ClimateSearch

Shangri-La, Yunnan

China · 186k people · 3282 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 high37°F (3°C)38°F (3°C)44°F (7°C)52°F (11°C)59°F (15°C)64°F (18°C)64°F (18°C)64°F (18°C)61°F (16°C)55°F (13°C)48°F (9°C)42°F (6°C)
Average low19°F (-7°C)21°F (-6°C)28°F (-2°C)35°F (2°C)43°F (6°C)50°F (10°C)52°F (11°C)51°F (11°C)49°F (9°C)41°F (5°C)32°F (0°C)25°F (-4°C)
Dew point19°F (-7°C)23°F (-5°C)29°F (-2°C)36°F (2°C)43°F (6°C)50°F (10°C)53°F (11°C)52°F (11°C)49°F (9°C)40°F (5°C)30°F (-1°C)22°F (-5°C)
Rainfall1.3 in (33 mm)1.7 in (43 mm)2.5 in (65 mm)2.6 in (65 mm)3.9 in (100 mm)5.6 in (143 mm)9.5 in (241 mm)9 in (228 mm)5.6 in (143 mm)2.6 in (66 mm)0.9 in (23 mm)0.5 in (13 mm)
Rainy days68121417232928231253
Snowfall10.4 in (26.4 cm)13.1 in (33.2 cm)16.4 in (41.7 cm)7.2 in (18.2 cm)2.1 in (5.3 cm)0 in (0 cm)0.1 in (0.2 cm)0 in (0 cm)0.6 in (1.6 cm)1.7 in (4.3 cm)3.2 in (8.2 cm)3.8 in (9.7 cm)
Sunshine298 h282 h313 h314 h320 h276 h225 h249 h251 h280 h282 h295 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

+2.0°F (+1.1°C)

Models range from +1.5°F (+0.8°C) to +2.3°F (+1.3°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +3.5°F (+2.0°C)
  • February: +2.9°F (+1.6°C)
  • March: +2.7°F (+1.5°C)
  • April: +3.0°F (+1.7°C)
  • May: +2.3°F (+1.3°C)
  • June: +2.2°F (+1.2°C)
  • July: +1.6°F (+0.9°C)
  • August: +2.3°F (+1.3°C)
  • September: +2.2°F (+1.2°C)
  • October: +2.4°F (+1.3°C)
  • November: +2.4°F (+1.4°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.