ClimateSearch

Roxas City, Western Visayas

Philippines · 185k people · 6 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 high80°F (27°C)81°F (27°C)82°F (28°C)85°F (29°C)86°F (30°C)85°F (30°C)85°F (29°C)85°F (30°C)85°F (29°C)83°F (29°C)83°F (28°C)81°F (27°C)
Average low76°F (24°C)75°F (24°C)76°F (25°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)77°F (25°C)77°F (25°C)77°F (25°C)
Dew point72°F (22°C)72°F (22°C)73°F (23°C)74°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)
Rainfall10.1 in (257 mm)7.4 in (188 mm)6.6 in (167 mm)4.2 in (106 mm)6.8 in (173 mm)9.7 in (246 mm)11.2 in (283 mm)8 in (203 mm)10.1 in (256 mm)11 in (280 mm)11.3 in (286 mm)16 in (408 mm)
Rainy days272122202627272526282829
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)
Sunshine293 h288 h342 h344 h343 h305 h288 h304 h283 h288 h286 h282 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

+1.4°F (+0.8°C)

Models range from +1.2°F (+0.7°C) to +1.5°F (+0.8°C)

Days above 90°F (32°C) a year

1 1

About 2.0× as many

Warming by month
  • January: +1.2°F (+0.7°C)
  • February: +1.1°F (+0.6°C)
  • March: +1.3°F (+0.7°C)
  • April: +1.2°F (+0.7°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.4°F (+0.8°C)
  • July: +1.3°F (+0.7°C)
  • August: +1.5°F (+0.8°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.1°F (+0.6°C)
  • November: +1.2°F (+0.7°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.