Search USGS⌕ Search

Geology topics

P.W. Mielke

Publications and source records attributed to P.W. Mielke.

3 recordsLinked to original sources

Rank score and permutation testing alternatives for regression quantile estimates

Performance of quantile rank score tests used for hypothesis testing and constructing confidence intervals for linear quantile regression estimates (0 ≤ τ ≤ 1) were evaluated by simulation for models with p = 2 and 6 predictors, moderate collinearity among predictors, homogeneous and hetero-geneous errors, small to moderate samples ( n = 20–300), and central to upper quantiles (0.50–0.99). Test statistics evaluated were the conventional quantile rank score T statistic distributed as χ 2 random variable with q degrees of freedom (where q parameters are constrained by H 0 :) and an F statistic with its sampling distribution approximated by permutation. The permutation F -test maintained better Type I errors than the T -test for homogeneous error models with smaller n and more extreme quantiles τ. An F distributional approximation of the F statistic provided some improvements in Type I errors over the T -test for models with > 2 parameters, smaller n , and more extreme quantiles but not as much improvement as the permutation approximation. Both rank score tests required weighting to maintain correct Type I errors when heterogeneity under the alternative model increased to 5 standard deviations across the domain of X . A double permutation procedure was developed to provide valid Type I errors for the permutation F -test when null models were forced through the origin. Power was similar for conditions where both T - and F -tests maintained correct Type I errors but the F -test provided some power at smaller n and extreme quantiles when the T -test had no power because of excessively conservative Type I errors. When the double permutation scheme was required for the permutation F -test to maintain valid Type I errors, power was less than for the T -test with decreasing sample size and increasing quantiles. Confidence intervals on parameters and tolerance intervals for future predictions were constructed based on test inversion for an example application relating trout densities to stream channel width:depth.

Journal of Statistical Computation and Simulation↗

Geological applications of multi-response permutation procedures

The multi-purpose permutation procedures (MRPP) test statistic is designed to analyze multivariate data at the ordinal or higher levels. It is based on the weighted averages of symmetric distance functions over all paired objects within a priori disjoint groups of objects from a finite population of objects where each object's response is a point in an r-dimensional space. Thus, the arguments of each r-dimensional point correspond to the r measured responses of each object in the finite population of objects. The null hypothesis underlying MRPP is that the observed sample of objects within groups of a specified size structure is randomly obtained from the pooled collection of objects comprising the finite population. The procedure is used to test the presumed geomorphic differences among three reaches of the Lower Mississippi River. A combination of the proposed reaches is favored and several variable-based reach configurations are proposed. ?? 1993 International Association for Mathernatical Geology.

Mathematical Geology↗

An empirical coverage test for the g-sample problem

A nonparametric g-sample empirical coverage test has recently been developed for univariate continuous data. It is based upon the empirical coverages which are spacings of multiple random samples. The test is capable of detecting any distributional differences which may exist among the parent populations, without additional assumptions beyond randomness and continuity. The test can be effective with the limited and/or unequal sample sizes most often encountered in geologic studies. A computer program for implementing this procedure, G-SECT 1, is available. ?? 1991 International Association for Mathematical Geology.

Mathematical Geology↗