ClimateSearch

San Pablo, Calabarzon

Philippines · 300k people · 115 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 high81°F (27°C)82°F (28°C)85°F (29°C)88°F (31°C)89°F (31°C)87°F (30°C)85°F (29°C)85°F (29°C)85°F (29°C)84°F (29°C)83°F (28°C)81°F (27°C)
Average low72°F (22°C)72°F (22°C)74°F (23°C)76°F (24°C)77°F (25°C)77°F (25°C)76°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)
Dew point70°F (21°C)69°F (21°C)71°F (22°C)73°F (23°C)75°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)
Rainfall1.7 in (44 mm)1.5 in (39 mm)1.8 in (46 mm)2.1 in (52 mm)6.9 in (176 mm)9.5 in (242 mm)15 in (380 mm)12.4 in (314 mm)14.1 in (359 mm)9.5 in (241 mm)5 in (127 mm)6.4 in (163 mm)
Rainy days868102126292727241714
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)
Sunshine314 h301 h350 h352 h342 h314 h281 h288 h275 h293 h294 h290 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

+1.6°F (+0.9°C)

Models range from +1.5°F (+0.8°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

20 40

About 2.0× as many

Warming by month
  • January: +1.3°F (+0.7°C)
  • February: +1.3°F (+0.7°C)
  • March: +1.4°F (+0.8°C)
  • April: +1.8°F (+1.0°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.9°F (+1.1°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.8°F (+1.0°C)
  • October: +1.6°F (+0.9°C)
  • November: +1.4°F (+0.8°C)
  • December: +1.5°F (+0.8°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.