ClimateSearch

Rodriguez, Calabarzon

Philippines · 134k people · 188 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)83°F (28°C)85°F (30°C)89°F (32°C)89°F (31°C)86°F (30°C)84°F (29°C)83°F (29°C)84°F (29°C)84°F (29°C)83°F (29°C)81°F (27°C)
Average low71°F (22°C)71°F (22°C)73°F (23°C)75°F (24°C)77°F (25°C)76°F (25°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)73°F (23°C)
Dew point69°F (21°C)69°F (20°C)70°F (21°C)72°F (22°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)
Rainfall2 in (50 mm)1.7 in (42 mm)2 in (50 mm)2.2 in (56 mm)9.4 in (240 mm)13.2 in (334 mm)21.8 in (555 mm)22.1 in (562 mm)18.7 in (475 mm)10.9 in (276 mm)5.4 in (138 mm)5.9 in (149 mm)
Rainy days768102126303029221414
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)
Sunshine313 h297 h349 h351 h339 h313 h279 h278 h272 h288 h291 h283 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

+1.5°F (+0.8°C)

Models range from +0.9°F (+0.5°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

25 48

About 1.9× as many

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.3°F (+0.7°C)
  • March: +1.3°F (+0.7°C)
  • April: +1.7°F (+1.0°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.8°F (+1.0°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.2°F (+0.7°C)
  • September: +1.7°F (+1.0°C)
  • October: +1.5°F (+0.9°C)
  • November: +1.5°F (+0.8°C)
  • December: +1.6°F (+0.9°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.