Final answer:
In meteorology, the temperature typically changes by an average of 1°C for each 100 m change in altitude, known as the dry adiabatic lapse rate, though this can vary due to atmospheric conditions.
Step-by-step explanation:
The temperature change with elevation is commonly referred to as the lapse rate in the field of meteorology, which is a part of physics. For dry air, the average lapse rate is 9.8°C per 1000 m (or about 1°C per 100 m) decline in altitude, known as the dry adiabatic lapse rate. However, this value can change under different atmospheric conditions, such as humidity levels and variations in the composition of the atmosphere. It's important to note that in real-world scenarios, the actual lapse rate can vary from this average due to local weather conditions and geographic features. This concept is essential in understanding weather patterns, climate, and the esposure rate of temperatures when ascending or descending in altitude.