Pasadena Weather Guide: Seasons, Winds & Microclimates

Travel time: Year-round

Pasadena sits in a unique geographic bowl at the base of the San Gabriel Mountains, creating a Mediterranean climate that is distinct from the neighboring coastal regions of Los Angeles. While only 40 miles from the Pacific Ocean, its inland position and mountain backdrop lead to hotter summers, cooler winters, and higher rainfall than the coast.

The Daily Cycle

Pasadena’s weather follows a predictable diurnal rhythm. Mornings often begin with a crispness, especially in the spring and early summer when the marine layer—a thick blanket of low clouds and fog—reaches inland from the coast. Locals refer to this as "Gray May" or "June Gloom." By mid-morning, the sun typically "burns off" the fog, leading to clear, bright afternoons.

Because of the dry air, temperatures can swing by more than 30°F (17°C) in a single day. Even on a hot 90°F summer day, the evening usually cools down rapidly once the sun dips behind the mountains, providing a natural nocturnal cooling effect that residents rely on.

Seasonal Trends

  • Summer (June – September): Summers are hot, arid, and nearly rainless. August and September are the warmest months, with average highs in the late 80s or low 90s, though heat waves exceeding 100°F (38°C) are common. The heat is typically "dry," making it feel less oppressive than humid climates, though the UV index is consistently high.
  • Autumn (October – November): This is a season of transition. While mornings stay cool, the arrival of the Santa Ana winds can cause sudden, sharp spikes in temperature and extreme drops in humidity. This is the peak time for brilliant blue skies and exceptional visibility.
  • Winter (December – February): Winters are mild but represent the region's rainy season. Most of Pasadena's ~20 inches of annual rain falls during these months, often in short, intense bursts caused by Pacific storms. Daytime highs remain comfortable (60s°F), but night temperatures can occasionally dip into the 40s°F.
  • Spring (March – May): Spring is characterized by blooming gardens and the return of the marine layer. It is a temperate season where the landscape turns vibrant green before the summer aridity sets in.

Local Weather Phenomena

Santa Ana Winds

Known as the "Devil Winds," these hot, dry offshore winds blow from the high desert toward the coast. When they hit the San Gabriel Mountains, they compress and accelerate through canyons, reaching Pasadena as powerful, dehydrating gusts. Beyond the fire risk they pose, they create a "nerves jump" feeling—a physical sensation of restlessness caused by the rapid drop in humidity and high wind speeds.

Orographic Lift

The San Gabriel Mountains act as a physical barrier. As moist air from the Pacific is forced up the mountain slopes, it cools and condenses, leading to significantly higher rainfall in Pasadena than in the flatter basins to the south. In winter, travelers may see snow-capped peaks at Mount Wilson while the city streets below remain bathed in sunshine.

Microclimates

Pasadena’s topography creates noticeable temperature variations within the city. The Upper Hastings Ranch and Altadena border areas, positioned higher against the foothills, often experience stronger winds and slightly cooler nighttime temperatures than the lower-lying Old Pasadena or South Pasadena areas. Canyons like the Arroyo Seco can trap cool air at night, creating localized pockets of chill even during warmer weeks.

Historical Context

Historically, Pasadena was marketed as a health resort in the late 19th century because of its "pure air" and Mediterranean climate. While much of Southern California is semi-arid, Pasadena’s proximity to mountain runoff and its status as a "floral heritage" city means it feels more lush and shaded than the surrounding urban sprawl. While snow is an extreme rarity (the last major event was in 1949), the city has witnessed record highs of 115°F, underscoring the intensity of the inland heat.