ClimateSearch

Suihua, Heilongjiang

China · 252k people · 178 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 (-15°C)17°F (-8°C)35°F (2°C)55°F (13°C)68°F (20°C)77°F (25°C)80°F (27°C)76°F (25°C)67°F (20°C)51°F (11°C)29°F (-1°C)10°F (-12°C)
Average low-13°F (-25°C)-5°F (-20°C)14°F (-10°C)32°F (0°C)46°F (8°C)58°F (15°C)65°F (18°C)62°F (16°C)50°F (10°C)34°F (1°C)15°F (-9°C)-6°F (-21°C)
Dew point-11°F (-24°C)-2°F (-19°C)7°F (-14°C)22°F (-5°C)39°F (4°C)55°F (13°C)64°F (18°C)62°F (17°C)47°F (9°C)29°F (-2°C)9°F (-13°C)-7°F (-22°C)
Rainfall0.2 in (4 mm)0.2 in (5 mm)0.6 in (14 mm)1.3 in (32 mm)2.2 in (56 mm)4 in (101 mm)6.1 in (156 mm)5.4 in (136 mm)2.8 in (72 mm)1.5 in (38 mm)0.6 in (15 mm)0.3 in (9 mm)
Rainy days124691315149733
Snowfall1.5 in (3.9 cm)1.8 in (4.5 cm)3.2 in (8.1 cm)1.2 in (3.1 cm)0.1 in (0.2 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.7 in (1.9 cm)3.1 in (7.8 cm)2.8 in (7.2 cm)
Sunshine239 h249 h302 h309 h337 h341 h321 h300 h288 h255 h219 h214 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 +0.5°F (+0.3°C) to +3.9°F (+2.1°C)

Days above 90°F (32°C) a year

2 1

Fewer than today

Warming by month
  • January: +3.6°F (+2.0°C)
  • February: +3.3°F (+1.8°C)
  • March: +2.6°F (+1.5°C)
  • April: +2.6°F (+1.5°C)
  • May: +2.3°F (+1.3°C)
  • June: +1.6°F (+0.9°C)
  • July: +2.0°F (+1.1°C)
  • August: +2.6°F (+1.4°C)
  • September: +3.1°F (+1.7°C)
  • October: +3.7°F (+2.1°C)
  • November: +4.2°F (+2.4°C)
  • December: +4.2°F (+2.4°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.