ClimateSearch

Cagayan de Oro, Northern Mindanao

Philippines · 742k people · 9 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 high81°F (27°C)82°F (28°C)83°F (28°C)84°F (29°C)84°F (29°C)83°F (28°C)82°F (28°C)83°F (28°C)83°F (28°C)82°F (28°C)82°F (28°C)82°F (28°C)
Average low72°F (22°C)72°F (22°C)72°F (22°C)73°F (23°C)74°F (24°C)74°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)
Dew point72°F (22°C)72°F (22°C)72°F (22°C)73°F (23°C)74°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)
Rainfall9.8 in (248 mm)8.4 in (213 mm)7.6 in (194 mm)8.4 in (214 mm)12 in (305 mm)15 in (381 mm)11.1 in (281 mm)8.5 in (216 mm)8.7 in (222 mm)11.2 in (285 mm)12 in (305 mm)10.1 in (257 mm)
Rainy days221920212727252123272625
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)
Sunshine287 h284 h331 h329 h329 h296 h300 h309 h286 h294 h285 h295 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

+1.2°F (+0.7°C)

Models range from +0.6°F (+0.4°C) to +1.6°F (+0.9°C)

Days above 90°F (32°C) a year

1 1

About 1.8× as many

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