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 high86°F (30°C)87°F (31°C)89°F (32°C)91°F (33°C)91°F (33°C)91°F (33°C)90°F (32°C)91°F (33°C)91°F (33°C)90°F (32°C)89°F (32°C)88°F (31°C)
Average low74°F (23°C)73°F (23°C)74°F (23°C)75°F (24°C)76°F (25°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 (24°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)
Rainfall14.2 in (360 mm)9.2 in (233 mm)7.3 in (185 mm)5.1 in (131 mm)7 in (178 mm)8.2 in (208 mm)9 in (228 mm)8.2 in (208 mm)7.4 in (187 mm)9.5 in (241 mm)9.6 in (244 mm)12.1 in (308 mm)
Rainy days14101091417171515181515
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)
Sunshine155 h166 h203 h210 h187 h146 h142 h154 h140 h148 h157 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

+1.6°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.