A metric frequently utilized in climatology and meteorology represents the arithmetic mean of the highest and lowest temperatures recorded during a 24-hour period. It is calculated by summing the maximum and minimum temperatures and dividing the result by two. For example, if the highest temperature on a given day is 80 degrees Fahrenheit and the lowest is 60 degrees Fahrenheit, the daily temperature average is 70 degrees Fahrenheit.
This calculated value offers a simplified representation of the thermal conditions experienced on a particular day. It facilitates the comparison of temperatures across different locations and time periods, allowing for the identification of trends and anomalies. Historically, such values have been crucial in agricultural planning, energy consumption forecasting, and public health initiatives, as they provide a general indicator of the day’s thermal environment and its potential impact on various sectors.