ClimateSearch

Lüliang, Shanxi

China · 3.3M people · 944 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 high33°F (1°C)41°F (5°C)52°F (11°C)66°F (19°C)76°F (24°C)83°F (29°C)85°F (30°C)82°F (28°C)73°F (23°C)61°F (16°C)47°F (9°C)35°F (2°C)
Average low16°F (-9°C)23°F (-5°C)31°F (0°C)42°F (6°C)53°F (12°C)62°F (17°C)67°F (19°C)64°F (18°C)55°F (13°C)43°F (6°C)31°F (-1°C)20°F (-7°C)
Dew point4°F (-16°C)10°F (-12°C)19°F (-7°C)29°F (-2°C)38°F (4°C)50°F (10°C)61°F (16°C)60°F (16°C)51°F (10°C)37°F (3°C)22°F (-5°C)7°F (-14°C)
Rainfall0.2 in (6 mm)0.4 in (11 mm)0.8 in (21 mm)1.4 in (36 mm)1.7 in (43 mm)2.5 in (62 mm)4.6 in (117 mm)4.7 in (120 mm)3 in (77 mm)1.9 in (48 mm)0.8 in (22 mm)0.2 in (6 mm)
Rainy days23566913129742
Snowfall1.8 in (4.6 cm)2.6 in (6.7 cm)3.1 in (7.9 cm)0.9 in (2.4 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.2 in (0.5 cm)2.3 in (5.8 cm)1.7 in (4.4 cm)
Sunshine262 h249 h291 h308 h324 h328 h332 h310 h261 h260 h236 h251 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

+2.5°F (+1.4°C)

Models range from +1.2°F (+0.6°C) to +3.6°F (+2.0°C)

Days above 90°F (32°C) a year

13 22

About 1.6× as many

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.6°F (+0.9°C)
  • April: +2.6°F (+1.5°C)
  • May: +1.6°F (+0.9°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.5°F (+1.4°C)
  • August: +2.9°F (+1.6°C)
  • September: +3.7°F (+2.1°C)
  • October: +2.0°F (+1.1°C)
  • November: +2.1°F (+1.1°C)
  • December: +2.8°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.