ClimateSearch

San Pedro, Calabarzon

Philippines · 349k people · 13 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 high87°F (31°C)89°F (31°C)91°F (33°C)94°F (34°C)93°F (34°C)91°F (33°C)88°F (31°C)88°F (31°C)88°F (31°C)88°F (31°C)88°F (31°C)87°F (31°C)
Average low73°F (23°C)73°F (23°C)75°F (24°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 (20°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)
Rainfall1.3 in (34 mm)0.8 in (21 mm)0.9 in (23 mm)1.1 in (29 mm)6.1 in (155 mm)9.2 in (235 mm)15.3 in (389 mm)14.6 in (371 mm)12.7 in (322 mm)8.7 in (220 mm)6 in (152 mm)5.3 in (134 mm)
Rainy days222213182424221486
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)
Sunshine207 h206 h246 h248 h202 h160 h122 h123 h123 h161 h182 h180 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

48 → 70

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 (+0.6°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: +1.0°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.