ClimateSearch

Stavanger, Rogaland

Norway · 152k people · 15 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 high39°F (4°C)38°F (4°C)41°F (5°C)47°F (8°C)53°F (12°C)58°F (14°C)62°F (17°C)63°F (17°C)58°F (15°C)51°F (11°C)45°F (7°C)40°F (5°C)
Average low34°F (1°C)32°F (0°C)34°F (1°C)38°F (4°C)44°F (7°C)49°F (10°C)54°F (12°C)55°F (13°C)51°F (11°C)45°F (7°C)39°F (4°C)35°F (2°C)
Dew point31°F (0°C)30°F (-1°C)32°F (0°C)36°F (2°C)42°F (5°C)47°F (9°C)52°F (11°C)53°F (12°C)49°F (9°C)42°F (6°C)37°F (3°C)33°F (1°C)
Rainfall7.2 in (184 mm)5.7 in (144 mm)4.8 in (121 mm)3.3 in (84 mm)3.2 in (82 mm)3.4 in (87 mm)4.3 in (110 mm)6.4 in (162 mm)7.4 in (188 mm)8.7 in (220 mm)8 in (204 mm)7.6 in (194 mm)
Rainy days191616141313151717191919
Snowfall8 in (20.2 cm)8 in (20.2 cm)6 in (15.2 cm)1.3 in (3.3 cm)0.1 in (0.2 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.3 in (0.7 cm)1.4 in (3.6 cm)5 in (12.7 cm)
Sunshine86 h131 h214 h298 h383 h377 h377 h333 h237 h172 h100 h66 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

+1.6°F (+0.9°C)

Models range from +1.3°F (+0.7°C) to +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +1.9°F (+1.1°C)
  • February: +0.7°F (+0.4°C)
  • March: +1.0°F (+0.5°C)
  • April: +1.2°F (+0.7°C)
  • May: +1.5°F (+0.8°C)
  • June: +1.5°F (+0.8°C)
  • July: +1.8°F (+1.0°C)
  • August: +1.6°F (+0.9°C)
  • September: +1.9°F (+1.1°C)
  • October: +1.5°F (+0.9°C)
  • November: +1.8°F (+1.0°C)
  • December: +1.5°F (+0.8°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.