ClimateSearch

NIA Valencia, Northern Mindanao

Philippines · 224k people · 311 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)92°F (33°C)90°F (32°C)89°F (31°C)89°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)
Average low71°F (21°C)70°F (21°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)71°F (22°C)71°F (22°C)
Dew point69°F (21°C)69°F (20°C)69°F (21°C)70°F (21°C)71°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)70°F (21°C)
Rainfall7.1 in (180 mm)4.8 in (123 mm)5 in (126 mm)5.7 in (145 mm)11.5 in (293 mm)12.4 in (314 mm)13.4 in (340 mm)11.3 in (286 mm)12.5 in (316 mm)10.7 in (271 mm)7.4 in (188 mm)6.1 in (155 mm)
Rainy days1189101922232022201311
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)
Sunshine133 h143 h179 h185 h152 h126 h123 h132 h123 h131 h138 h141 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 +0.9°F (+0.5°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

6 → 11

About 1.9× as many

Warming by month
  • January: +1.6°F (+0.9°C)
  • February: +1.6°F (+0.9°C)
  • March: +1.9°F (+1.0°C)
  • April: +1.6°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: +1.4°F (+0.8°C)
  • October: +1.7°F (+0.9°C)
  • November: +1.7°F (+0.9°C)
  • December: +1.5°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.