Descriptive statistics, univariate data, data distributions

Author

Mason Stahl (ENS-215)

Published

February 19, 2026

At this point in the term, you’ve

Established a foundation in programming and basic computer science concepts
Learned key concepts and tools in data wrangling/manipulation
Learned key concepts and tools in data visualization
Manipulated, analyzed, visualized, and interpret many large datasets (often containing > 10,000 rows and tens of columns!)
Learned some key concepts and tools in data acquisition
Learned some key concepts and tools in map making

Today and in upcoming lectures you will learn some foundational concepts and technical aspects related to the interpretation and statistical components of exploratory data analysis. These tools and concepts will allow you extract greater information and understanding from your data and to make more rigorous and defensible statements related to your analysis.

We will begin this stage of the class with a refresher/introduction to basic statistics and deeper dive into univariate data.

Univariate data

Univariate data is data that consists of observations of a single quantitative variable. For instance when we examine a a set of temperature data we are dealing with univariate data (i.e. the single characteristic in this case is temperature). Often we will break univariate data into categories (e.g. temperatures before year 1950 and temperatures after 1950) to see how the statistics and distributions of these groups differ.

When we compare two quantitative variables (e.g. temperature and precipitation) together we are dealing with bivariate data, which we will dive into in a greater detail in upcoming lectures. However, for today we will just focus on univariate data.

Before we move on, let’s load in a univariate dataset that we can work with in today’s lecture. We’ll load in the NOAA monthly precipitation dataset that we’ve worked with prior

Code

library(tidyverse)

Code

precip_data <- read_csv("https://stahlm.github.io/ENS_215/Data/NOAA_State_Precip_LabData.csv")

Take a quick look at the data to re-familiarize yourself with it.

Now let’s create a new dataset that just has the precipitation data for NY.

Code

ny_precip <- filter(precip_data, state_cd == "NY")

Basic statistics refresher

Kinds of data

Nominal (categorical)

Nominal variables are categorical data that have no inherent ordering/ranking. For example:

Country (US, Canada, China,…)
Rock type (limestone, shale, basalt,…)
Land use (agricultural, residential, forested,…)
Species

Ordinal

Ordinal data is similar to categorical except that there is an inherent ordering/ranking to the data. For example:

Concentration categories (e.g. very low, low, medium, high, very high)
Storm intensity categories (e.g. Category 1, Category 2, Category 3,…)

Continuous and discrete

Measurements can be described as either continuous or discrete.

Continuous variables have values that can take all possible intermediate values. For example temperature, concentration, flow are all continuous variables.

Discrete variables can only take a certain set of values. For example number of individuals is reported as integers and can only take integer values (e.g. number of individuals could be 500 people or 501 people but not 500.02524 people).

Population vs. sample

A population (in statistics) refers to a the whole group of objects or values that exist. Typically is it not possible to measure all possible objects, and thus a sample, which is a subset of the population is measured.

For instance, imagine you are a fisheries biologist and you would like to know the average mass of salmon in a river. It is not feasible to capture and weigh every salmon (i.e. the population), so instead you collect measurements on a subset of the population (i.e. a sample) and make inferences based on this sample.

In the vast majority of cases where you deal with data, you will be dealing with samples and not populations. In later lectures we will discuss how we can mathematically evaluate our degree of confidence for an estimate derived from a sample.

Measures of location

Mean

The mean is simply the sum of the all of the values in a sample divided by the sample size (number of values). The mean of a population is typically denoted by the Greek letter \(\mu\) (pronounced “mu”) and the sample mean is denoted by \(\bar x\) (pronounced “x bar”).

\(\mu = \frac{\sum_{i=1}^n x_i}{n}\)

As you are already well aware and have done hundreds of times by now, the mean is computed in R using the mean() function.

