ClimateSearch

Binangonan, Calabarzon

Philippines · 219k people · 11 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 high83°F (28°C)84°F (29°C)87°F (31°C)90°F (32°C)91°F (33°C)89°F (32°C)87°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)85°F (30°C)84°F (29°C)
Average low72°F (22°C)72°F (22°C)74°F (23°C)76°F (25°C)77°F (25°C)76°F (25°C)76°F (24°C)76°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)74°F (23°C)
Dew point69°F (21°C)69°F (21°C)71°F (21°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 (23°C)73°F (23°C)71°F (22°C)
Rainfall1.4 in (35 mm)1 in (26 mm)1.2 in (31 mm)1.4 in (35 mm)6.3 in (159 mm)8.7 in (220 mm)14.8 in (376 mm)14.4 in (365 mm)13.9 in (353 mm)9 in (229 mm)6.4 in (164 mm)6 in (153 mm)
Rainy days22229142121201165
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)
Sunshine213 h210 h251 h256 h206 h163 h122 h118 h122 h164 h187 h188 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 +0.9°F (+0.5°C) to +1.9°F (+1.1°C)

Days above 90°F (32°C) a year

28 → 54

About 2.0× as many

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.5°F (+0.8°C)
  • April: +1.9°F (+1.0°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.0°F (+1.1°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.3°F (+0.7°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.