ClimateSearch

Cebu City, Central Visayas

Philippines · 965k people · 43 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 high88°F (31°C)89°F (32°C)91°F (33°C)92°F (33°C)93°F (34°C)91°F (33°C)90°F (32°C)90°F (32°C)91°F (33°C)90°F (32°C)90°F (32°C)89°F (32°C)
Average low74°F (23°C)73°F (23°C)74°F (23°C)75°F (24°C)76°F (25°C)76°F (25°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)
Dew point73°F (23°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)
Rainfall4.6 in (116 mm)3.7 in (95 mm)3.1 in (79 mm)1.8 in (46 mm)4.3 in (110 mm)6.9 in (175 mm)8.2 in (209 mm)6.7 in (170 mm)7.6 in (194 mm)7.9 in (200 mm)7.1 in (180 mm)5.9 in (151 mm)
Rainy days8553915161314161211
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)
Sunshine170 h178 h218 h223 h198 h152 h134 h152 h136 h145 h160 h163 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 +0.5°F (+0.3°C) to +1.9°F (+1.0°C)

Days above 90°F (32°C) a year

—

Too few hot days today to project a reliable change

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