ClimateSearch

Port Moresby, National Capital

Papua New Guinea · 284k people · 10 m elevation · Southern 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 high90°F (32°C)90°F (32°C)89°F (32°C)89°F (32°C)88°F (31°C)86°F (30°C)85°F (29°C)85°F (29°C)86°F (30°C)89°F (31°C)90°F (32°C)91°F (33°C)
Average low75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)73°F (23°C)73°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)75°F (24°C)
Dew point74°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)73°F (23°C)72°F (22°C)70°F (21°C)69°F (21°C)70°F (21°C)72°F (22°C)73°F (23°C)74°F (23°C)
Rainfall8 in (203 mm)6.4 in (161 mm)10.2 in (259 mm)5.6 in (141 mm)4.5 in (115 mm)3.5 in (89 mm)1.4 in (36 mm)1.8 in (47 mm)3.6 in (91 mm)4.6 in (116 mm)3.7 in (95 mm)5.8 in (148 mm)
Rainy days14131811752468712
Snowfall0 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 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)
Sunshine140 h122 h126 h146 h185 h182 h195 h200 h196 h206 h190 h173 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

+1.4°F (+0.8°C)

Models range from +1.2°F (+0.7°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

24 → 44

About 1.8× as many

Warming by month
  • January: +1.5°F (+0.8°C)
  • February: +1.5°F (+0.9°C)
  • March: +1.2°F (+0.7°C)
  • April: +1.5°F (+0.8°C)
  • May: +1.7°F (+0.9°C)
  • June: +1.3°F (+0.7°C)
  • July: +1.5°F (+0.9°C)
  • August: +1.2°F (+0.7°C)
  • September: +1.4°F (+0.8°C)
  • October: +0.9°F (+0.5°C)
  • November: +1.1°F (+0.6°C)
  • December: +1.2°F (+0.7°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.