ClimateSearch

Grenoble, Rhône-Alpes

France · 159k people · 216 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 high45°F (7°C)47°F (8°C)54°F (12°C)61°F (16°C)68°F (20°C)75°F (24°C)80°F (26°C)80°F (26°C)71°F (22°C)64°F (18°C)53°F (12°C)46°F (8°C)
Average low31°F (0°C)32°F (0°C)38°F (3°C)43°F (6°C)51°F (10°C)58°F (15°C)62°F (17°C)62°F (17°C)55°F (13°C)48°F (9°C)39°F (4°C)33°F (0°C)
Dew point31°F (0°C)32°F (0°C)38°F (4°C)44°F (7°C)52°F (11°C)58°F (15°C)61°F (16°C)61°F (16°C)56°F (13°C)50°F (10°C)40°F (5°C)33°F (1°C)
Rainfall4.6 in (117 mm)3.9 in (100 mm)4.2 in (107 mm)4.7 in (120 mm)5.7 in (145 mm)4.9 in (125 mm)4.4 in (112 mm)4.3 in (108 mm)4.3 in (108 mm)4.6 in (118 mm)5.6 in (143 mm)5.1 in (130 mm)
Rainy days131113141715131212131413
Snowfall16.4 in (41.7 cm)14.5 in (36.8 cm)10.7 in (27.2 cm)8.8 in (22.4 cm)2.3 in (5.8 cm)0.2 in (0.4 cm)0 in (0.1 cm)0 in (0 cm)0.3 in (0.8 cm)2.4 in (6.1 cm)11.3 in (28.6 cm)15.2 in (38.7 cm)
Sunshine182 h206 h273 h298 h337 h363 h394 h360 h288 h243 h183 h171 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

+3.2°F (+1.8°C)

Models range from +2.3°F (+1.3°C) to +3.7°F (+2.0°C)

Days above 90°F (32°C) a year

7 16

About 2.3× as many

Warming by month
  • January: +2.5°F (+1.4°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.6°F (+0.9°C)
  • April: +1.4°F (+0.8°C)
  • May: +2.8°F (+1.6°C)
  • June: +2.0°F (+1.1°C)
  • July: +3.3°F (+1.8°C)
  • August: +4.3°F (+2.4°C)
  • September: +3.6°F (+2.0°C)
  • October: +2.3°F (+1.3°C)
  • November: +2.2°F (+1.2°C)
  • December: +2.9°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.