ClimateSearch

Dinaig, Autonomous Region in Muslim Mindanao

Philippines · 117k people · 48 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 high84°F (29°C)85°F (29°C)86°F (30°C)86°F (30°C)85°F (30°C)84°F (29°C)83°F (29°C)83°F (29°C)84°F (29°C)84°F (29°C)85°F (29°C)84°F (29°C)
Average low75°F (24°C)75°F (24°C)75°F (24°C)76°F (25°C)77°F (25°C)76°F (24°C)75°F (24°C)75°F (24°C)76°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)
Dew point73°F (23°C)72°F (22°C)73°F (23°C)74°F (23°C)75°F (24°C)75°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)74°F (24°C)74°F (23°C)
Rainfall6.6 in (166 mm)5.5 in (140 mm)6.1 in (155 mm)6.8 in (172 mm)11.4 in (289 mm)12.4 in (315 mm)11.1 in (282 mm)9.7 in (248 mm)8.7 in (221 mm)10.4 in (263 mm)8.7 in (220 mm)7.1 in (182 mm)
Rainy days191719232828282626282623
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 h297 h336 h325 h317 h287 h298 h305 h288 h295 h289 h305 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 +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

4 14

About 3.2× as many

Warming by month
  • January: +1.5°F (+0.9°C)
  • February: +1.7°F (+0.9°C)
  • March: +1.7°F (+1.0°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.5°F (+0.8°C)
  • June: +1.5°F (+0.8°C)
  • July: +1.5°F (+0.9°C)
  • August: +1.8°F (+1.0°C)
  • September: +1.7°F (+0.9°C)
  • October: +1.9°F (+1.1°C)
  • November: +1.8°F (+1.0°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.