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 high41°F (5°C)41°F (5°C)44°F (7°C)51°F (10°C)58°F (15°C)63°F (17°C)67°F (19°C)67°F (19°C)61°F (16°C)53°F (12°C)47°F (8°C)43°F (6°C)
Average low33°F (0°C)31°F (0°C)33°F (1°C)38°F (3°C)44°F (7°C)49°F (9°C)53°F (12°C)54°F (12°C)50°F (10°C)44°F (6°C)38°F (4°C)34°F (1°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)
Rainfall4.9 in (124 mm)4.2 in (108 mm)3.4 in (86 mm)2.6 in (65 mm)2.7 in (69 mm)3.2 in (81 mm)4.1 in (103 mm)5.5 in (139 mm)5.6 in (141 mm)6.5 in (164 mm)5.8 in (148 mm)5.7 in (144 mm)
Rainy days161414111112131415171717
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)
Sunshine41 h66 h116 h178 h247 h221 h217 h191 h130 h91 h49 h32 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.