ClimateSearch

Pagadian, Zamboanga Peninsula

Philippines · 206k people · 41 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 high89°F (32°C)90°F (32°C)92°F (33°C)92°F (33°C)91°F (33°C)89°F (32°C)88°F (31°C)88°F (31°C)89°F (32°C)89°F (32°C)90°F (32°C)90°F (32°C)
Average low73°F (23°C)72°F (22°C)74°F (23°C)74°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)74°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)
Dew point73°F (23°C)72°F (22°C)73°F (23°C)74°F (23°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)75°F (24°C)74°F (23°C)
Rainfall4.9 in (124 mm)4.1 in (103 mm)5.6 in (142 mm)7.1 in (181 mm)11.1 in (282 mm)15.2 in (387 mm)14.8 in (375 mm)14.4 in (367 mm)14.5 in (368 mm)13.3 in (338 mm)12.2 in (309 mm)6.2 in (158 mm)
Rainy days868101923242322221711
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)
Sunshine163 h167 h202 h197 h153 h117 h121 h132 h122 h129 h144 h156 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

+1.0°F (+0.6°C)

Models range from −0.2°F (−0.1°C) to +1.6°F (+0.9°C)

Days above 90°F (32°C) a year

3 → 8

About 2.7× as many

Warming by month
  • January: +0.9°F (+0.5°C)
  • February: +1.3°F (+0.7°C)
  • March: +1.1°F (+0.6°C)
  • April: +1.1°F (+0.6°C)
  • May: +1.3°F (+0.7°C)
  • June: +1.1°F (+0.6°C)
  • July: +1.0°F (+0.6°C)
  • August: +1.0°F (+0.6°C)
  • September: +0.9°F (+0.5°C)
  • October: +1.2°F (+0.6°C)
  • November: +1.1°F (+0.6°C)
  • December: +1.0°F (+0.6°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.