ClimateSearch

Mantampay, Northern Mindanao

Philippines · 265k people · 162 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 high88°F (31°C)88°F (31°C)91°F (33°C)92°F (33°C)92°F (34°C)91°F (33°C)90°F (32°C)90°F (32°C)90°F (32°C)90°F (32°C)90°F (32°C)89°F (32°C)
Average low72°F (22°C)72°F (22°C)73°F (23°C)75°F (24°C)76°F (24°C)75°F (24°C)74°F (24°C)74°F (24°C)74°F (23°C)74°F (23°C)73°F (23°C)73°F (23°C)
Dew point72°F (22°C)71°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)
Rainfall5.3 in (134 mm)4.6 in (116 mm)4.3 in (109 mm)4.5 in (114 mm)8.2 in (209 mm)10.4 in (265 mm)11.6 in (294 mm)13.4 in (341 mm)18.4 in (468 mm)20.7 in (525 mm)11.3 in (287 mm)8.8 in (224 mm)
Rainy days118891719181722241916
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 h159 h196 h200 h173 h137 h139 h153 h139 h143 h148 h153 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

+1.5°F (+0.8°C)

Models range from +1.3°F (+0.7°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

—

Too few hot days today to project a reliable change

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.4°F (+0.8°C)
  • April: +1.1°F (+0.6°C)
  • May: +1.3°F (+0.7°C)
  • June: +1.4°F (+0.8°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.5°F (+0.9°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.7°F (+0.9°C)
  • November: +1.8°F (+1.0°C)
  • December: +1.7°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.