ClimateSearch

Västerås, Västmanland

Sweden · 128k people · 10 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 high31°F (0°C)33°F (0°C)40°F (4°C)51°F (10°C)61°F (16°C)67°F (20°C)72°F (22°C)69°F (21°C)60°F (16°C)48°F (9°C)39°F (4°C)34°F (1°C)
Average low23°F (-5°C)23°F (-5°C)27°F (-3°C)35°F (1°C)43°F (6°C)52°F (11°C)57°F (14°C)55°F (13°C)48°F (9°C)40°F (4°C)33°F (0°C)26°F (-3°C)
Dew point24°F (-5°C)23°F (-5°C)26°F (-3°C)32°F (0°C)40°F (4°C)48°F (9°C)54°F (12°C)53°F (12°C)47°F (9°C)39°F (4°C)33°F (1°C)27°F (-3°C)
Rainfall1.5 in (38 mm)1.2 in (31 mm)1.2 in (31 mm)1.4 in (37 mm)1.9 in (49 mm)2.7 in (69 mm)2.9 in (74 mm)2.9 in (73 mm)2.1 in (53 mm)2.1 in (54 mm)1.9 in (48 mm)1.8 in (46 mm)
Rainy days9888101112129101010
Snowfall6.8 in (17.3 cm)6 in (15.3 cm)4.6 in (11.7 cm)2 in (5 cm)0.3 in (0.8 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.5 in (1.2 cm)3.4 in (8.7 cm)6.9 in (17.6 cm)
Sunshine80 h123 h214 h297 h377 h395 h396 h344 h239 h148 h71 h60 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

+2.4°F (+1.4°C)

Models range from +1.9°F (+1.1°C) to +3.0°F (+1.6°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +3.1°F (+1.7°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.6°F (+1.4°C)
  • May: +2.5°F (+1.4°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.7°F (+1.5°C)
  • August: +2.6°F (+1.4°C)
  • September: +3.0°F (+1.6°C)
  • October: +2.1°F (+1.2°C)
  • November: +3.2°F (+1.8°C)
  • December: +2.4°F (+1.3°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.