ClimateSearch

Angeles City, Central Luzon

Philippines · 483k people · 93 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 high89°F (32°C)90°F (32°C)92°F (34°C)95°F (35°C)93°F (34°C)91°F (33°C)88°F (31°C)88°F (31°C)88°F (31°C)90°F (32°C)90°F (32°C)89°F (32°C)
Average low71°F (22°C)71°F (22°C)73°F (23°C)75°F (24°C)76°F (25°C)76°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)
Dew point67°F (19°C)67°F (19°C)68°F (20°C)71°F (21°C)73°F (23°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)69°F (21°C)
Rainfall0.9 in (22 mm)0.8 in (21 mm)1.4 in (36 mm)2.2 in (56 mm)8.5 in (216 mm)12 in (305 mm)19.3 in (490 mm)18.4 in (466 mm)15.7 in (398 mm)7 in (178 mm)3.9 in (100 mm)2.6 in (67 mm)
Rainy days123415202525221154
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 h162 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

54 → 78

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.