ClimateSearch

Kotamobagu, North Sulawesi

Indonesia · 122k people · 249 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 high87°F (31°C)87°F (31°C)88°F (31°C)89°F (31°C)88°F (31°C)87°F (31°C)87°F (30°C)87°F (31°C)89°F (31°C)89°F (32°C)89°F (32°C)88°F (31°C)
Average low71°F (22°C)71°F (22°C)71°F (22°C)71°F (21°C)71°F (22°C)71°F (22°C)71°F (21°C)70°F (21°C)70°F (21°C)70°F (21°C)71°F (22°C)71°F (22°C)
Dew point74°F (23°C)73°F (23°C)74°F (23°C)74°F (24°C)74°F (24°C)74°F (23°C)73°F (23°C)72°F (22°C)72°F (22°C)73°F (23°C)74°F (23°C)74°F (23°C)
Rainfall8.3 in (211 mm)7.3 in (185 mm)7.5 in (191 mm)8.6 in (219 mm)9.1 in (232 mm)8.2 in (208 mm)6.3 in (160 mm)3.8 in (95 mm)3.8 in (96 mm)5.9 in (149 mm)9.1 in (230 mm)8 in (203 mm)
Rainy days1816172021181499142120
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)
Sunshine150 h145 h164 h150 h157 h147 h171 h191 h182 h174 h147 h140 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

+1.3°F (+0.7°C)

Models range from +1.0°F (+0.5°C) to +1.5°F (+0.9°C)

Days above 90°F (32°C) a year

1 → 3

About 2.2× as many

Warming by month
  • January: +1.8°F (+1.0°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.6°F (+0.9°C)
  • April: +1.7°F (+1.0°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.4°F (+0.8°C)
  • July: +1.2°F (+0.7°C)
  • August: +1.3°F (+0.7°C)
  • September: +1.1°F (+0.6°C)
  • October: +1.2°F (+0.7°C)
  • November: +1.6°F (+0.9°C)
  • December: +1.8°F (+1.0°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.