ClimateSearch

Osan, Gyeonggi-do

South Korea · 239k people · 24 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)41°F (5°C)50°F (10°C)62°F (17°C)72°F (22°C)80°F (27°C)83°F (28°C)84°F (29°C)77°F (25°C)66°F (19°C)52°F (11°C)40°F (4°C)
Average low22°F (-6°C)25°F (-4°C)32°F (0°C)42°F (6°C)53°F (12°C)63°F (17°C)71°F (22°C)72°F (22°C)62°F (17°C)49°F (10°C)36°F (2°C)25°F (-4°C)
Dew point16°F (-9°C)19°F (-7°C)29°F (-1°C)40°F (4°C)51°F (11°C)61°F (16°C)71°F (21°C)71°F (22°C)61°F (16°C)47°F (9°C)34°F (1°C)21°F (-6°C)
Rainfall0.8 in (20 mm)1.1 in (27 mm)1.5 in (39 mm)2.7 in (69 mm)3.6 in (90 mm)4.7 in (119 mm)11.3 in (288 mm)9.7 in (245 mm)5 in (126 mm)2.2 in (56 mm)1.8 in (46 mm)0.9 in (23 mm)
Rainy days44677816148575
Snowfall2.3 in (5.8 cm)1.7 in (4.2 cm)1.2 in (3 cm)0 in (0.1 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)0.3 in (0.7 cm)1.5 in (3.7 cm)
Sunshine242 h243 h289 h300 h308 h293 h245 h268 h258 h278 h226 h236 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

+2.5°F (+1.4°C)

Models range from +2.1°F (+1.1°C) to +2.7°F (+1.5°C)

Days above 90°F (32°C) a year

5 13

About 2.7× as many

Warming by month
  • January: +2.6°F (+1.4°C)
  • February: +2.2°F (+1.2°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.6°F (+1.5°C)
  • May: +2.3°F (+1.3°C)
  • June: +2.6°F (+1.4°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.6°F (+1.4°C)
  • September: +3.1°F (+1.7°C)
  • October: +2.9°F (+1.6°C)
  • November: +2.5°F (+1.4°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.