ClimateSearch

Bishan, Chongqing

China · 205k people · 288 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 high51°F (11°C)56°F (14°C)64°F (18°C)73°F (23°C)79°F (26°C)83°F (29°C)89°F (32°C)90°F (32°C)82°F (28°C)71°F (22°C)63°F (17°C)54°F (12°C)
Average low42°F (5°C)45°F (7°C)51°F (11°C)59°F (15°C)65°F (18°C)71°F (22°C)76°F (25°C)76°F (25°C)70°F (21°C)61°F (16°C)53°F (12°C)44°F (7°C)
Dew point39°F (4°C)42°F (6°C)49°F (9°C)57°F (14°C)64°F (18°C)70°F (21°C)74°F (24°C)73°F (23°C)67°F (19°C)59°F (15°C)51°F (11°C)42°F (6°C)
Rainfall1 in (26 mm)1.1 in (29 mm)2.6 in (66 mm)4.2 in (107 mm)5.7 in (144 mm)6.6 in (167 mm)6.8 in (172 mm)6 in (152 mm)4.4 in (112 mm)3.8 in (96 mm)2.5 in (63 mm)1.3 in (34 mm)
Rainy days881315161615141316119
Snowfall0.2 in (0.4 cm)0 in (0.1 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)0.1 in (0.3 cm)
Sunshine125 h127 h165 h202 h227 h232 h293 h282 h202 h133 h126 h120 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

+2.1°F (+1.2°C)

Models range from +1.3°F (+0.7°C) to +2.5°F (+1.4°C)

Days above 90°F (32°C) a year

40 66

About 1.7× as many

Warming by month
  • January: +2.9°F (+1.6°C)
  • February: +1.9°F (+1.1°C)
  • March: +1.5°F (+0.8°C)
  • April: +2.4°F (+1.4°C)
  • May: +1.8°F (+1.0°C)
  • June: +2.3°F (+1.3°C)
  • July: +1.7°F (+0.9°C)
  • August: +2.2°F (+1.2°C)
  • September: +3.3°F (+1.8°C)
  • October: +2.4°F (+1.4°C)
  • November: +2.3°F (+1.3°C)
  • December: +3.0°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.