ClimateSearch

Commonwealth, National Capital Region

Philippines · 215k people · 81 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 high82°F (28°C)84°F (29°C)87°F (31°C)90°F (32°C)89°F (32°C)86°F (30°C)84°F (29°C)83°F (29°C)84°F (29°C)84°F (29°C)84°F (29°C)82°F (28°C)
Average low71°F (22°C)72°F (22°C)73°F (23°C)76°F (24°C)77°F (25°C)77°F (25°C)76°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)73°F (23°C)
Dew point68°F (20°C)68°F (20°C)69°F (21°C)72°F (22°C)74°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)73°F (23°C)70°F (21°C)
Rainfall1.3 in (34 mm)1.1 in (27 mm)1.2 in (31 mm)1.7 in (43 mm)8.1 in (206 mm)11.7 in (297 mm)18.5 in (470 mm)17.9 in (455 mm)16.1 in (409 mm)9.4 in (240 mm)4.1 in (104 mm)4.1 in (104 mm)
Rainy days4358202629302921108
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)
Sunshine316 h299 h350 h350 h333 h304 h266 h264 h260 h288 h294 h290 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

+0.9°F (+0.5°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

42 60

About 1.4× as many

Warming by month
  • January: +0.9°F (+0.5°C)
  • February: +0.8°F (+0.5°C)
  • March: +1.0°F (+0.6°C)
  • April: +1.5°F (+0.8°C)
  • May: +1.2°F (+0.7°C)
  • June: +1.3°F (+0.7°C)
  • July: +0.9°F (+0.5°C)
  • August: +0.6°F (+0.3°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.0°F (+0.6°C)
  • November: +1.1°F (+0.6°C)
  • December: +1.3°F (+0.7°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.