ClimateSearch

Yichun, Heilongjiang

China · 156k people · 228 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 high6°F (-14°C)17°F (-8°C)32°F (0°C)51°F (10°C)64°F (18°C)73°F (23°C)78°F (25°C)74°F (24°C)65°F (18°C)48°F (9°C)26°F (-3°C)9°F (-13°C)
Average low-15°F (-26°C)-8°F (-22°C)8°F (-13°C)29°F (-2°C)42°F (6°C)55°F (13°C)62°F (16°C)59°F (15°C)47°F (8°C)31°F (0°C)11°F (-12°C)-8°F (-22°C)
Dew point-12°F (-24°C)-5°F (-20°C)7°F (-14°C)22°F (-5°C)40°F (4°C)55°F (13°C)63°F (17°C)60°F (16°C)46°F (8°C)28°F (-2°C)6°F (-14°C)-8°F (-22°C)
Rainfall0.2 in (5 mm)0.3 in (7 mm)0.7 in (18 mm)1.5 in (37 mm)2.8 in (72 mm)4.1 in (104 mm)5.6 in (142 mm)4.9 in (123 mm)2.8 in (70 mm)1.6 in (41 mm)0.7 in (17 mm)0.4 in (10 mm)
Rainy days22581214151511853
Snowfall1.9 in (4.9 cm)2.4 in (6.2 cm)5 in (12.7 cm)2.9 in (7.4 cm)0.4 in (1 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.2 in (0.4 cm)2.2 in (5.7 cm)4.3 in (11 cm)3.5 in (9 cm)
Sunshine235 h245 h292 h305 h328 h319 h304 h283 h275 h241 h208 h201 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

+2.4°F (+1.3°C)

Models range from +1.3°F (+0.7°C) to +3.6°F (+2.0°C)

Days above 90°F (32°C) a year

1 2

About 2.1× as many

Warming by month
  • January: +3.0°F (+1.7°C)
  • February: +2.7°F (+1.5°C)
  • March: +1.9°F (+1.1°C)
  • April: +2.7°F (+1.5°C)
  • May: +2.3°F (+1.3°C)
  • June: +1.9°F (+1.1°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.9°F (+1.6°C)
  • September: +3.2°F (+1.8°C)
  • October: +3.9°F (+2.1°C)
  • November: +3.9°F (+2.2°C)
  • December: +3.9°F (+2.1°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.