Detailed Explanation:

Answer: Option 4 — Marine West coast climate

The Marine West Coast climate (Cfb in Köppen classification) is characterized by low annual and daily temperature ranges due to oceanic moderation, year-round precipitation brought by prevailing westerly winds, and precipitation totals typically ranging from 50-250 cm. This climate is found on western coasts of continents between 40°-60° latitude, such as the Pacific Northwest of North America and Western Europe.

📝 Short Notes: Marine West Coast Climate

• Location: Found on western coasts of continents between 40°-60° latitude (e.g., Pacific Northwest USA, British Columbia, Western Europe, Southern Chile, Southeast Australia, New Zealand)
• Temperature Characteristics: Mild winters (above 0°C) and cool summers (below 22°C); narrow annual temperature range due to maritime influence; typically no month averages below -3°C
• Precipitation Pattern: Year-round rainfall with slight winter maximum; brought by mid-latitude cyclones and orographic lifting; ranges from 50-250 cm annually depending on topography
• Atmospheric Controls: Dominated by prevailing westerlies that carry moist oceanic air; frequent passage of frontal systems and cyclonic storms; maritime air masses moderate temperature extremes
• Vegetation: Dense evergreen and deciduous forests; includes temperate rainforests in areas with higher precipitation; characteristic species include Douglas fir, redwood, spruce, and beech
• Distinguishing Features: Cloudy, foggy conditions common; low sunshine hours; high relative humidity; minimal temperature extremes compared to continental interiors at similar latitudes
• Contrast with Other Climates: Unlike Mediterranean climate (dry summers), Marine West Coast has year-round precipitation; unlike Humid Subtropical (hot summers), it has cool summers; unlike Equatorial (high temperatures year-round), it has distinct seasonal temperature variation though mild