ClimateSearch

Pulong Santa Cruz, Calabarzon

Philippines · 127k people · 48 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 high87°F (31°C)88°F (31°C)91°F (33°C)94°F (34°C)93°F (34°C)91°F (33°C)88°F (31°C)88°F (31°C)88°F (31°C)89°F (31°C)88°F (31°C)87°F (31°C)
Average low73°F (23°C)73°F (23°C)74°F (24°C)76°F (24°C)77°F (25°C)76°F (25°C)76°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)
Dew point69°F (21°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 (41 mm)0.9 in (24 mm)1.1 in (27 mm)1.4 in (34 mm)6.4 in (163 mm)9.6 in (244 mm)14.8 in (375 mm)13.4 in (340 mm)12.1 in (308 mm)8.8 in (223 mm)6.8 in (172 mm)6.3 in (159 mm)
Rainy days222313192423211487
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)
Sunshine207 h205 h245 h248 h201 h159 h122 h122 h122 h161 h182 h180 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

32 → 54

About 1.7× as many

Warming by month
  • January: +1.2°F (+0.7°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.3°F (+0.7°C)
  • April: +1.7°F (+0.9°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.2°F (+0.7°C)
  • August: +1.1°F (+0.6°C)
  • September: +1.7°F (+0.9°C)
  • October: +1.4°F (+0.8°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.