ClimateSearch

Manolo Fortich, Northern Mindanao

Philippines · 118k people · 512 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 high85°F (30°C)87°F (30°C)89°F (32°C)90°F (32°C)90°F (32°C)88°F (31°C)87°F (31°C)87°F (31°C)88°F (31°C)88°F (31°C)88°F (31°C)87°F (31°C)
Average low69°F (20°C)68°F (20°C)69°F (21°C)70°F (21°C)72°F (22°C)71°F (22°C)71°F (21°C)70°F (21°C)70°F (21°C)70°F (21°C)70°F (21°C)69°F (21°C)
Dew point68°F (20°C)67°F (20°C)67°F (20°C)69°F (20°C)70°F (21°C)70°F (21°C)69°F (21°C)69°F (21°C)69°F (21°C)69°F (21°C)69°F (21°C)69°F (20°C)
Rainfall5 in (126 mm)4 in (101 mm)5 in (127 mm)4.7 in (118 mm)11.2 in (285 mm)13.8 in (349 mm)14.4 in (366 mm)11.3 in (288 mm)11.4 in (289 mm)10.4 in (265 mm)8.2 in (208 mm)8 in (203 mm)
Rainy days12911112124242122221817
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)
Sunshine149 h159 h194 h198 h165 h133 h133 h142 h130 h138 h147 h153 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

+1.5°F (+0.9°C)

Models range from +1.2°F (+0.7°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

1 → 2

About 1.6× as many

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.7°F (+0.9°C)
  • March: +1.6°F (+0.9°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.5°F (+0.8°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.7°F (+0.9°C)
  • September: +1.6°F (+0.9°C)
  • October: +1.6°F (+0.9°C)
  • November: +1.5°F (+0.9°C)
  • December: +1.5°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.