Abstract
We present a method for drawing isolines indicating regions of equal joint exceedance probability for bivariate data. The method relies on bivariate regular variation, a dependence framework widely used for extremes. The method we utilize for characterizing dependence in the tail is largely nonparametric. The extremes framework enables drawing isolines corresponding to very low exceedance probabilities and may even lie beyond the range of the data; such cases would be problematic for standard nonparametric methods. Furthermore, we extend this method to the case of asymptotic independence and propose a procedure which smooths the transition from hidden regular variation in the interior to the first-order behavior on the axes. We propose a diagnostic plot for assessing the isoline estimate and choice of smoothing, and a bootstrap procedure to visually assess uncertainty.
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Acknowledgements
Cooley, Thibaud, and Castillo received support from the project “EaSM 2: Advancing extreme value analysis of high impact climate and weather events” NSF-DMS-1243102. Wehner’s contributions to this work are supported by the Regional and Global Climate Modeling Program of the Office of Biological and Environmental Research in the Department of Energy Office of Science under contract number DE-AC02-05CH11231.
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Appendix
Appendix
We show that the smoothed scaling procedure in Section 4 preserves the requirement that isolines of exceedance probabilities must have negative slopes.
Assume the estimated survival function is strictly decreasing, i.e., if x1 = (x1,1,x1,2)≠x2 = (x2,1,x2,2), x1,1 ≤ x2,1, and x1,2 ≤ x2,2, then \(\hat {\bar F}_{\boldsymbol X}(\boldsymbol x_{1}) > \hat {\bar F}_{\boldsymbol X}(\boldsymbol x_{2})\). We first show that it follows that any isoline \(\hat \ell _{\boldsymbol X}(p)\) must have a negative slope. Let x1 and x2 be two distinct locations on \(\hat \ell _{\boldsymbol X}(p)\). WLOG, assume x2,2 − x1,2 ≥ 0 and x2,1 − x1,1 ≥ 0, implying the slope is not negative. This implies x2,2 ≥ x1,2 and x2,1 ≥ x1,1, but \(\hat {\bar F}_{\boldsymbol X}(\boldsymbol x_{1}) = \hat {\bar F}_{\boldsymbol X}(\boldsymbol x_{2})\), which is a contradiction.
As the transformation to Fréchet scale is monotonic, \(\hat \ell _{\boldsymbol Z}(p)\) has negative slopes.
Let \(\boldsymbol z_{1}^{(proj)}, \boldsymbol z_{2}^{(proj)}\) be any two points in \(\hat \ell _{\boldsymbol Z}(p_{proj})\). Let s = pbase/pproj. Let \(\boldsymbol z_{1}^{(base)}, \boldsymbol z_{2}^{(base)}\) be the points in \(\hat \ell _{\boldsymbol Z}(p_{base})\) such that \(\boldsymbol z_{i}^{(proj)} = (s^{\eta _{1}(\boldsymbol z_{i}^{(base)})} z^{(base)}_{i,1},\)\( s^{\eta _{2}(\boldsymbol z_{i}^{(base)})} z^{(base)}_{i,2})\) for i = 1, 2. WLOG assume \(z^{(base)}_{2,2} < z^{(base)}_{1,2}\) and \(z^{(base)}_{2,1} > z^{(base)}_{1,1}\).
Note that since \(z^{(base)}_{2,1} > z^{(base)}_{1,1}\), \(\eta _{1}(\boldsymbol z^{(base)}_{2}) > \eta _{1}(\boldsymbol z^{(base)}_{1})\), and likewise since \(z^{(base)}_{2,2} < z^{(base)}_{1,2}\), \(\eta _{2}(\boldsymbol z^{(base)}_{2}) < \eta _{2}(\boldsymbol z^{(base)}_{1})\). Hence,
and
Thus, the slope between any two points on \(\hat \ell _{\boldsymbol Z}(p_{proj})\) is negative, and since the marginal transformation is monotonic, the slope between any two points on \(\hat \ell _{\boldsymbol X}(p_{proj})\) is negative.
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Cooley, D., Thibaud, E., Castillo, F. et al. A nonparametric method for producing isolines of bivariate exceedance probabilities. Extremes 22, 373–390 (2019). https://doi.org/10.1007/s10687-019-00348-0
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DOI: https://doi.org/10.1007/s10687-019-00348-0