ClimateSearch

Gingoog, Northern Mindanao

Philippines · 139k people · 6 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 high84°F (29°C)85°F (29°C)87°F (30°C)89°F (32°C)89°F (32°C)88°F (31°C)87°F (31°C)88°F (31°C)88°F (31°C)87°F (31°C)86°F (30°C)86°F (30°C)
Average low75°F (24°C)75°F (24°C)75°F (24°C)76°F (25°C)78°F (26°C)78°F (25°C)77°F (25°C)78°F (25°C)78°F (25°C)77°F (25°C)76°F (25°C)76°F (25°C)
Dew point75°F (24°C)74°F (23°C)74°F (24°C)75°F (24°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)76°F (25°C)76°F (24°C)
Rainfall11.4 in (289 mm)9 in (230 mm)6.3 in (160 mm)6 in (154 mm)9.4 in (239 mm)12.7 in (324 mm)11 in (279 mm)9.1 in (232 mm)9.5 in (240 mm)10.7 in (271 mm)10 in (255 mm)9.5 in (241 mm)
Rainy days211817172527272425282423
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)
Sunshine280 h279 h328 h330 h333 h297 h300 h309 h286 h293 h284 h292 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

+1.6°F (+0.9°C)

Models range from +1.3°F (+0.7°C) to +2.2°F (+1.2°C)

Days above 90°F (32°C) a year

44 98

About 2.3× as many

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