Being both a mountain dweller and a skier, I’ve always thought that the rule for temperature change in relation to altitude was 3° Fahrenheit per 1,000 feet (or 6°C per 1,000 meters), but I wasn’t too sure and decided to dig a little deeper into a subject that’s becoming more important as we get into full global warming.
Here’s what I’ve found, starting with what causes that change. Temperatures drop as we gain elevation simply simply because atmospheric pressure decreases and the air expands and cools. Now, let’s talk numbers for what’s called the Standard Lapse Rate.
In Fahrenheit, temperature drops approximately 3.5°F per 1,000 feet of elevation gain (or roughly 5°F per 1,000 meters). In Celsius, temperature drops approximately 6.5°C per 1,000 meters of elevation gain (or roughly 2°C per 1,000 feet). For example, if we climb a mountain 2,000 feet higher up, we can generally expect the temperature to be around 7°F cooler at the top than at the base.) Of course, while 3.5°F per 1,000 feet is the standard average, real-world conditions frequently break this rule.Let’s start with humidity and moisture. If the air is dry, it cools faster as it rises, at a rate that’s about 5.4°F per 1,000 feet (9.8°C per 1,000 meters). If, on the other hand, the air cools to its dew point and moisture condenses into clouds or fog, latent heat is released into the surrounding air. This slows the cooling rate down to roughly 3.0°F per 1,000 feet (5°C per 1,000 meters).
Then we’ve got the temperature inversions, in which if temperature always decreases with height, during an inversion, the opposite happens as warmer air sits over a pool of cold air. This is very common in mountain valleys (Salt Lake City) during winter or clear, windless nights, where cold heavy air sinks into the valley floor while Park City’s higher elevation stays significantly warmer.
Finally the terrain topography and wind also influence the system. Dark rock faces and exposed alpine terrain can heat up significantly under direct sunlight, creating warm microclimates high up that defy the surrounding free-air lapse rate. Conversely, strong alpine winds can pull down cold air masses (these are called katabatic winds) or enhance wind chill, making it feel far colder than the ambient lapse rate suggests.
Now you know all the details about the whole altitude and temperature relationship!







