Locally tail-scale invariant scoring rules for evaluation of extreme value forecasts
Helga Kristin Olafsdottir, Holger Rootz\'en, David Bolin

TL;DR
This paper introduces local tail-scale invariant scoring rules for evaluating extreme value forecasts, including a new scaled version of the CRPS, to better assess models in regions with varying extreme event scales.
Contribution
It proposes the concept of local weight-scale invariance and develops the scaled wCRPS score, providing a tailored evaluation method for extreme value models in diverse regions.
Findings
The scaled wCRPS score is effective for extreme event evaluation.
Explicit formulas for the score are derived for GEV distributions.
Simulation and real-world applications demonstrate the score's usefulness.
Abstract
Statistical analysis of extremes can be used to predict the probability of future extreme events, such as large rainfalls or devastating windstorms. The quality of these forecasts can be measured through scoring rules. Locally scale invariant scoring rules give equal importance to the forecasts at different locations regardless of differences in the prediction uncertainty. This is a useful feature when computing average scores but can be an unnecessarily strict requirement when mostly concerned with extremes. We propose the concept of local weight-scale invariance, describing scoring rules fulfilling local scale invariance in a certain region of interest, and as a special case local tail-scale invariance, for large events. Moreover, a new version of the weighted Continuous Ranked Probability score (wCRPS) called the scaled wCRPS (swCRPS) that possesses this property is developed and…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsHydrology and Drought Analysis · Climate variability and models · Meteorological Phenomena and Simulations
