ClimateSearch

Mansilingan, Western Visayas

Philippines · 454k people · 43 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 high87°F (31°C)89°F (32°C)91°F (33°C)93°F (34°C)92°F (34°C)91°F (33°C)89°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)88°F (31°C)
Average low73°F (23°C)72°F (22°C)73°F (23°C)75°F (24°C)76°F (24°C)75°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)74°F (23°C)
Dew point73°F (23°C)73°F (23°C)73°F (23°C)74°F (24°C)76°F (24°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)
Rainfall5 in (128 mm)3.7 in (94 mm)4 in (101 mm)3.7 in (93 mm)8.3 in (211 mm)10.4 in (263 mm)14.5 in (369 mm)12.4 in (315 mm)11.3 in (287 mm)12.6 in (321 mm)10.1 in (258 mm)8.8 in (223 mm)
Rainy days106761620242221221614
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)
Sunshine172 h180 h221 h227 h192 h140 h123 h139 h128 h139 h161 h159 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 (+1.0°C)

Models range from +1.7°F (+0.9°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

18 → 37

About 2.1× as many

Warming by month
  • January: +1.1°F (+0.6°C)
  • February: +1.0°F (+0.6°C)
  • March: +1.3°F (+0.7°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.8°F (+1.0°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.8°F (+1.0°C)
  • September: +1.6°F (+0.9°C)
  • October: +1.5°F (+0.9°C)
  • November: +1.3°F (+0.7°C)
  • December: +1.2°F (+0.7°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.