ClimateSearch

Daxing, Beijing

China · 105k people · 40 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 high36°F (2°C)43°F (6°C)56°F (13°C)71°F (22°C)82°F (28°C)89°F (32°C)89°F (32°C)86°F (30°C)80°F (26°C)67°F (19°C)50°F (10°C)38°F (3°C)
Average low19°F (-7°C)23°F (-5°C)32°F (0°C)45°F (7°C)58°F (14°C)67°F (20°C)72°F (22°C)70°F (21°C)60°F (16°C)46°F (8°C)31°F (-1°C)21°F (-6°C)
Dew point4°F (-15°C)10°F (-12°C)19°F (-7°C)29°F (-1°C)42°F (6°C)57°F (14°C)68°F (20°C)67°F (20°C)55°F (13°C)38°F (4°C)22°F (-5°C)9°F (-13°C)
Rainfall0.1 in (3 mm)0.2 in (5 mm)0.4 in (9 mm)0.8 in (20 mm)1.4 in (36 mm)2.8 in (70 mm)6.1 in (154 mm)4.8 in (121 mm)2.1 in (55 mm)1.3 in (33 mm)0.6 in (15 mm)0.1 in (3 mm)
Rainy days11245813117521
Snowfall0.9 in (2.4 cm)1 in (2.6 cm)0.7 in (1.8 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)0 in (0 cm)1.3 in (3.2 cm)0.9 in (2.4 cm)
Sunshine259 h262 h308 h313 h335 h321 h304 h306 h287 h269 h243 h246 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 +1.6°F (+0.9°C) to +2.5°F (+1.4°C)

Days above 90°F (32°C) a year

42 58

About 1.4× as many

Warming by month
  • January: +2.9°F (+1.6°C)
  • February: +2.3°F (+1.3°C)
  • March: +1.4°F (+0.8°C)
  • April: +2.7°F (+1.5°C)
  • May: +2.1°F (+1.1°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.9°F (+1.1°C)
  • August: +2.4°F (+1.3°C)
  • September: +2.7°F (+1.5°C)
  • October: +1.5°F (+0.9°C)
  • November: +2.4°F (+1.4°C)
  • December: +2.4°F (+1.4°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.