ClimateSearch

Isulan, Soccsksargen

Philippines · 101k people · 68 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 (30°C)87°F (30°C)89°F (32°C)90°F (32°C)89°F (32°C)87°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)
Average low74°F (23°C)74°F (24°C)75°F (24°C)76°F (25°C)76°F (24°C)75°F (24°C)74°F (24°C)74°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)
Dew point72°F (22°C)71°F (22°C)71°F (22°C)72°F (22°C)74°F (23°C)74°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)
Rainfall5.5 in (139 mm)4 in (102 mm)4.9 in (125 mm)5.2 in (132 mm)9.2 in (234 mm)10.4 in (263 mm)10 in (254 mm)8.3 in (210 mm)8.4 in (213 mm)9.4 in (240 mm)6.9 in (176 mm)5.4 in (136 mm)
Rainy days181516192727272525262421
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)
Sunshine300 h292 h331 h321 h303 h276 h290 h302 h287 h290 h284 h298 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 +1.2°F (+0.7°C) to +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

47 93

About 2.0× as many

Warming by month
  • January: +1.8°F (+1.0°C)
  • February: +2.1°F (+1.1°C)
  • March: +1.8°F (+1.0°C)
  • April: +1.8°F (+1.0°C)
  • May: +1.7°F (+0.9°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.8°F (+1.0°C)
  • August: +2.1°F (+1.2°C)
  • September: +1.8°F (+1.0°C)
  • October: +2.1°F (+1.2°C)
  • November: +2.4°F (+1.3°C)
  • December: +2.1°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.