ClimateSearch

Yeosu, Jeollanam-do

South Korea · 269k people · 9 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 high45°F (7°C)48°F (9°C)56°F (13°C)66°F (19°C)74°F (23°C)78°F (26°C)83°F (28°C)86°F (30°C)80°F (27°C)72°F (22°C)60°F (16°C)48°F (9°C)
Average low29°F (-2°C)31°F (0°C)39°F (4°C)48°F (9°C)57°F (14°C)65°F (19°C)73°F (23°C)74°F (23°C)66°F (19°C)55°F (13°C)43°F (6°C)32°F (0°C)
Dew point25°F (-4°C)27°F (-3°C)35°F (2°C)45°F (7°C)55°F (13°C)64°F (18°C)72°F (22°C)73°F (23°C)64°F (18°C)52°F (11°C)41°F (5°C)29°F (-1°C)
Rainfall0.9 in (23 mm)1.4 in (36 mm)2.8 in (70 mm)4.5 in (115 mm)5.3 in (133 mm)7 in (177 mm)9.9 in (251 mm)10.7 in (272 mm)6 in (152 mm)2.3 in (60 mm)1.7 in (42 mm)1 in (26 mm)
Rainy days34787810107453
Snowfall0.5 in (1.2 cm)0.5 in (1.2 cm)0.2 in (0.6 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 in (0 cm)0 in (0 cm)0.3 in (0.7 cm)
Sunshine168 h165 h182 h188 h185 h145 h136 h179 h166 h203 h175 h175 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

+2.3°F (+1.3°C)

Models range from +2.1°F (+1.2°C) to +2.4°F (+1.4°C)

Days above 90°F (32°C) a year

—

Too few hot days today to project a reliable change

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +1.9°F (+1.1°C)
  • March: +1.6°F (+0.9°C)
  • April: +2.4°F (+1.3°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.4°F (+1.3°C)
  • August: +2.4°F (+1.3°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.6°F (+1.4°C)
  • November: +2.2°F (+1.2°C)
  • December: +2.5°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.