ClimateSearch

Magugpo Poblacion, Davao Region

Philippines · 233k people · 25 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 high83°F (28°C)83°F (29°C)85°F (29°C)86°F (30°C)86°F (30°C)85°F (29°C)84°F (29°C)85°F (30°C)86°F (30°C)86°F (30°C)85°F (29°C)84°F (29°C)
Average low73°F (23°C)73°F (23°C)73°F (23°C)74°F (23°C)75°F (24°C)75°F (24°C)74°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)74°F (23°C)
Dew point71°F (22°C)70°F (21°C)71°F (21°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)
Rainfall6.4 in (162 mm)5.3 in (134 mm)4.4 in (112 mm)3.7 in (95 mm)5.9 in (151 mm)6.4 in (164 mm)4.4 in (112 mm)4.4 in (111 mm)4 in (102 mm)4.6 in (118 mm)4.9 in (125 mm)5.5 in (139 mm)
Rainy days191516162424211919222120
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)
Sunshine264 h265 h309 h308 h305 h268 h286 h300 h282 h289 h267 h270 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

+1.7°F (+0.9°C)

Models range from +1.0°F (+0.6°C) to +2.6°F (+1.4°C)

Days above 90°F (32°C) a year

9 23

About 2.7× as many

Warming by month
  • January: +1.7°F (+1.0°C)
  • February: +1.5°F (+0.8°C)
  • March: +1.9°F (+1.1°C)
  • April: +1.8°F (+1.0°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.8°F (+1.0°C)
  • August: +1.6°F (+0.9°C)
  • September: +1.6°F (+0.9°C)
  • October: +1.6°F (+0.9°C)
  • November: +1.8°F (+1.0°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.