The mean, or arithmetic average, is a central concept in mathematics used to find the average of a set of numbers. In the context of daylight hours, calculating the mean requires summing all recorded hours over a year, then dividing by the number of days.
This process provides an indicator of the central tendency of the data distribution. In simple terms, it's the typical amount of daylight one might expect over the year. The mean is particularly informative when comparing two different geographical locations, like Tucson and Anchorage, as it aggregates the influence of high and low extremes experienced seasonally.
A consistent daylight pattern, like in Tucson, results in a mean that's reflective of steady daily averages. On the other hand, Anchorage's highly variable daylight pattern could skew the mean, potentially showing lower annual averages due to its long, dark winters despite its bright summers.
- Sum all data points (total daylight hours).
- Divide by the number of observations (days of the year).
- Interpret the mean in context—consider geographic and seasonal implications.
Understanding the mean helps provide a summary statistic that simplifies and conveys a general sense of the data set, making comparisons between different locales clear and meaningful.