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 high85°F (29°C)86°F (30°C)89°F (31°C)91°F (33°C)89°F (32°C)86°F (30°C)85°F (29°C)85°F (29°C)85°F (29°C)85°F (29°C)86°F (30°C)85°F (30°C)
Average low74°F (23°C)74°F (23°C)74°F (24°C)76°F (25°C)77°F (25°C)76°F (25°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)
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)
Rainfall4.2 in (107 mm)4 in (103 mm)4.4 in (113 mm)4.8 in (123 mm)10.5 in (266 mm)14.6 in (371 mm)14.7 in (373 mm)12.2 in (309 mm)13.9 in (352 mm)12.4 in (315 mm)7.6 in (193 mm)7.1 in (179 mm)
Rainy days141112142528292729292220
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)
Sunshine310 h299 h347 h341 h326 h281 h268 h287 h261 h279 h291 h301 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.