What is the monthly mean precipitation in New York? Before taking the means you should first add a new column to ny_precip whose values are “Pre-1950” if the year is before 1950 and “Post-1950” if the year is 1950 or later. Then compute the following means.
- For all years
- For years before 1950
- For years \(\ge\) 1950

Code

# Your code here

Are the means between the two periods different?

Quantiles

Quantiles are an important way of describing a dataset. The \(f\) quantile, \(q(f)\), of a set of data is the value in a dataset such that a fraction \(f\) of the data are less than or equal to that value (Cleveland, 1994)¹. For example, the 0.25 quantile (also referred to as the 25^th percentile) is the value in a given dataset where 25% of the data are less than that value.

To compute a quantile \(q(f)\) for a given dataset, you first need to compute the percentile ranking of each value in a dataset. Once the data have been ordered from smallest to largest, the percentile \(f_i\) for the i^th value, \(x_i\) is computed as follows:

\(f_i = \frac{i-0.5}{n}\)

\(q(f)\) is then the value of \(x\) that has corresponds to \(f\).

It is worth noting that there are other methods (algorithms) for computing quantiles, they are all generally similar though may differ in some of the finer detail (e.g. how tied values are treated,…)

You are all likely familiar with quantiles as you have dealt with medians before. The median of a dataset is the 0.50 quantile (50^th percentile). The median, like the mean, is a measure of location. However, the median is not skewed by outlier values like the mean.

You can use the quantile() function from the stats package to compute the value at specified quantiles for a given dataset. In the example below, we compute the 5^th, 25^th, 50^th, 75^th, and 95^th percentiles for monthly rainfall in NY.

Code

quantile(ny_precip$Precip_inches, probs = c(0.05, 0.25, 0.50, 0.75, 0.95))

    5%    25%    50%    75%    95% 
1.6200 2.5275 3.2500 4.1200 5.5725

Exercise

Add a column called frac to the ny_precip data frame, which has the fraction \(f\) (i.e. the percentile ranking) for each precipitation value in the dataset. Note: you can compute it relatively easily using the equation shown above or you can rely on a function in dplyr that will do it for you.

You table should look similar the one below

Measures of spread

The spread (or variability) of a variable is an important property to consider when analyzing a dataset. Among other things, the spread of a dataset gives us an idea of the range of possible values a variable can take as well as how confident we can be when making statements regarding the data when we have only a limited sample.

Variance and standard deviation

The variance is the average of the of squared deviations from the mean for all of the observations. The population variance is denoted by \(\sigma^2\) and the sample variance is denoted by \(s^2\).

\(\sigma^2 = \frac{1}{n}\sum_{i=1}^n (x_i-\mu)^2\)

The standard deviation, \(\sigma\) (population) and \(s\) (sample), is simply the square root of the the variance. The standard deviation has the same units as the measurements.

So essentially, the variance and standard deviation are telling us on average how much the sample values deviate from the sample mean. A sample with a variance of zero, implies that all of the measured values are equal to the mean (i.e. there is no sample variation). As the variance grows it indicates that there is greater deviation from the mean (i.e. the samples are not tightly clustered about the mean).

In the graphic below I’ve created two samples (A and B) that have the exact same mean (mean = 5.0), though the variances differ. The variance of Group A = 0.01, and the variance of Group B = 0.56.

You can easily compute the variance using the var() function and the standard deviation using the sd() function.

Exercise

Compute the variance and standard deviation of the NY precipitation data:
- For all years
- For years before 1950
- For years \(\ge\) 1950

Has the variance (and standard deviation) changed over time? Conceptually what does this mean.

Range and interquartile range

The range is the difference between the largest and smallest value in a dataset. One thing to note is that the range tends to increase as your sample size increases (due to the fact that you are more likely to eventually sample extreme values as you sample size grows).

The interquartile range (also denoted IQR) is the difference between the 25^th percentile and 75^th percentile values in a datset. The IQR is useful in that it tells us the range in which we can expect to find the middle 50% of the sample.

