ClimateSearch

Calasiao, Ilocos

Philippines · 101k people · 6 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 high84°F (29°C)86°F (30°C)89°F (32°C)92°F (33°C)90°F (32°C)88°F (31°C)85°F (30°C)85°F (29°C)85°F (29°C)85°F (30°C)86°F (30°C)85°F (29°C)
Average low71°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 (24°C)76°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)73°F (23°C)
Dew point67°F (19°C)67°F (19°C)68°F (20°C)71°F (22°C)74°F (23°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)69°F (21°C)
Rainfall0.4 in (11 mm)0.5 in (13 mm)0.8 in (21 mm)1.6 in (40 mm)7.8 in (198 mm)10 in (255 mm)15.8 in (402 mm)16.2 in (412 mm)13.4 in (339 mm)7.2 in (183 mm)2.6 in (67 mm)1.5 in (38 mm)
Rainy days224820252828271566
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)
Sunshine323 h306 h359 h353 h324 h293 h257 h242 h258 h297 h301 h302 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

+1.5°F (+0.9°C)

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

Days above 90°F (32°C) a year

61 97

About 1.6× as many

Warming by month
  • January: +1.5°F (+0.8°C)
  • February: +1.6°F (+0.9°C)
  • March: +1.7°F (+0.9°C)
  • April: +2.3°F (+1.3°C)
  • May: +1.7°F (+1.0°C)
  • June: +1.7°F (+1.0°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.5°F (+0.8°C)
  • September: +1.8°F (+1.0°C)
  • October: +1.5°F (+0.8°C)
  • November: +1.3°F (+0.7°C)
  • December: +1.6°F (+0.9°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.