ClimateSearch

Santa Rosa, Calabarzon

Philippines · 217k people · 9 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 high82°F (28°C)83°F (29°C)86°F (30°C)90°F (32°C)89°F (32°C)87°F (31°C)85°F (30°C)85°F (29°C)85°F (29°C)85°F (29°C)84°F (29°C)82°F (28°C)
Average low73°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)76°F (25°C)76°F (25°C)76°F (24°C)75°F (24°C)
Dew point69°F (21°C)69°F (21°C)70°F (21°C)73°F (23°C)75°F (24°C)76°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)74°F (24°C)73°F (23°C)72°F (22°C)
Rainfall1.8 in (47 mm)1.4 in (35 mm)2 in (52 mm)2.6 in (65 mm)9.7 in (246 mm)12.8 in (326 mm)18.8 in (477 mm)16 in (407 mm)16.5 in (420 mm)9.5 in (242 mm)4.8 in (121 mm)5.7 in (146 mm)
Rainy days868112227292928231512
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)
Sunshine316 h300 h351 h353 h337 h307 h273 h275 h265 h291 h296 h290 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

+0.9°F (+0.5°C)

Models range from −1.3°F (−0.7°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

35 58

About 1.6× as many

Warming by month
  • January: +1.0°F (+0.6°C)
  • February: +1.0°F (+0.6°C)
  • March: +1.0°F (+0.6°C)
  • April: +1.3°F (+0.7°C)
  • May: +1.2°F (+0.7°C)
  • June: +1.3°F (+0.7°C)
  • July: +0.8°F (+0.5°C)
  • August: +0.6°F (+0.4°C)
  • September: +1.2°F (+0.7°C)
  • October: +1.2°F (+0.6°C)
  • November: +1.1°F (+0.6°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.