ClimateSearch

Santa Cruz, Calabarzon

Philippines · 108k 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 high81°F (27°C)82°F (28°C)84°F (29°C)88°F (31°C)89°F (32°C)87°F (31°C)86°F (30°C)86°F (30°C)85°F (30°C)85°F (29°C)83°F (28°C)81°F (27°C)
Average low74°F (23°C)73°F (23°C)75°F (24°C)77°F (25°C)78°F (26°C)78°F (25°C)77°F (25°C)77°F (25°C)77°F (25°C)76°F (25°C)76°F (24°C)75°F (24°C)
Dew point71°F (22°C)71°F (21°C)72°F (22°C)74°F (23°C)76°F (25°C)77°F (25°C)76°F (25°C)76°F (25°C)76°F (25°C)75°F (24°C)74°F (24°C)73°F (23°C)
Rainfall3.2 in (82 mm)2.7 in (68 mm)2.8 in (71 mm)2.5 in (62 mm)7.9 in (201 mm)10.5 in (268 mm)14.8 in (377 mm)12.4 in (316 mm)13.7 in (347 mm)9.5 in (242 mm)7.2 in (182 mm)9.7 in (247 mm)
Rainy days161313132227292828252322
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)
Sunshine308 h296 h346 h350 h341 h315 h283 h285 h274 h287 h287 h281 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 +1.5°F (+0.8°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

21 43

About 2.0× as many

Warming by month
  • January: +1.3°F (+0.7°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.4°F (+0.8°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.7°F (+1.0°C)
  • June: +1.9°F (+1.1°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.7°F (+0.9°C)
  • October: +1.5°F (+0.8°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.