ClimateSearch

Andong, Gyeongsangbuk-do

South Korea · 153k people · 98 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 high40°F (4°C)45°F (7°C)55°F (13°C)68°F (20°C)77°F (25°C)83°F (28°C)85°F (29°C)86°F (30°C)78°F (26°C)69°F (21°C)56°F (13°C)43°F (6°C)
Average low19°F (-7°C)23°F (-5°C)31°F (0°C)42°F (6°C)53°F (11°C)62°F (17°C)69°F (21°C)69°F (21°C)59°F (15°C)45°F (7°C)33°F (0°C)22°F (-6°C)
Dew point15°F (-9°C)19°F (-7°C)28°F (-2°C)38°F (3°C)49°F (10°C)60°F (15°C)69°F (21°C)70°F (21°C)60°F (16°C)48°F (9°C)35°F (1°C)21°F (-6°C)
Rainfall0.9 in (24 mm)1.3 in (33 mm)1.9 in (48 mm)2.9 in (73 mm)2.9 in (73 mm)4.4 in (112 mm)9.2 in (234 mm)8.8 in (223 mm)5.7 in (146 mm)2.2 in (56 mm)1.4 in (36 mm)1 in (25 mm)
Rainy days3467761097454
Snowfall1.9 in (4.8 cm)1.5 in (3.9 cm)1.7 in (4.3 cm)0.2 in (0.5 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)0.2 in (0.5 cm)1 in (2.6 cm)
Sunshine176 h176 h189 h201 h203 h169 h128 h154 h153 h191 h172 h180 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

+2.6°F (+1.4°C)

Models range from +2.4°F (+1.4°C) to +2.8°F (+1.5°C)

Days above 90°F (32°C) a year

10 → 28

About 2.6× as many

Warming by month
  • January: +2.5°F (+1.4°C)
  • February: +2.2°F (+1.2°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.8°F (+1.5°C)
  • May: +2.5°F (+1.4°C)
  • June: +2.4°F (+1.3°C)
  • July: +2.5°F (+1.4°C)
  • August: +2.9°F (+1.6°C)
  • September: +3.2°F (+1.8°C)
  • October: +2.5°F (+1.4°C)
  • November: +2.6°F (+1.4°C)
  • December: +2.6°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.