ClimateSearch

Himamaylan, Western Visayas

Philippines · 117k 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 high87°F (31°C)88°F (31°C)91°F (33°C)92°F (34°C)92°F (33°C)90°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)89°F (31°C)
Average low73°F (23°C)73°F (23°C)74°F (23°C)76°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 point72°F (22°C)72°F (22°C)72°F (22°C)73°F (23°C)75°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 (23°C)
Rainfall3.2 in (81 mm)2.3 in (57 mm)3 in (76 mm)3.6 in (92 mm)7.8 in (197 mm)12.7 in (322 mm)16.7 in (425 mm)14.9 in (377 mm)13.8 in (351 mm)12.6 in (321 mm)7.8 in (199 mm)5.7 in (145 mm)
Rainy days65671623262324221410
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)
Sunshine183 h184 h223 h222 h181 h131 h116 h133 h119 h133 h164 h171 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 +1.6°F (+0.9°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

38 → 67

About 1.8× as many

Warming by month
  • January: +1.3°F (+0.7°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.4°F (+0.8°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.8°F (+1.0°C)
  • July: +1.5°F (+0.9°C)
  • August: +1.8°F (+1.0°C)
  • September: +1.7°F (+0.9°C)
  • October: +1.5°F (+0.9°C)
  • November: +1.5°F (+0.8°C)
  • December: +1.4°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.