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 high81°F (27°C)83°F (28°C)85°F (30°C)89°F (32°C)89°F (32°C)87°F (30°C)84°F (29°C)84°F (29°C)84°F (29°C)84°F (29°C)84°F (29°C)82°F (28°C)
Average low73°F (23°C)74°F (23°C)75°F (24°C)77°F (25°C)79°F (26°C)78°F (26°C)77°F (25°C)77°F (25°C)76°F (25°C)76°F (25°C)76°F (25°C)75°F (24°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)
Rainfall1.2 in (32 mm)0.8 in (20 mm)0.9 in (24 mm)0.8 in (20 mm)4.7 in (119 mm)6.8 in (172 mm)12.2 in (310 mm)11.5 in (292 mm)11.2 in (283 mm)6.5 in (165 mm)3.1 in (80 mm)4.2 in (107 mm)
Rainy days333415232728271798
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)
Sunshine316 h299 h350 h352 h335 h305 h267 h265 h259 h289 h295 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 +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.