Kustklimaten

Kustklimaten, often translated as maritime or oceanic climate, describes weather patterns influenced by proximity to large bodies of water, typically oceans. These climates are characterized by moderate temperatures, with less extreme variations between summer and winter compared to continental climates. The presence of water acts as a thermal regulator, absorbing heat during warmer months and releasing it during colder periods.

Precipitation in kustklimaten tends to be more evenly distributed throughout the year, though specific patterns can vary based on prevailing wind directions and ocean currents. Coastal areas often experience higher humidity levels due to evaporation from the water surface. Fog and cloud cover are also common, particularly during certain seasons, as moist air encounters cooler landmasses or temperature gradients.

The geographical distribution of kustklimaten is widespread, occurring along the coastlines of continents. Examples include Western Europe, the Pacific Northwest of North America, and parts of New Zealand. The specific characteristics of a kustklimat can be further modified by factors such as latitude, prevailing winds, and the presence of nearby mountain ranges. These climates generally support rich biodiversity, with ecosystems adapted to the consistent moisture and milder temperature ranges.