because the south-facing sides receives more sunlight than the north-facing sides.
because the south-facing sides receives more sunlight than the north-facing sides.
because the south-facing sides receives more sunlight than the north-facing sides.
South-facing mountain slopes receive more direct sunlight and warmth, creating a drier and warmer microclimate compared to north-facing slopes. This results in faster snowmelt and higher temperatures, which can support different plant and animal species adapted to these conditions.
Warmer and drier (relatively).
South-facing mountain slopes in the northern hemisphere receive more direct sunlight, which leads to warmer temperatures compared to north-facing slopes. This exposure to sunlight creates a microclimate that is typically drier and warmer, promoting different vegetation and wildlife compared to the surrounding areas.
Much warmer and drier.
cooler and receive less direct sunlight than north-facing slopes. This can lead to differences in temperature, humidity, and vegetation between the two slopes, creating a unique microclimate.
leaves
dry and warmer
Africa is warmer and wetter near the equator and drier north and south.
South-facing mountains in the Northern Hemisphere receive more direct sunlight, leading to warmer temperatures compared to the north-facing slopes. This exposure to sunlight creates a microclimate that is typically drier and sunnier, allowing for different vegetation to thrive and supporting unique ecosystems.
On the leeward side of a mountain, air descends and warms due to compression, leading to warmer temperatures. Additionally, as the air descends, it loses much of its moisture through precipitation on the windward side, resulting in drier conditions on the leeward side.