ClimateSearch

Mabalacat City, Central Luzon

Philippines · 188k people · 107 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)89°F (32°C)92°F (33°C)94°F (35°C)93°F (34°C)90°F (32°C)88°F (31°C)87°F (31°C)88°F (31°C)89°F (32°C)89°F (32°C)88°F (31°C)
Average low71°F (22°C)71°F (22°C)73°F (23°C)75°F (24°C)76°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)72°F (22°C)
Dew point67°F (19°C)67°F (19°C)68°F (20°C)70°F (21°C)73°F (23°C)75°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)73°F (23°C)71°F (22°C)69°F (20°C)
Rainfall0.7 in (18 mm)0.7 in (18 mm)1.4 in (36 mm)2.3 in (59 mm)8.2 in (207 mm)11.2 in (285 mm)18.1 in (459 mm)17.4 in (441 mm)15 in (382 mm)6.8 in (172 mm)3.7 in (95 mm)2.3 in (58 mm)
Rainy days112515192425221054
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)
Sunshine217 h213 h252 h248 h189 h145 h106 h94 h107 h163 h190 h195 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

+1.4°F (+0.8°C)

Models range from +0.6°F (+0.3°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

56 → 80

About 1.4× as many

Warming by month
  • January: +1.3°F (+0.7°C)
  • February: +1.1°F (+0.6°C)
  • March: +1.2°F (+0.7°C)
  • April: +2.0°F (+1.1°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.7°F (+1.0°C)
  • July: +1.3°F (+0.7°C)
  • August: +1.2°F (+0.7°C)
  • September: +1.5°F (+0.9°C)
  • October: +1.2°F (+0.7°C)
  • November: +1.2°F (+0.7°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.