ClimateSearch

Taytay, Calabarzon

Philippines · 231k people · 7 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)91°F (33°C)93°F (34°C)93°F (34°C)91°F (33°C)89°F (31°C)88°F (31°C)88°F (31°C)88°F (31°C)88°F (31°C)86°F (30°C)
Average low72°F (22°C)72°F (22°C)74°F (23°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)75°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 (24°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)
Rainfall1.6 in (40 mm)1.2 in (30 mm)1.2 in (30 mm)1.4 in (36 mm)6.8 in (174 mm)9.8 in (250 mm)17.1 in (436 mm)16.9 in (430 mm)15.1 in (383 mm)9.4 in (238 mm)6 in (153 mm)5.9 in (151 mm)
Rainy days222210152222211266
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)
Sunshine214 h210 h251 h256 h206 h163 h122 h119 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

+0.9°F (+0.5°C)

Models range from −1.3°F (−0.7°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

42 → 65

About 1.5× as many

Warming by month
  • January: +1.0°F (+0.5°C)
  • February: +0.9°F (+0.5°C)
  • March: +1.0°F (+0.6°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.2°F (+0.7°C)
  • June: +1.2°F (+0.7°C)
  • July: +0.9°F (+0.5°C)
  • August: +0.6°F (+0.3°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.1°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.