ClimateSearch

Circoiscrizione II, Piedmont

Italy · 141k people · 258 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 high43°F (6°C)46°F (8°C)55°F (13°C)61°F (16°C)68°F (20°C)76°F (24°C)81°F (27°C)80°F (27°C)71°F (22°C)61°F (16°C)51°F (11°C)44°F (7°C)
Average low28°F (-2°C)29°F (-1°C)36°F (2°C)43°F (6°C)51°F (11°C)58°F (15°C)62°F (17°C)62°F (17°C)56°F (13°C)48°F (9°C)38°F (3°C)30°F (-1°C)
Dew point27°F (-3°C)29°F (-2°C)35°F (2°C)42°F (6°C)50°F (10°C)57°F (14°C)59°F (15°C)59°F (15°C)53°F (12°C)47°F (9°C)38°F (3°C)29°F (-2°C)
Rainfall2 in (51 mm)2.2 in (57 mm)2.7 in (69 mm)3.9 in (100 mm)4.5 in (115 mm)3.4 in (87 mm)2 in (51 mm)2.5 in (62 mm)3.6 in (91 mm)3.7 in (93 mm)4.7 in (121 mm)2.3 in (58 mm)
Rainy days77811131081091097
Snowfall5.3 in (13.5 cm)5 in (12.8 cm)2.2 in (5.6 cm)0.2 in (0.5 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0.1 cm)1 in (2.6 cm)4.2 in (10.6 cm)
Sunshine210 h217 h274 h289 h336 h375 h410 h360 h282 h209 h178 h195 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

+3.1°F (+1.7°C)

Models range from +2.5°F (+1.4°C) to +3.5°F (+1.9°C)

Days above 90°F (32°C) a year

4 8

About 2.2× as many

Warming by month
  • January: +2.3°F (+1.3°C)
  • February: +1.2°F (+0.6°C)
  • March: +2.0°F (+1.1°C)
  • April: +1.5°F (+0.9°C)
  • May: +2.9°F (+1.6°C)
  • June: +2.6°F (+1.4°C)
  • July: +3.0°F (+1.7°C)
  • August: +3.7°F (+2.1°C)
  • September: +3.2°F (+1.8°C)
  • October: +1.8°F (+1.0°C)
  • November: +1.9°F (+1.1°C)
  • December: +2.3°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.