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 high86°F (30°C)88°F (31°C)91°F (33°C)94°F (34°C)93°F (34°C)91°F (33°C)89°F (31°C)88°F (31°C)88°F (31°C)89°F (32°C)88°F (31°C)87°F (30°C)
Average low71°F (22°C)71°F (22°C)73°F (23°C)75°F (24°C)76°F (25°C)76°F (25°C)75°F (24°C)76°F (24°C)75°F (24°C)74°F (24°C)74°F (23°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)
Rainfall1.6 in (42 mm)1.5 in (38 mm)1.5 in (38 mm)1.8 in (47 mm)8.2 in (208 mm)12.1 in (308 mm)21 in (533 mm)20.9 in (531 mm)17.2 in (437 mm)9.4 in (238 mm)5.5 in (140 mm)5.6 in (141 mm)
Rainy days232413202626241376
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)
Sunshine216 h211 h251 h252 h201 h159 h119 h115 h120 h161 h187 h188 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.