ClimateSearch

Manokwari, West Papua

Indonesia · 132k people · 12 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 high82°F (28°C)82°F (28°C)82°F (28°C)82°F (28°C)82°F (28°C)82°F (28°C)81°F (27°C)82°F (28°C)82°F (28°C)82°F (28°C)82°F (28°C)82°F (28°C)
Average low74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)
Dew point73°F (23°C)73°F (23°C)73°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)74°F (23°C)74°F (23°C)
Rainfall12.4 in (315 mm)10.5 in (268 mm)12.4 in (315 mm)13.6 in (345 mm)8.7 in (221 mm)8.3 in (210 mm)7.5 in (189 mm)6.5 in (164 mm)6 in (152 mm)6.9 in (175 mm)9.6 in (243 mm)12.3 in (311 mm)
Rainy days272528272626242323242629
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)
Sunshine305 h275 h305 h298 h329 h310 h313 h325 h323 h333 h307 h306 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

+1.6°F (+0.9°C)

Models range from +1.3°F (+0.7°C) to +2.1°F (+1.2°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +1.7°F (+1.0°C)
  • February: +1.5°F (+0.8°C)
  • March: +1.5°F (+0.8°C)
  • April: +1.5°F (+0.9°C)
  • May: +1.5°F (+0.8°C)
  • June: +1.4°F (+0.8°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.6°F (+0.9°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.4°F (+0.8°C)
  • November: +1.4°F (+0.8°C)
  • December: +1.6°F (+0.9°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.