ClimateSearch

Silang, Calabarzon

Philippines · 119k people · 330 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)89°F (31°C)86°F (30°C)84°F (29°C)84°F (29°C)84°F (29°C)84°F (29°C)84°F (29°C)83°F (28°C)
Average low70°F (21°C)69°F (21°C)71°F (22°C)72°F (22°C)73°F (23°C)73°F (23°C)72°F (22°C)73°F (23°C)72°F (22°C)72°F (22°C)72°F (22°C)71°F (22°C)
Dew point67°F (19°C)67°F (19°C)68°F (20°C)70°F (21°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)71°F (22°C)69°F (21°C)
Rainfall2.2 in (56 mm)1.5 in (38 mm)1.5 in (38 mm)1.7 in (44 mm)7.9 in (201 mm)10.2 in (260 mm)18.6 in (471 mm)15.6 in (397 mm)13.5 in (343 mm)7.6 in (194 mm)7 in (177 mm)7 in (179 mm)
Rainy days333415192524231398
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)
Sunshine206 h204 h244 h247 h200 h159 h121 h122 h121 h160 h181 h179 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

+1.3°F (+0.7°C)

Models range from +0.2°F (+0.1°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

10 → 22

About 2.2× as many

Warming by month
  • January: +1.2°F (+0.7°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.2°F (+0.7°C)
  • April: +1.8°F (+1.0°C)
  • May: +1.2°F (+0.7°C)
  • June: +1.5°F (+0.8°C)
  • July: +1.2°F (+0.7°C)
  • August: +1.2°F (+0.6°C)
  • September: +1.6°F (+0.9°C)
  • October: +1.3°F (+0.7°C)
  • November: +1.2°F (+0.7°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.