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Evaluating Alternative Operations Strategies to Improve Travel Time ...

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SHRP 2 L11: Final Appendices<br />

Equation 3: European Put Option with EV Variability<br />

f<br />

( x;<br />

µ , σ )<br />

Gumbel<br />

1<br />

= e<br />

σ<br />

where<br />

−(<br />

x−µ<br />

)<br />

σ<br />

µ = location parameter<br />

σ = scale parameter<br />

and where<br />

e<br />

−(<br />

x−µ<br />

)<br />

σ<br />

−e<br />

x is the random variable of interest<br />

This formulation may be useful in situations in which speed variability is due entirely <strong>to</strong> a rare<br />

event that occurs within a relatively short interval. For example, this might apply <strong>to</strong> a normally<br />

uncongested country road where an accident occurs, causing speed reductions (delays) that<br />

represent an EV distribution. Sufficient data would be needed <strong>to</strong> estimate the location, scale, and<br />

shape parameters for the EV distribution. Conceptually, the valuation of unreliability would then<br />

proceed in a manner completely analogous <strong>to</strong> the manner described earlier where speeds are<br />

distributed log-normally.<br />

An Illustrative Example of the European Put Option<br />

A more-typical case occurs when the events that precipitate unreliability are known <strong>to</strong> be<br />

distributed EV, but there is no record of associated traffic metrics. This can be because insufficient<br />

data is collected or because speed is not a sufficient measure of the impact of the events on<br />

network reliability. In this case, the event distribution is estimated from information regarding the<br />

event, rather than from a roadway performance metric such as speed. This means that a second<br />

step can link the events <strong>to</strong> travel-time performance.<br />

This situation is illustrated using the European EV put formulation in a setting of avalanche<br />

closures. Avalanches have characteristics of rare events, in that for most days and months in the<br />

winter, no avalanches occur, but periodically, avalanches of varying intensity and extensiveness<br />

occur. If an avalanche event is distributed EV, then Equation 3 can provide us with the certaintyequivalent<br />

value of closure duration under various conditions of control or mitigation of the<br />

avalanche impacts.<br />

The other relevant feature of this example is that the traffic count data, though collected with high<br />

frequency in the vicinity of the avalanche; do not fully convey the traffic unreliability associated<br />

with the avalanche. Specifically, without considerable additional effort, one cannot determine the<br />

useful traffic performance metrics associated with the avalanche. Thus, the unreliability valuation<br />

exercise must be broken in<strong>to</strong> two pieces. First, the duration of avalanches can be analyzed in an<br />

options framework <strong>to</strong> derive a certainty-equivalent delay from the (presumed) EV-distributed<br />

duration data. Thus, highly variable and rare-event data can be reduced <strong>to</strong> a deterministic indica<strong>to</strong>r.<br />

Second, a separate study (not performed here) linking closure duration <strong>to</strong> traffic delay can then be<br />

applied <strong>to</strong> the certainty equivalent closure duration for monetizing the benefits of a strategy or<br />

treatment.<br />

The illustrative example that is presented here is of an avalanche closure for Snoqualmie Pass on I-<br />

90 in the State of Washing<strong>to</strong>n. The rare event nature of a road closure caused by an avalanche is<br />

determined by examining the number of hours of pass closure per month (for December through<br />

VALUATION OF TRAVEL-TIME RELIABILITY FOR RARE EVENTS Page C-6

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