ClimateSearch

Suining, Sichuan

China · 657k people · 294 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 high49°F (10°C)55°F (13°C)64°F (18°C)74°F (23°C)81°F (27°C)84°F (29°C)90°F (32°C)90°F (32°C)80°F (27°C)70°F (21°C)62°F (17°C)52°F (11°C)
Average low40°F (5°C)44°F (7°C)50°F (10°C)59°F (15°C)65°F (19°C)71°F (22°C)76°F (24°C)75°F (24°C)69°F (20°C)60°F (16°C)52°F (11°C)43°F (6°C)
Dew point37°F (3°C)41°F (5°C)47°F (8°C)55°F (13°C)61°F (16°C)69°F (20°C)74°F (23°C)72°F (22°C)66°F (19°C)57°F (14°C)49°F (9°C)40°F (4°C)
Rainfall0.5 in (12 mm)0.5 in (14 mm)1.1 in (27 mm)2.5 in (63 mm)4.1 in (103 mm)6.7 in (169 mm)8.4 in (215 mm)6.8 in (173 mm)5.2 in (133 mm)2.9 in (73 mm)1.1 in (28 mm)0.5 in (12 mm)
Rainy days3368991211101063
Snowfall0.2 in (0.5 cm)0.1 in (0.2 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.2 in (0.4 cm)
Sunshine79 h70 h91 h112 h123 h123 h152 h160 h98 h63 h68 h69 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 (+1.3°C)

Models range from +1.2°F (+0.7°C) to +3.0°F (+1.7°C)

Days above 90°F (32°C) a year

33 → 64

About 1.9× as many

Warming by month
  • January: +2.9°F (+1.6°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.7°F (+0.9°C)
  • April: +2.3°F (+1.3°C)
  • May: +1.8°F (+1.0°C)
  • June: +3.1°F (+1.7°C)
  • July: +1.8°F (+1.0°C)
  • August: +2.2°F (+1.2°C)
  • September: +3.4°F (+1.9°C)
  • October: +2.2°F (+1.2°C)
  • November: +2.3°F (+1.3°C)
  • December: +3.1°F (+1.7°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.