Travel time: Year-round
Munich’s weather is a dynamic tapestry woven from its high-altitude position (519 meters above sea level) and its proximity to the northern edge of the Alps. This location creates a "slightly continental" climate that is both unpredictable and full of character, where clear mountain air and sudden atmospheric shifts are the norm.
The most distinct feature of Munich’s climate is the Föhn, a warm, dry mountain wind that descends from the Alps. It can occur at any time but is most prevalent in autumn and spring.
Spring is a season of awakening and volatility. In March, frost still grips the mornings, and snow can occasionally fall. By May, the city undergoes a green explosion.
Summers are warm and pleasant rather than scorching, though heatwaves (reaching 30°C+) are becoming more frequent.
This is perhaps Munich's most stable weather period. September often enjoys an "Altweibersommer" (Indian Summer), with mild, golden days.
Munich is frequently the coldest major city in Germany due to its elevation and exposure to cold air masses from the East (Siberia).
Munich's urban sprawl creates a noticeable heat island effect—the city center (Marienplatz) is often 2°C to 3°C warmer than the wooded periphery or the English Garden. To the north (near the airport), the terrain is flatter and more prone to persistent autumn fog, whereas the southern districts closer to the Isar River and the mountains often catch the first rays of the Föhn.
Munich residents have a pragmatic relationship with their weather. They are "weather-active," meaning they utilize every window of sunshine immediately. If the sun comes out in February, the outdoor chairs at cafes are instantly filled. Conversely, they are rarely deterred by rain; the phrase "There is no such thing as bad weather, only bad clothing" is a local mantra. Locals also monitor the "Alpensicht" (Alps visibility) as a primary indicator of upcoming weather changes.