ClimateSearch

Namp’o, Nampo

North Korea · 455k people · 8 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 high32°F (0°C)37°F (3°C)48°F (9°C)61°F (16°C)71°F (22°C)79°F (26°C)82°F (28°C)83°F (28°C)76°F (24°C)64°F (18°C)49°F (10°C)36°F (2°C)
Average low19°F (-7°C)22°F (-6°C)29°F (-1°C)41°F (5°C)52°F (11°C)62°F (17°C)70°F (21°C)71°F (22°C)61°F (16°C)48°F (9°C)35°F (2°C)23°F (-5°C)
Dew point14°F (-10°C)17°F (-8°C)27°F (-3°C)38°F (4°C)50°F (10°C)61°F (16°C)70°F (21°C)71°F (21°C)60°F (16°C)46°F (8°C)33°F (0°C)19°F (-7°C)
Rainfall0.5 in (14 mm)0.7 in (18 mm)1 in (25 mm)1.9 in (48 mm)3.5 in (90 mm)4 in (101 mm)9.8 in (249 mm)8.3 in (210 mm)3.7 in (93 mm)1.6 in (42 mm)1.7 in (43 mm)0.9 in (22 mm)
Rainy days34478915137675
Snowfall2.6 in (6.7 cm)1.9 in (4.8 cm)1.1 in (2.7 cm)0.1 in (0.3 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)0.7 in (1.8 cm)2.2 in (5.5 cm)
Sunshine249 h246 h302 h305 h316 h310 h263 h281 h279 h281 h220 h228 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 +1.7°F (+1.0°C) to +3.3°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: +2.9°F (+1.6°C)
  • February: +2.2°F (+1.2°C)
  • March: +1.9°F (+1.0°C)
  • April: +3.0°F (+1.6°C)
  • May: +2.4°F (+1.3°C)
  • June: +2.5°F (+1.4°C)
  • July: +2.4°F (+1.3°C)
  • August: +2.9°F (+1.6°C)
  • September: +3.3°F (+1.8°C)
  • October: +2.6°F (+1.4°C)
  • November: +2.6°F (+1.5°C)
  • December: +2.8°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.