ClimateSearch

Quezon, Northern Mindanao

Philippines · 115k people · 275 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 (34°C)91°F (33°C)90°F (32°C)89°F (31°C)89°F (31°C)89°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)
Average low71°F (22°C)71°F (22°C)71°F (22°C)72°F (22°C)73°F (23°C)73°F (23°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)
Dew point69°F (21°C)69°F (21°C)69°F (21°C)70°F (21°C)72°F (22°C)72°F (22°C)71°F (22°C)71°F (22°C)71°F (22°C)71°F (22°C)71°F (22°C)71°F (22°C)
Rainfall7 in (177 mm)5 in (126 mm)4.8 in (121 mm)6 in (152 mm)12.1 in (308 mm)12 in (305 mm)12.9 in (328 mm)11 in (279 mm)12 in (304 mm)10.5 in (267 mm)7.2 in (184 mm)5.9 in (151 mm)
Rainy days1189102022232021201411
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)
Sunshine145 h156 h191 h193 h158 h129 h128 h137 h129 h136 h145 h149 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 +1.1°F (+0.6°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

12 → 24

About 1.9× as many

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