ClimateSearch

Angono, Calabarzon

Philippines · 135k 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 high84°F (29°C)85°F (30°C)88°F (31°C)92°F (33°C)92°F (33°C)90°F (32°C)87°F (31°C)87°F (30°C)87°F (30°C)87°F (30°C)86°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)75°F (24°C)75°F (24°C)74°F (23°C)
Dew point69°F (21°C)69°F (21°C)70°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 (37 mm)1.1 in (27 mm)1.2 in (30 mm)1.4 in (35 mm)6.5 in (165 mm)9.1 in (232 mm)16.1 in (409 mm)15.9 in (404 mm)14.6 in (372 mm)9.1 in (232 mm)6.1 in (154 mm)5.8 in (148 mm)
Rainy days22229152122211165
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 h121 h118 h122 h164 h188 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

+1.0°F (+0.6°C)

Models range from −1.2°F (−0.7°C) to +1.9°F (+1.1°C)

Days above 90°F (32°C) a year

30 → 55

About 1.8× as many

Warming by month
  • January: +1.1°F (+0.6°C)
  • February: +1.0°F (+0.6°C)
  • March: +1.0°F (+0.6°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.3°F (+0.7°C)
  • June: +1.4°F (+0.8°C)
  • July: +1.0°F (+0.5°C)
  • August: +0.6°F (+0.4°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.2°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.