Measures, Metrics¶
Risks¶
This page outlines tools under investigation for real-time areas at risk identification.
Rates of Change of River Level¶
Let
represent the time series of a gauge's river level measures, separated by \(\tau\) hours, and unit of measure ↠ millimetres. Then the weighted-rate-of-change, w.r.t. each \(\tau\) hours interval, is
wherein
- \(i = 0, 1, 2, 3, \ldots\)
- \(t\:\) is a/the current time point.
- \(r_{t - i\tau}\:\) is the rate of change at time point \(t - i\tau\), and its unit of measure is millimetres/hour.
Noting that
determines the relative river level change w.r.t. consecutive river level values, i.e., values that are \(\tau\) hours apart.
Drift¶
For time series drift calculations, this hub depends on
- Jensen-Shannon Distance \(J_{dist}\)
- Wasserstein Distance \(\mathcal{W}\)
wherein
\(J_{div}\) is the Jensen-Shannon Divergence, a method for determining the similarity of a pair of distributions1. The similarity between a pair of distributions increases as \(J_{dist} \rightarrow 0\). Note, for a pair of distributions
therefore
The Wasserstein Distance is a distance measure2.
Important, do not consider scores in isolation, also consider the pattern of the scores over time.
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Study Divergence Measures Based on Shannon Entropy for an in-depth understanding of Jensen-Shannon Divergence. ↩
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Part 6 of From GAN to WGAN has an in-depth discussion of the Wasserstein Distance. GAN: Generative Adversarial Network, WGAN: Wasserstein Generative Adversarial Network ↩