ClimateSearch

Koronadal, Soccsksargen

Philippines · 202k people · 54 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 high84°F (29°C)85°F (29°C)87°F (30°C)88°F (31°C)87°F (30°C)85°F (29°C)84°F (29°C)85°F (29°C)85°F (29°C)85°F (29°C)84°F (29°C)84°F (29°C)
Average low73°F (23°C)73°F (23°C)74°F (23°C)75°F (24°C)75°F (24°C)74°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)
Dew point72°F (22°C)71°F (22°C)71°F (22°C)72°F (22°C)74°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)
Rainfall5.3 in (134 mm)3.9 in (99 mm)4.4 in (112 mm)4.5 in (115 mm)7.8 in (197 mm)8.6 in (219 mm)8.2 in (208 mm)6.9 in (176 mm)7.2 in (182 mm)8.1 in (206 mm)5.9 in (149 mm)5 in (126 mm)
Rainy days171415162526262324262219
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)
Sunshine296 h289 h328 h319 h299 h272 h289 h302 h286 h291 h280 h295 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

+1.8°F (+1.0°C)

Models range from +1.3°F (+0.7°C) to +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

20 55

About 2.8× as many

Warming by month
  • January: +1.9°F (+1.0°C)
  • February: +2.2°F (+1.2°C)
  • March: +1.9°F (+1.1°C)
  • April: +2.0°F (+1.1°C)
  • May: +1.9°F (+1.1°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.9°F (+1.0°C)
  • August: +2.0°F (+1.1°C)
  • September: +1.8°F (+1.0°C)
  • October: +2.2°F (+1.2°C)
  • November: +2.4°F (+1.4°C)
  • December: +2.2°F (+1.2°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.