Britannica AI Icon

Quick Summary

Temperature is a measure of hotness or coldness, expressed on scales like Fahrenheit and Celsius. It indicates the direction of heat energy flow, moving from hotter to colder bodies. Air temperatures originate from the Sun's radiant energy absorption and are influenced by the atmosphere, oceans, and land.123

Short-term temperature fluctuations can be dramatic. A cold front can cause rapid temperature drops, while descending air over mountains can lead to significant increases. Temperatures generally decrease with altitude due to less favorable radiation balance and the expansion of rising air, a phenomenon known as the adiabatic lapse rate.23

Summary created from Britannica articles using AI. AI can make mistakes, so verify using Britannica articles.

Ask Britannica AI about this topic

Britannica doesn't have a full article on this topic, so we've curated a list of our relevant coverage.