ClimateSearch

Jishu, Jilin

China · 104k people · 248 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 high12°F (-11°C)22°F (-6°C)37°F (3°C)55°F (13°C)68°F (20°C)77°F (25°C)80°F (27°C)78°F (25°C)69°F (20°C)53°F (12°C)33°F (1°C)17°F (-9°C)
Average low-8°F (-22°C)0°F (-18°C)17°F (-8°C)33°F (1°C)47°F (8°C)58°F (15°C)65°F (18°C)63°F (17°C)51°F (11°C)36°F (2°C)19°F (-7°C)-1°F (-18°C)
Dew point-6°F (-21°C)1°F (-17°C)11°F (-12°C)26°F (-3°C)42°F (6°C)56°F (13°C)65°F (18°C)63°F (17°C)50°F (10°C)33°F (0°C)14°F (-10°C)-1°F (-18°C)
Rainfall0.3 in (8 mm)0.4 in (11 mm)0.9 in (23 mm)1.5 in (39 mm)3.1 in (78 mm)4.2 in (106 mm)6.9 in (176 mm)6.1 in (155 mm)2.7 in (68 mm)1.9 in (49 mm)1.2 in (30 mm)0.5 in (14 mm)
Rainy days3357111416149864
Snowfall2.7 in (6.9 cm)3.1 in (7.9 cm)4.3 in (11 cm)1.1 in (2.9 cm)0.2 in (0.4 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0.1 cm)1.1 in (2.9 cm)5 in (12.7 cm)4.1 in (10.4 cm)
Sunshine240 h245 h296 h303 h315 h333 h306 h288 h288 h257 h210 h220 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

+1.9°F (+1.1°C)

Models range from +0.8°F (+0.4°C) to +3.5°F (+1.9°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +3.8°F (+2.1°C)
  • February: +3.1°F (+1.7°C)
  • March: +2.4°F (+1.3°C)
  • April: +2.7°F (+1.5°C)
  • May: +2.1°F (+1.2°C)
  • June: +1.9°F (+1.1°C)
  • July: +1.7°F (+0.9°C)
  • August: +2.2°F (+1.2°C)
  • September: +3.2°F (+1.8°C)
  • October: +3.0°F (+1.7°C)
  • November: +3.3°F (+1.8°C)
  • December: +3.6°F (+2.0°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.