ClimateSearch

Linxia Chengguanzhen, Gansu

China · 274k people · 1891 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 high32°F (0°C)37°F (3°C)48°F (9°C)60°F (16°C)67°F (20°C)73°F (23°C)77°F (25°C)74°F (24°C)66°F (19°C)56°F (13°C)45°F (7°C)35°F (2°C)
Average low11°F (-11°C)15°F (-9°C)24°F (-4°C)34°F (1°C)43°F (6°C)51°F (11°C)56°F (13°C)56°F (13°C)49°F (9°C)38°F (3°C)26°F (-3°C)16°F (-9°C)
Dew point6°F (-15°C)11°F (-12°C)19°F (-7°C)28°F (-2°C)38°F (4°C)47°F (9°C)53°F (12°C)54°F (12°C)48°F (9°C)37°F (3°C)22°F (-5°C)9°F (-13°C)
Rainfall0.3 in (7 mm)0.5 in (12 mm)0.9 in (22 mm)1.3 in (34 mm)2.6 in (65 mm)3 in (75 mm)4.3 in (109 mm)5.1 in (130 mm)4.2 in (106 mm)2.5 in (65 mm)0.6 in (15 mm)0.2 in (4 mm)
Rainy days345711111415151341
Snowfall2.8 in (7 cm)3.9 in (9.9 cm)5.2 in (13.1 cm)3 in (7.6 cm)1.2 in (3 cm)0.1 in (0.2 cm)0 in (0 cm)0 in (0 cm)0.4 in (0.9 cm)3.3 in (8.5 cm)3.3 in (8.4 cm)1.7 in (4.3 cm)
Sunshine272 h268 h304 h305 h319 h316 h323 h298 h237 h246 h262 h274 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

+2.6°F (+1.5°C)

Models range from +1.8°F (+1.0°C) to +3.9°F (+2.2°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +2.1°F (+1.2°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.9°F (+1.1°C)
  • April: +2.4°F (+1.4°C)
  • May: +1.4°F (+0.8°C)
  • June: +2.4°F (+1.4°C)
  • July: +2.1°F (+1.2°C)
  • August: +3.3°F (+1.9°C)
  • September: +3.1°F (+1.7°C)
  • October: +1.6°F (+0.9°C)
  • November: +2.1°F (+1.2°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.