ClimateSearch

Candelaria, Calabarzon

Philippines · 138k people · 72 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 high86°F (30°C)87°F (31°C)90°F (32°C)92°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)87°F (31°C)86°F (30°C)
Average low73°F (23°C)72°F (22°C)74°F (23°C)75°F (24°C)77°F (25°C)77°F (25°C)76°F (25°C)76°F (25°C)76°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)
Dew point70°F (21°C)70°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)74°F (23°C)72°F (22°C)
Rainfall3.6 in (90 mm)2.7 in (69 mm)2.1 in (53 mm)2.3 in (58 mm)5.6 in (142 mm)7.2 in (184 mm)8.8 in (223 mm)8.1 in (206 mm)9.3 in (237 mm)10.8 in (273 mm)11 in (279 mm)12.6 in (320 mm)
Rainy days54331116181618161413
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)
Sunshine193 h195 h235 h241 h203 h164 h130 h134 h131 h154 h171 h169 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 +1.5°F (+0.8°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

11 → 27

About 2.4× as many

Warming by month
  • January: +1.3°F (+0.7°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.4°F (+0.8°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.9°F (+1.0°C)
  • July: +1.3°F (+0.7°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.7°F (+0.9°C)
  • October: +1.6°F (+0.9°C)
  • November: +1.3°F (+0.7°C)
  • December: +1.4°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.