ClimateSearch

Zhaotong, Yunnan

China · 788k people · 1970 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 high48°F (9°C)54°F (12°C)61°F (16°C)67°F (19°C)70°F (21°C)71°F (22°C)74°F (23°C)73°F (23°C)68°F (20°C)60°F (16°C)56°F (13°C)49°F (9°C)
Average low29°F (-2°C)32°F (0°C)39°F (4°C)47°F (8°C)53°F (12°C)58°F (15°C)60°F (16°C)60°F (15°C)55°F (13°C)48°F (9°C)40°F (5°C)31°F (0°C)
Dew point28°F (-2°C)30°F (-1°C)37°F (3°C)44°F (7°C)51°F (10°C)58°F (14°C)61°F (16°C)60°F (15°C)55°F (13°C)48°F (9°C)40°F (5°C)32°F (0°C)
Rainfall0.6 in (16 mm)0.6 in (16 mm)1.2 in (31 mm)1.8 in (47 mm)3.5 in (89 mm)6.4 in (162 mm)8.1 in (205 mm)7.2 in (183 mm)4.9 in (124 mm)3.1 in (80 mm)1.2 in (30 mm)0.6 in (15 mm)
Rainy days4581217222221191884
Snowfall4.6 in (11.7 cm)3.5 in (9 cm)2.3 in (5.9 cm)0.2 in (0.4 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)1.1 in (2.8 cm)3.7 in (9.3 cm)
Sunshine256 h246 h266 h245 h236 h208 h261 h260 h201 h145 h186 h214 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 +1.7°F (+0.9°C) to +2.3°F (+1.3°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +2.7°F (+1.5°C)
  • February: +1.7°F (+1.0°C)
  • March: +1.3°F (+0.7°C)
  • April: +3.0°F (+1.7°C)
  • May: +2.8°F (+1.6°C)
  • June: +2.4°F (+1.3°C)
  • July: +1.7°F (+1.0°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.6°F (+1.4°C)
  • October: +2.6°F (+1.4°C)
  • November: +1.9°F (+1.1°C)
  • December: +2.7°F (+1.5°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.