You can compute the interquartile range either by using the quartile() function and taking the difference between the 75^th and 25^th percentile or by using the IQR() function

Code

quantile(ny_precip$Precip_inches, probs = 0.75) - quantile(ny_precip$Precip_inches, probs = 0.25) # using quantile

   75% 
1.5925

Code

IQR(ny_precip$Precip_inches) # using IQR function

[1] 1.5925

Coefficient of variation

The coefficient of variation is a measure of spread and is defined as the ratio of the standard deviation to the mean.

\(CV =\frac{\sigma}{\mu}\)

The CV is widely used in chemistry and engineering (to characterize the precision/repeatability of a process or measurement).

The CV is particularly useful when comparing how meaningful the degree of variation (i.e., \(\sigma\)) is as compared against the central value (i.e., \(\mu\)) of a given dataset. For instance consider a two different manufacturing process, where process A is making a part that should be 100 m in length and process B is making a part that should be 0.01 m in length. As in any manufacturing process there is not perfect precision and thus there is some variation of the length of the parts made within each process. Below are some statistics regarding the manufacture of 5000 parts from both Process A and B.

Process A has a mean of 100.00 m and a standard deviation of 0.100 m.
Process B has a mean of 0.010 m and a standard deviation of 0.001 m.

As you can see the standard deviation is much lower in process B as compared to A. However, this does not tell the whole story. Let’s take a look at the coefficient of variation for the two processes.

Process A has a \(CV = \frac{0.100\, m}{100.00\, m} = 0.001\)

Process B has a \(CV = \frac{0.001\, m}{0.010\, m} = 0.1\)

Thus, we can see that since the mean is also much smaller in process B, the standard deviation of B is a much greater proportion of the mean part length. The CV helps to highlight that Process B has much greater variation in the part sizes relative to the average part size. Thus, the manufacturer would see that the Process B parts are not particularly well manufactured since the variation amounts to 10% of the mean size.

Important note: The CV should only be calculated for data that is measured on measurement scales that have a meaningful zero value (i.e., ratio scale). For instance, you would not want to compute CVs on temperature data that is measured in C or F, since their zero values do not actually represent a true physical minimum value. Thus the computed CV would be dependent on the scale (units) used. The example, I presented above makes sense since length does indeed have a true physical minimum of zero and thus our CV is independent of the units used (i.e., we could have used units of feet and we would get the same answer for the CV).

Shape

The shape of distribution helps us in part describe how symmetric (or asymmetric) the data distribution is as well as which portions of the distribution have the greatest density.

Modes

The modes, which are the most common values, are frequently used to describe a distribution. The graphic below shows the distribution of a unimodal sample - one that has a single peak in its distribution.

The distribution below has two peaks and thus is described as bimodal

Skewness

The skewness of a distribution describes its symmetry (or asymmetry). The graphic below shows a symmetric distribution.

Asymmetric distributions are described as skewed.

A right-skewed distribution has a long-tail to the right. These distributions are positively skewed, as they have extreme positive values that occur with low probability.

A left-skewed distribution has a long-tail to the left. These distributions are negatively skewed, as they have extreme negative values that occur with low probability.

Visualizing and interpreting univariate distributions: first steps

You’ve already been visualizing and also interpreting univariate distributions, however previously you were more focused on the programming and generating visuals as opposed to rigorously describing the data. Now that you have a basic framework and language to begin characterizing data distributions, we will further expand your understanding by going into the technical details and approaches to interpreting data distributions.

Box plots

Box plots provide a nice visual summary of a sample’s distribution. The box plot does not show all of the data points, but rather displays some key summary statistics that describe the distribution of the data.

The graphic below shows an example box plot, with the features of the graphic nicely annotated.

The geom_boxplot() function from the ggplot2 package generates a box plot with the features shown above.

