ste6an-hub.r-universe.dev

[ste6an-hub] evd 2.3-7.1

alec_stephenson@hotmail.com (Alec Stephenson) — Sun, 22 Sep 2024 03:02:17 GMT

Extends simulation, distribution, quantile and density functions to univariate and multivariate parametric extreme value distributions, and provides fitting functions which calculate maximum likelihood estimates for univariate and bivariate maxima models, and for univariate and bivariate threshold models.

[ste6an-hub] evdbayes 1.1-3

alec_stephenson@hotmail.com (Alec Stephenson) — Wed, 01 Mar 2023 08:00:05 GMT

Provides functions for the Bayesian analysis of extreme value models, using Markov chain Monte Carlo methods. Allows the construction of both uninformative and informed prior distributions for common statistical models applied to extreme event data, including the generalized extreme value distribution.

[ste6an-hub] PlayerRatings 1.1-0

alec_stephenson@hotmail.com (Alec Stephenson) — Sun, 01 Mar 2020 14:50:06 GMT

Implements schemes for estimating player or team skill based on dynamic updating. Implemented methods include Elo, Glicko, Glicko-2 and Stephenson. Contains pdf documentation of a reproducible analysis using approximately two million chess matches. Also contains an Elo based method for multi-player games where the result is a placing or a score. This includes zero-sum games such as poker and mahjong.

[ste6an-hub] cubing 1.0-5

alec_stephenson@hotmail.com (Alec Stephenson) — Mon, 23 Apr 2018 11:29:32 GMT

Functions for visualizing, animating, solving and analyzing the Rubik's cube. Includes data structures for solvable and unsolvable cubes, random moves and random state scrambles and cubes, 3D displays and animations using 'OpenGL', patterned cube generation, and lightweight solvers. See Rokicki, T. (2008) for the Kociemba solver.

[ste6an-hub] TideHarmonics 0.1-1

alec_stephenson@hotmail.com (Alec Stephenson) — Thu, 04 May 2017 07:16:54 GMT

Implements harmonic analysis of tidal and sea-level data. Over 400 harmonic tidal constituents can be estimated, all with daily nodal corrections. Time-varying mean sea-levels can also be used.