The process of determining average temperature involves aggregating temperature readings over a specific period and dividing by the number of readings. For instance, to ascertain the daily average, one sums the high and low temperatures and divides the result by two. This provides a representative temperature for that day. More complex calculations, utilizing multiple readings throughout the day, offer a more refined average.
The determination of average temperature serves various critical functions. It enables the tracking of climatic trends over time, facilitates informed decision-making in sectors such as agriculture and energy, and aids in monitoring potential environmental changes. Historical temperature records, processed to derive averages, provide invaluable insights into long-term climate patterns and potential anomalies.