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3 Univariate Statistics













           3.1 Introduction

           The statistical properties of a single parameter are investigated by means of
             univariate analysis. Such variable could be the organic carbon content of a
           sedimentary unit, thickness of a sandstone layer, age of sanidine crystals in a
           volcanic ash or volume of landslides in the Central Andes. The number and
           size of samples we collect from a larger  population is often limited by fi nan-
           cial and logistical constraints. The methods of univariate statistics help to
           conclude from the  samples for the larger phenomenon, i.e., the  population.
             Firstly, we describe the sample characteristics by means of statistical
           parameters and compute an empirical distribution ( descriptive statistics)
           (Chapters 3.2 and 3.3). A brief introduction to the most important measures
           of central tendency and dispersion is followed by MATLAB examples.
           Next, we select a theoretical distribution, which shows similar characteris-
           tics as the empirical distribution (Chapters 3.4 and 3.5). A suite of theoreti-
           cal distributions is then introduced and their potential applications outlined,
           before we use MATLAB tools to explore these distributions. Finally, we try
           to conclude from the sample for the larger phenomenon of interest ( hypoth-
           esis testing) (Chapters 3.6 to 3.8).  The corresponding chapters introduce the
           three most important statistical tests for applications in earth sciences, the
           t-test to compare the means of two data sets, the F-test comparing variances
                   2
           and the χ -test to compare distributions.


           3.2 Empirical Distributions


           Assume that we have collected a number of measurements of a specifi c ob-
           ject. The collection of data can be written as a vector x
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