ClimateSearch

Rosario, Calabarzon

Philippines · 128k 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 high82°F (28°C)84°F (29°C)86°F (30°C)89°F (32°C)89°F (32°C)88°F (31°C)86°F (30°C)86°F (30°C)85°F (30°C)85°F (29°C)84°F (29°C)83°F (28°C)
Average low74°F (23°C)74°F (23°C)75°F (24°C)77°F (25°C)78°F (26°C)78°F (26°C)77°F (25°C)77°F (25°C)77°F (25°C)76°F (25°C)76°F (25°C)75°F (24°C)
Dew point71°F (21°C)70°F (21°C)71°F (22°C)73°F (23°C)75°F (24°C)76°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)
Rainfall2 in (51 mm)1.8 in (46 mm)2.1 in (53 mm)2.1 in (53 mm)5.7 in (146 mm)8.8 in (224 mm)13.3 in (337 mm)10.6 in (269 mm)12.9 in (328 mm)9.4 in (240 mm)5.9 in (149 mm)7.1 in (181 mm)
Rainy days11810112125282627252017
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)
Sunshine314 h301 h350 h352 h344 h313 h283 h293 h278 h294 h294 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

+1.7°F (+0.9°C)

Models range from +1.6°F (+0.9°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

32 65

About 2.1× 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: +1.7°F (+1.0°C)
  • May: +1.8°F (+1.0°C)
  • June: +2.0°F (+1.1°C)
  • July: +1.5°F (+0.9°C)
  • August: +1.5°F (+0.8°C)
  • September: +1.8°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.