global complex system dynamics could lead to insights and perhaps monitoring and mitigation of large blackouts

Page 8: Initial evidence for self-organized criticality in blackouts Ben Carreras & Bruce Poole Oak Ridge National Lab David Newman Physics, U. of Alaska Ian Dobson

100

101

102

103

104

105

106

0 500 1000 1500 2000

Energy unserved (MWh)

Time (day)

Figure 2. Blackout energy unserved time series.

Page 9: Initial evidence for self-organized criticality in blackouts Ben Carreras & Bruce Poole Oak Ridge National Lab David Newman Physics, U. of Alaska Ian Dobson

0.1

1

10

1

10

100

10 100 1000

Time lag (days)

Number events H = 0.50

MWh unserved H = 0.70

σ

m

( )events

σm

( )MWh unserved

Scaled windowed variance analysis of the number of blackouts

Page 10: Initial evidence for self-organized criticality in blackouts Ben Carreras & Bruce Poole Oak Ridge National Lab David Newman Physics, U. of Alaska Ian Dobson

10

-7

10

-6

10

-5

10

-4

10

1

10

2

10

3

10

4

10

5

P= 0.00455 *(MWh)

-0.98

Probability

MWhour unserved

Probability distribution function of energy unserved

for North American blackouts 1993-1998.

Page 11: Initial evidence for self-organized criticality in blackouts Ben Carreras & Bruce Poole Oak Ridge National Lab David Newman Physics, U. of Alaska Ian Dobson

Power system Sand pile

system state loading pattern gradient profile

driving force customer demand adding sand

relaxing force response to blackout gravity

event limit flow or trip sand topples

Analogy between power system and sand pile

Page 12: Initial evidence for self-organized criticality in blackouts Ben Carreras & Bruce Poole Oak Ridge National Lab David Newman Physics, U. of Alaska Ian Dobson

Time series Hurst exponent H

Number of blackouts 0.52

Energy unserved (MWh) 0.70

Power lost (MW) 0.58

Number of customers 0.69

Restoration time 0.67

Hurst exponents of blackout numbers and sizes

Page 13: Initial evidence for self-organized criticality in blackouts Ben Carreras & Bruce Poole Oak Ridge National Lab David Newman Physics, U. of Alaska Ian Dobson

0

1000

2000

3000

4000

5000

6000

0 500 1000 1500 2000

Power loss (MW)

Time (days)

Figure 1. Blackout power loss time series.