The Marine West Coast Climate (Cfb), according to Koeppen’s climate classification, is a type of humid climate identified by its moderate temperatures and consistent precipitation. This climate is prevalent in regions situated poleward from Mediterranean climates, predominantly along the western coasts of continents. Characterized by mild summers with average temperatures ranging from 15° to 20°C and cool winters with temperatures between 4° and 10°C, this climate shows minimal temperature variation both annually and daily. Precipitation is abundant, varying from 50 to 250 cm yearly, allowing lush vegetation such as temperate rainforests to thrive. The consistent moisture is due to prevailing westerly winds transporting oceanic influences, resulting in a climate favorable to diverse ecosystems and agriculture. Understanding Cfb is crucial as it provides insight into local weather patterns and their implications for natural resources and human activity.