Code

ny_precip %>% 
  ggplot(aes(x = state_cd, y = Precip_inches)) + 
  geom_boxplot(fill = "grey") + 
  
  labs(y = "Precip (inches)",
       x = ""
       ) +
  
  theme_classic()

the box plot is helpful in that it succinctly displays the summary statistics related to the distribution of a given variable. However, it does not display the data points themselves (except for the outliers), while this is often desired when summarizing data, we sometimes would like to see all of the data in addition to the box plot. To do this we can simply add a geom_jitter() layer on top of our box plot.

Code

ny_precip %>% 
  ggplot(aes(x = state_cd, y = Precip_inches)) + 
  geom_boxplot(fill = "grey") + 
  
  geom_jitter(alpha = 0.1, width = 0.15, height = 0) +
  
  labs(y = "Precip (inches)",
       x = ""
       ) +
  
  theme_classic()

Based on the graphic above:
- Does the distribution of precipitation in NY appear symmetric or skewed?
- Does the distribution appear unimodal or multimodal?
- What is range of monthly precipitation values within which the middle 50% of samples fall?
- What is the maximum monthly precipitation ever recorded in NY?

Note, that we specified height = 0 in the geom_jitter() function to prevent jittering in the y-direction (since this would jitter the y-values which is the variable of interest).

Box plots (and other graphics showing a variables distribution) are particularly useful when comparing univariate distributions between groups (e.g. precipitation pre-1950 and post-1950).

In past labs have used box plots to visualize distributions, however we hadn’t gone into the the technical details of comparing distributions. Let’s look at the pre-1950 and post-1950 precipitation in NY and examine how the distributions compare with one another.

Code

ny_precip %>% 
  ggplot(aes(x = time_period, y = Precip_inches)) + 
  geom_boxplot(fill = "grey", notch = TRUE) + 
  
  labs(y = "Precip (inches)",
       x = ""
       ) +
  
  theme_classic()

Notice how we specified notch = TRUE in the geom_boxplot() function. The notches around the median values display confidence intervals around the median. Since we can’t know the “true” median based on any given sample, these confidence intervals essentially tell us the range of plausible values that the “true” median is likely to fall within.

If the notches overlap between two groups then we do not have statistical confidence that the medians are truly different between the groups (i.e. difference may simply be due to chance based on limited sample sizes). If the notches do not overlap then we can have statistical confidence that the medians differ.

We will cover confidence intervals in later lectures, though I am introducing them now so that are aware of the concept and can start to employ the concept in your project/lab work if you want.

Exercise

Create a box plot comparing the precipitation distribution between months (just using the NY data)
1. Try adding additional features that help you interpret the data (e.g. jittered points, notches,…)
2. Think about the features of the monthly distributions. How do the distributions vary between months (with respect to medians, IQR, skewness,…)

Like we did with NY, use a box plot to compare the pre and post-1950 precipitation for another state of your choosing. Examine the distributions and discuss how they compare and how they differ between time periods.
Choose a subset of 4 states from the full precipitation dataset precip_data. Using this subset of states generate a box plot that compares the precipitation between the states. Think about how the precipitation distribution varies across the states and discuss these features with your classmates.
Practice with the statistics functions. Using the full precipitation dataset precip_data you should
1. Generate a summary table that has the 25^th, 50^th, and 75^th percentile monthly precipitation values and the standard deviation for each state.
2. Generate a dot plot showing these values

Your graphic will look similar to the one below

Visualizing and interpreting univariate distributions

Let’s continue learning about how to generate visualizations that display a univariate data distribution and how to interpret these data.

First we’ll load in the ggridges package, which has some useful functions for visualizing data distributions.

You probably don’t have the ggridges package yet so first go ahead and install it in your Package window.

Code

library(ggridges)

Before we move on, let’s load in a univariate dataset that we can work with in today’s lecture. We’ll load in the NOAA monthly precipitation dataset that we’ve worked with prior

Code

precip_data <- read_csv("https://stahlm.github.io/ENS_215/Data/noaa_cag_state_precipitation.csv")

Let’s add a column with state abbreviations to the dataset and rename a few columns.

