ClimateSearch

Toledo, Central Visayas

Philippines · 207k people · 8 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 high81°F (27°C)82°F (28°C)83°F (28°C)85°F (30°C)86°F (30°C)85°F (30°C)85°F (29°C)85°F (29°C)85°F (29°C)84°F (29°C)83°F (28°C)82°F (28°C)
Average low76°F (24°C)76°F (24°C)76°F (24°C)77°F (25°C)79°F (26°C)78°F (26°C)78°F (26°C)78°F (26°C)78°F (26°C)78°F (25°C)77°F (25°C)77°F (25°C)
Dew point73°F (23°C)73°F (23°C)73°F (23°C)74°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)75°F (24°C)74°F (24°C)
Rainfall7.1 in (182 mm)6 in (152 mm)5.5 in (139 mm)4.8 in (121 mm)7 in (177 mm)9.9 in (251 mm)9.6 in (245 mm)6.5 in (165 mm)7.1 in (180 mm)9.7 in (248 mm)10.4 in (265 mm)10.8 in (275 mm)
Rainy days221920212627252123272627
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 h340 h341 h345 h307 h296 h314 h286 h294 h286 h291 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

1 5

About 3.4× as many

Warming by month
  • January: +1.5°F (+0.8°C)
  • February: +1.3°F (+0.7°C)
  • March: +1.5°F (+0.9°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.5°F (+0.8°C)
  • June: +1.5°F (+0.8°C)
  • July: +1.2°F (+0.7°C)
  • August: +1.5°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.