ClimateSearch

Bacolod City, Western Visayas

Philippines · 455k people · 15 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)86°F (30°C)89°F (32°C)88°F (31°C)86°F (30°C)84°F (29°C)85°F (29°C)84°F (29°C)85°F (29°C)85°F (29°C)84°F (29°C)
Average low76°F (24°C)76°F (24°C)76°F (25°C)78°F (25°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)77°F (25°C)77°F (25°C)
Dew point73°F (23°C)73°F (23°C)73°F (23°C)75°F (24°C)76°F (24°C)76°F (25°C)76°F (24°C)76°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)74°F (24°C)
Rainfall7 in (179 mm)6 in (152 mm)5.2 in (133 mm)4.1 in (105 mm)8.3 in (210 mm)12.9 in (329 mm)14.1 in (357 mm)11.4 in (289 mm)11.2 in (286 mm)11.8 in (299 mm)9.7 in (248 mm)11.4 in (289 mm)
Rainy days201615152428292828292525
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)
Sunshine295 h291 h341 h341 h332 h289 h275 h295 h271 h282 h284 h285 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 (+1.0°C)

Models range from +1.7°F (+0.9°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

21 45

About 2.1× as many

Warming by month
  • January: +1.0°F (+0.6°C)
  • February: +1.0°F (+0.6°C)
  • March: +1.3°F (+0.7°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.8°F (+1.0°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.7°F (+1.0°C)
  • September: +1.6°F (+0.9°C)
  • October: +1.5°F (+0.9°C)
  • November: +1.4°F (+0.8°C)
  • December: +1.2°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.