Code

df_names <- tibble(STATE = state.name, state_cd = state.abb)

precip_data <- precip_data %>% 
  left_join(df_names) %>% 
  rename(Year = YEAR,
         Month = MONTH,
         Precip_inches = Value
         )

Code

precip_data <- precip_data %>% 
  mutate(time_period = if_else(Year >= 1950,"Post-1950","Pre-1950"))

Take a quick look at the data to re-familiarize yourself with it.

Now let’s create a new dataset that just has the precipitation data for NY.

Code

ny_precip <- precip_data %>% 
  filter(state_cd == "NY")

Histograms and density plots

Histograms are another method of displaying the distribution of univariate data. A histogram bins the values and plots the frequency of values falling into each bin. Typically the bins are of equal width

Let’s generate a histogram of the monthly precipitation data for NY to highlight how they look and their utility. To generate a histogram we use geom_histogram(). Notice that we only need to pass a single variable (in this case Precip_inches). The histogram displays values of the variable on the x-axis and the number of occurrences (counts) within bins (ranges) of the variable.

Code

ny_precip %>% 
  ggplot(aes(Precip_inches)) +
  geom_histogram(bins = 30) +
  theme_classic()

You can see that the bins (columns) are of equal width and their height corresponds to the number of observations falling within that bin. For instance, the bin with the most observations is from 2.98-3.26 inches and has >150 observations.

Histograms allow you to identify how frequently values of the variable of interest are observed (in the above example monthly precipitation in inches). By looking at the histogram and comparing bar heights you can determine the relative frequencies in each bin.

Looking at the above histogram we can see that while observed monthly precipitation values range from near zero to about 8 inches, the vast majority of observations fall within 2 to 5 inches. While observations outside of the range 2 to 5 inches do occur, we can see that they are relatively infrequent.

You can specify the number of bins using the bins = argument to allow for greater control over your histogram’s appearance and the level its level of detail.

Oftentimes we are interested in displaying relative frequencies on the y-axis and not the absolute number of observations in each bin. To display the relative frequency you can specify stat(density) or stat(ndensity) in your aes() function. The density and ndensity display the bin heights that have been normalized so that the area integrates to one (density) or so that the height of the tallest bin is one (ndensity)

The example below demonstrates the use of stat(density)

Code

ny_precip %>% 
  ggplot(aes(Precip_inches, stat(density))) +
  geom_histogram() +
  theme_classic()

Warning: `stat(density)` was deprecated in ggplot2 3.4.0.
ℹ Please use `after_stat(density)` instead.

`stat_bin()` using `bins = 30`. Pick better value `binwidth`.

Now generate a similar histogram, this time using bins = 50 and setting the stat to ndensity

Code

# Your code here

You can generate a smoothed version of a histogram, which is referred to as a density curve, using the geom_density() function. The area under the density curve integrates to one.

Code

ny_precip %>% 
  ggplot(aes(Precip_inches)) +
  geom_density(fill = "grey") +
  theme_classic()

Does the histogram/density plot provide more information than a box plot?
Based on the density plot, is the above distribution symmetric or skewed?
What else can you conclude based on the density plot? Look back at the stats overview section to recall how we describe distributions.

Density curves are a great way to compare distributions between groups. We can examine how the modes, ranges, central tendancies, and relative frequencies across values vary between the different groups.

Let’s use density curves to examine how the distribution of monthly precipitation has changed over time in the state of New York.

Code

ny_precip %>% 
  ggplot(aes(Precip_inches, group = time_period, fill = time_period)) +
  geom_density(alpha = 0.5) +
  scale_fill_manual(values = c("grey", "blue")) +
  theme_classic()

Describe the distributions (symmetry/skewness, modes, …)
- Add vertical lines showing the medians for each of the periods
Has the distribution of precipitation changed over time? With you neighbor discuss the potential implications of any changes.

