ClimateSearch

Malabon, National Capital Region

Philippines · 366k people · 4 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 high83°F (29°C)85°F (30°C)88°F (31°C)91°F (33°C)90°F (32°C)87°F (31°C)85°F (29°C)84°F (29°C)84°F (29°C)85°F (30°C)85°F (30°C)84°F (29°C)
Average low73°F (23°C)73°F (23°C)74°F (24°C)77°F (25°C)78°F (26°C)78°F (25°C)77°F (25°C)77°F (25°C)76°F (25°C)76°F (25°C)76°F (24°C)74°F (24°C)
Dew point69°F (20°C)69°F (20°C)70°F (21°C)72°F (22°C)74°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)73°F (23°C)71°F (22°C)
Rainfall1.2 in (30 mm)1 in (26 mm)1.2 in (30 mm)1.5 in (39 mm)7.6 in (194 mm)11 in (280 mm)17.7 in (450 mm)16.9 in (429 mm)15.4 in (392 mm)8.8 in (225 mm)3.8 in (97 mm)4 in (102 mm)
Rainy days4357202629302820108
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)
Sunshine318 h301 h351 h352 h335 h305 h268 h265 h261 h289 h295 h291 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

53 72

About 1.4× as many

Warming by month
  • January: +1.0°F (+0.6°C)
  • February: +0.9°F (+0.5°C)
  • March: +1.0°F (+0.6°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.2°F (+0.6°C)
  • June: +1.2°F (+0.7°C)
  • July: +0.9°F (+0.5°C)
  • August: +0.7°F (+0.4°C)
  • September: +1.2°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.