mountain climate
Elevated terrain conditions
Mountain climate is the weather pattern typical of high-elevation regions, characterized by cooler temperatures, thinner air, increased precipitation, and rapid weather changes.
Temperature drops predictably with altitude—roughly 3.5°F per thousand feet.
Mountain climates create distinct vegetation zones and can vary dramatically between a peak's sunny and shaded slopes.
- microclimatesLocalized atmospheric conditions
- morning frostIce crystals at dawn
- altitudeMeasured height above reference
- topographyPhysical feature mapping
- frost lineSoil's frozen zone limit
wind chill · air pressure · acclimatization · treeline · snow line · alpine meadows · snowpack · glacier retreat · rain shadow · cloud formation · slopes · peaks · high altitude · thin air · valleys · plateaus · rocky terrain · crisp
- climateweather, global warming, temperature, greenhouse effect, greenhouse gas
- climatestropical, subtropical, temperate forest, equatorial, continental
- mountainspeaks, peak, summit, summits, Alps
- cold climatestundra, taiga, boreal forest, alpine zone, permafrost
- desert climatearid, aridity, dry heat, extreme heat, scorching heat
- national parksYellowstone, Yosemite, Grand Canyon, Everglades, Glacier National Park
mountain climatecoastal climate
Weather moderated by ocean proximity
island climate · desert climate · Mediterranean climate · tropical climate