Sun-facing mountain slopes often run warmer and drier than shaded aspects
In mid and high latitudes, equator-facing slopes receive stronger sunlight than pole-facing ones a few hundred meters away. Snow melts earlier; soils dry faster; plant communities shift toward drought-tolerant species.
Hikers notice grass on one side of a ridge and deep forest or lingering snowpack on the other — a microclimate split written in aspect, not altitude alone.
A mountain is a mosaic of climates. Aspect decides whether a slope lives in a warmer, drier neighborhood than its shaded twin.
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