ClimateSearch

Cotabato, Autonomous Region in Muslim Mindanao

Philippines · 383k 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 high90°F (32°C)91°F (33°C)92°F (33°C)93°F (34°C)92°F (33°C)91°F (33°C)90°F (32°C)90°F (32°C)90°F (32°C)91°F (33°C)91°F (33°C)91°F (33°C)
Average low74°F (24°C)74°F (23°C)74°F (23°C)75°F (24°C)76°F (24°C)75°F (24°C)74°F (24°C)75°F (24°C)74°F (24°C)74°F (24°C)75°F (24°C)74°F (24°C)
Dew point73°F (23°C)73°F (23°C)73°F (23°C)74°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)
Rainfall5 in (128 mm)4.8 in (123 mm)6.9 in (174 mm)6.9 in (175 mm)12.3 in (313 mm)11 in (280 mm)12.6 in (321 mm)11.9 in (302 mm)10.3 in (262 mm)11.8 in (299 mm)8.8 in (223 mm)6 in (151 mm)
Rainy days101012132122212018211712
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)
Sunshine176 h178 h207 h200 h169 h138 h141 h152 h143 h148 h159 h171 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 +1.5°F (+0.8°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

10 → 31

About 3.0× as many

Warming by month
  • January: +1.3°F (+0.7°C)
  • February: +1.7°F (+0.9°C)
  • March: +1.7°F (+0.9°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.5°F (+0.8°C)
  • June: +1.5°F (+0.8°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.8°F (+1.0°C)
  • September: +1.6°F (+0.9°C)
  • October: +1.7°F (+1.0°C)
  • November: +1.6°F (+0.9°C)
  • December: +1.7°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.