ClimateSearch

Kaech’ŏn, South Pyongan

North Korea · 320k people · 33 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 high29°F (-1°C)37°F (3°C)48°F (9°C)61°F (16°C)71°F (22°C)78°F (26°C)82°F (28°C)83°F (28°C)75°F (24°C)63°F (17°C)47°F (8°C)33°F (0°C)
Average low10°F (-12°C)18°F (-8°C)28°F (-2°C)38°F (4°C)51°F (10°C)61°F (16°C)69°F (21°C)69°F (21°C)58°F (15°C)44°F (7°C)31°F (-1°C)17°F (-8°C)
Dew point6°F (-14°C)11°F (-11°C)23°F (-5°C)37°F (3°C)50°F (10°C)61°F (16°C)69°F (21°C)69°F (21°C)58°F (14°C)43°F (6°C)27°F (-3°C)11°F (-11°C)
Rainfall0.6 in (15 mm)0.9 in (24 mm)1.3 in (34 mm)2.5 in (64 mm)4.3 in (108 mm)5.2 in (133 mm)14.1 in (357 mm)11.1 in (283 mm)4.7 in (120 mm)2.4 in (60 mm)2.5 in (63 mm)1.2 in (30 mm)
Rainy days3468101219168886
Snowfall3.9 in (9.8 cm)3.9 in (10 cm)2.7 in (6.9 cm)0.5 in (1.3 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)2.2 in (5.6 cm)5.3 in (13.4 cm)
Sunshine249 h244 h293 h293 h302 h294 h238 h266 h274 h273 h211 h226 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 +1.6°F (+0.9°C) to +3.3°F (+1.8°C)

Days above 90°F (32°C) a year

2 7

About 3.6× as many

Warming by month
  • January: +3.2°F (+1.8°C)
  • February: +2.6°F (+1.4°C)
  • March: +1.9°F (+1.1°C)
  • April: +3.0°F (+1.7°C)
  • May: +2.6°F (+1.4°C)
  • June: +2.7°F (+1.5°C)
  • July: +1.8°F (+1.0°C)
  • August: +3.1°F (+1.7°C)
  • September: +3.3°F (+1.8°C)
  • October: +2.8°F (+1.5°C)
  • November: +2.5°F (+1.4°C)
  • December: +2.9°F (+1.6°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.