ClimateSearch

Taguig, National Capital Region

Philippines · 1.3M people · 3 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)87°F (31°C)90°F (32°C)93°F (34°C)93°F (34°C)91°F (33°C)88°F (31°C)87°F (31°C)88°F (31°C)88°F (31°C)88°F (31°C)86°F (30°C)
Average low72°F (22°C)72°F (22°C)74°F (23°C)76°F (25°C)77°F (25°C)77°F (25°C)76°F (25°C)76°F (25°C)76°F (24°C)76°F (24°C)75°F (24°C)74°F (23°C)
Dew point69°F (21°C)69°F (20°C)70°F (21°C)72°F (22°C)74°F (23°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)71°F (22°C)
Rainfall1.2 in (31 mm)0.9 in (23 mm)0.9 in (23 mm)1.1 in (29 mm)6 in (154 mm)8.7 in (221 mm)15.8 in (401 mm)16.2 in (411 mm)14 in (355 mm)9.1 in (231 mm)5.4 in (138 mm)5.1 in (130 mm)
Rainy days22129152122201265
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)
Sunshine214 h211 h251 h256 h207 h163 h122 h119 h122 h164 h188 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

+1.0°F (+0.6°C)

Models range from −1.3°F (−0.7°C) to +1.9°F (+1.1°C)

Days above 90°F (32°C) a year

41 → 61

About 1.5× as many

Warming by month
  • January: +1.1°F (+0.6°C)
  • February: +1.0°F (+0.6°C)
  • March: +1.0°F (+0.5°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.2°F (+0.7°C)
  • June: +1.4°F (+0.8°C)
  • July: +0.9°F (+0.5°C)
  • August: +0.7°F (+0.4°C)
  • September: +1.2°F (+0.7°C)
  • October: +1.1°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.