ClimateSearch

San Jose, Mimaropa

Philippines · 143k people · 5 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)85°F (30°C)87°F (31°C)86°F (30°C)84°F (29°C)82°F (28°C)82°F (28°C)82°F (28°C)83°F (28°C)84°F (29°C)83°F (29°C)
Average low76°F (24°C)76°F (24°C)77°F (25°C)79°F (26°C)79°F (26°C)78°F (25°C)77°F (25°C)77°F (25°C)77°F (25°C)77°F (25°C)78°F (25°C)77°F (25°C)
Dew point70°F (21°C)70°F (21°C)71°F (22°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)75°F (24°C)74°F (23°C)72°F (22°C)
Rainfall1.7 in (43 mm)1.5 in (37 mm)1.4 in (36 mm)2 in (50 mm)7.9 in (202 mm)13.1 in (334 mm)21.9 in (556 mm)19 in (483 mm)17.5 in (444 mm)12.8 in (324 mm)5.5 in (139 mm)5.2 in (133 mm)
Rainy days86891925282827251612
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)
Sunshine325 h308 h356 h350 h334 h289 h252 h264 h255 h286 h298 h301 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 +1.4°F (+0.8°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

9 25

About 2.8× as many

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