You saw above how overlaying density curves can be a great way to compare the distribution of a univariate data between multiple groups. With the example above we were comparing just two groups so the graphic wasn’t too cluttered and we were able to easily interpret the results. However, when you want to compare more than 2 or 3 groups, the graphic can become difficult to read.

In the example below we are comparing the distribution of monthly precipitation between five US states. You can see that with five groups the graphic is becoming unwieldy.

Code

precip_data %>% 
  filter(state_cd %in% c("NY","FL","CA","AZ","NE")) %>% 
  ggplot() + geom_density(aes(x = Precip_inches, fill = state_cd), alpha = 0.3) +
  theme_classic()

Thankfully, we can rely on the geom_density_ridges() function from the ggridges package. This function puts each density curve on its own baseline – allowing us to easily compare across groups while keeping the graphic uncluttered. The graphic below displays the exact same data as the previous example, though this time the graphic is much easier to read.

Code

precip_data %>% 
  filter(state_cd %in% c("NY","FL","CA","AZ","NE")) %>% 
  ggplot(aes(x = Precip_inches, y = state_cd)) + 
  geom_density_ridges(aes(fill = state_cd)) +
  theme_classic()

Picking joint bandwidth of 0.326

Exercise

Examine the precipitation distribution between each month for the state of Florida (FL). You should use a geom_density_ridges plot as part of your analysis. You can also generate a summary table with precipitation statistics for each month.

Based on your analysis describe the distribution of precipitation within each month and across months
- Is there a strong seasonal pattern in precipitation?
- Are the monthly distributions (some or all) skewed? Left-skewed? Right-skewed?
- Do some months display a wide range of precipitation values (i.e. high variance) and do others have a tighter distribution of values?
- With your neighbors discuss any potential environmental and/or societal issues that might result from the precipitation patterns observed.
- When you finish the above, you should try the same exercise on another state. California is pretty interesting to check (as I’m sure many other states are as well).

Below is an example of what your graphic should like like – note that I am plotting NY here and you should plot FL. Try to make your graphic presentation quality (look back at our lectures on presentation quality graphics for additional guidance).

Create density curves that examine how the distribution of precipitation has changed from pre-1950 to post-1950 for the following US states: “NY”,“NH”,“VT”,“ME”.

Do this with a single call to ggplot(). On the graphic for each state you should have two density curves (one for each time period). Hint: you will need to rely on faceting here.

Have conditions become wetter or drier in the Northeast?
Have extreme events become more or less frequent?
Has the variability in monthly precipitation changed? With your neighbor discuss some of the implications of any changes.

Quantile plots and cumulative distributions

Histograms and density curves display the density of observations across the range of values that the variable of interest takes. At a given value on the x-axis, the higher/taller the curve/bar the greater the frequency of observations at (or around) that value.

Another way of displaying a variables distribution is with quantile plots or with cumulative distribution plots, which are quantile plots where the axes have been flipped.

Note that we can use the cume_dist() function to compute the f-value for each observation (i.e. the percentage of observations \(\le\) to that observation).

Let’s create a quantile plot showing the distribution of monthly precipitation in New York.

Code

ny_precip %>% 
  ggplot(aes(x = cume_dist(Precip_inches), y = Precip_inches)) +
  geom_point(size = 1) +
  theme_classic() + 
  labs(title = "Quantile plot",
       subtitle = "NY monthly precipitation",
       x = "f-value",
       y = "Monthly precipitation (inches)",
       caption = "Data source: NOAA")

The quantile plot is very useful when characterizing and describing the distribution of a variable’s values. The f-value corresponding to a given value of the variable (in this case monthly precipitation) indicates that a proportion \(f\) of the observations are less than or equal to the corresponding variable value.

For instance, in the above graphic, an f-value of 0.25 corresponds to 2.5275 inches. This means that 25% of the observations have a precipitation value less than or equal to 2.5275 inches.

