The average temperature is a measure that represents the typical or expected temperature for a given location, time period and weather conditions. It is calculated by taking into account all the temperatures recorded over a specific period (usually daily readings) and then finding their mean value. The result of this calculation gives an idea about how hot or cold it was on average during that particular day, week, month or year.
For instance, if we take the temperature record for one day in New York City, we might find a range of temperatures from 50°F to 80°F. The mean value would be calculated by adding all these temperatures together and then dividing by the total number of readings taken that day. This result will give us an average temperature for that particular day in New York City, which can help us understand how warm or cold it was on average during that time period.
In summary, the term "average temperature" refers to a measure of central tendency used to describe typical weather conditions over a given period and location.