ClimateSearch

Innsbruck, Tyrol

Austria · 132k people · 580 m elevation · Northern Hemisphere

Every month in detail

Thirty-year averages for each calendar month.

Monthly climate normals. Values shown as an em dash are missing from the source data.
MonthJanFebMarAprMayJunJulAugSepOctNovDec
Average high42°F (6°C)46°F (8°C)55°F (13°C)63°F (17°C)71°F (22°C)76°F (25°C)78°F (26°C)77°F (25°C)69°F (21°C)61°F (16°C)50°F (10°C)43°F (6°C)
Average low26°F (-3°C)28°F (-2°C)34°F (1°C)41°F (5°C)50°F (10°C)56°F (14°C)58°F (15°C)58°F (15°C)51°F (11°C)44°F (7°C)37°F (3°C)29°F (-2°C)
Dew point24°F (-4°C)26°F (-3°C)33°F (1°C)39°F (4°C)48°F (9°C)56°F (13°C)59°F (15°C)59°F (15°C)53°F (12°C)45°F (7°C)35°F (2°C)26°F (-3°C)
Rainfall1.8 in (47 mm)1.8 in (45 mm)2.4 in (61 mm)2.4 in (62 mm)4.3 in (109 mm)4.8 in (123 mm)5.5 in (140 mm)5.3 in (136 mm)3.4 in (87 mm)3 in (75 mm)2.7 in (69 mm)2.3 in (58 mm)
Rainy days9912121716161412111111
Snowfall22 in (56 cm)21 in (53.4 cm)25.4 in (64.6 cm)20.5 in (52.1 cm)9.3 in (23.6 cm)2.8 in (7.2 cm)0.9 in (2.2 cm)1 in (2.6 cm)4.5 in (11.5 cm)12 in (30.5 cm)21 in (53.3 cm)23.3 in (59.1 cm)
Sunshine121 h122 h163 h180 h175 h180 h208 h187 h151 h135 h103 h102 h

Scroll the table sideways for all twelve months.

Projected change, 2031–2050

Model projection, not an observation

How this city’s climate may change, measured against the same models’ own 1995–2014 output. Nothing here affects the match score above.

Change in summer afternoon highs

+2.5°F (+1.4°C)

Models range from +1.2°F (+0.7°C) to +3.2°F (+1.8°C)

Days above 90°F (32°C) a year

—

Too few hot days today to project a reliable change

Warming by month
  • January: +2.6°F (+1.4°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.5°F (+0.9°C)
  • April: +1.9°F (+1.0°C)
  • May: +2.6°F (+1.5°C)
  • June: +1.7°F (+0.9°C)
  • July: +2.5°F (+1.4°C)
  • August: +3.3°F (+1.8°C)
  • September: +3.3°F (+1.8°C)
  • October: +2.0°F (+1.1°C)
  • November: +2.3°F (+1.3°C)
  • December: +2.8°F (+1.6°C)
Scenario
SSP5-8.5 (high emissions)
Models
4 · CMIP6 HighResMIP, downscaled

This is a high-emissions pathway — the upper end of plausible futures, not a central estimate. Changes are measured by each model against its own past output and then applied to the observed record, which cancels each model’s bias but not the genuine uncertainty about how much warming occurs. Where the models disagree widely, the range above is the honest answer.