In a quantile plot, sections of the plot where the curve is flat indicate a high density of observations over the corresponding range of y-values. For example, note how the curve is very flat between f-values of 0.25 and 0.75. This reveals that as you go from the 25^th to 75^th percentile there is very little change in the monthly precipitation value – thus 50% of the observations fall in a very tight range of precipitation values (in this case 2.5275 to 3.25 inches).

Furthermore, steep areas of the curve indicate a low density of observations over the corresponding range of y-values. For instance, the top 10% of samples (from f-values 0.9 to 1.0) has a precipitation range from 5.025 to 8.58 inches. This is a huge range in values as we move 10 percentage points (from 90^th to 100^th percentile). Compare this with the 50% of observations between f-values of 0.25 to 0.75, that fall within a much narrower range of precipitation values (2.5275 to 3.25 inches).

Cumulative distribution plots Cumulative distribution plots are identical to a quantile plot, except the x and y axes are switched. Cumulative distributions provide another way of examining the distribution of univariate data.

Let’s create a cumulative distribution plot showing the distribution of monthly precipitation in New York.

Code

ny_precip %>% 
  ggplot(aes(x = Precip_inches, y = cume_dist(Precip_inches))) +
  geom_line(linewidth = 1) +
  theme_classic() + 
  labs(title = "Cumulative distribution plot",
       subtitle = "NY monthly precipitation",
       x = "Monthly precipitation (inches)",
       y = "f-value",
       caption = "Data source: NOAA")

You interpret cumulative distributions similar to how you interpret quantile plots – however you need to keep in mind that their axes are switched.

Looking at cumulative distribution above, you can quickly see that 90% of the precipitation observations are less than 5.025 inches. You can also see that while monthly precipitation in excess of 7.5 inches has been observed, it is exceedingly rare as it appears that < 1% of observations exceed 7.5 inches ( > 99% of observations are less than 7.5 inches).

FYI, you can also create a cumulative distribution plot using the stat_ecdf() function which is from the ggplot2 package

Code

ny_precip %>% 
  ggplot(aes(Precip_inches)) + 
  stat_ecdf(linewidth = 1) +
  theme_classic() + 
  labs(title = "Cumulative distribution plot",
       subtitle = "NY monthly precipitation",
       x = "Monthly precipitation (inches)",
       y = "f-value",
       caption = "Data source: NOAA")

Exercise

Create a cumulative distribution plot of annual (not monthly) precipitation

You should show the cumulative distribution for “CA”,“FL”,“NY”,“VT”,“NH” on a single graphic (a curve for each state)
Once you’ve created the graphic examine the results and think about the distribution of annual precipitation for each state (e.g. are the values tightly centered around the median, are their significant outliers,…)

`summarise()` has regrouped the output.
ℹ Summaries were computed grouped by state_cd and Year.
ℹ Output is grouped by state_cd.
ℹ Use `summarise(.groups = "drop_last")` to silence this message.
ℹ Use `summarise(.by = c(state_cd, Year))` for per-operation grouping
  (`?dplyr::dplyr_by`) instead.

Challenge

We’ve been examining the distribution of monthly precipitaton data and have made some interesting observations.
We’ve seen that in many states the amount of precipitation varies significantly between the different months. Based on this observation I’d like to pose a challenge.

Can you determine which states have the most precipitation, as a fraction of that state’s total annual precipitation, fall in just three months? Note that the months do not need to be consecutive – for instance, it could be the case that in a given state the three wettest month are Feb, May, Sept and combined they make up 60% of the total annual precipitation.

This question is more than just a programming challenge – it yields insight into how unequal (or equal) the distribution of rainfall is across the months. In an extreme case three months could provide 100% of a state’s precip (very unequal distribution in time). Conversely, in a very uniform distribution of precipitation with time, three months would provide 25% of a state’s precip. How evenly a state’s precip is spread out with time has important ecological and societal implications.

Try giving this challenge a go (you’ll need to rely on many of the dplyr tools you’ve learned).

Code

# Your code here

Footnotes

Visualizing Data (William S. Cleveland, 1993)↩︎