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 high91°F (33°C)91°F (33°C)93°F (34°C)94°F (34°C)93°F (34°C)91°F (33°C)90°F (32°C)91°F (33°C)91°F (33°C)92°F (33°C)92°F (33°C)92°F (33°C)
Average low74°F (23°C)73°F (23°C)74°F (23°C)74°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)74°F (24°C)74°F (23°C)74°F (24°C)74°F (24°C)74°F (23°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)
Rainfall4.2 in (106 mm)3.9 in (98 mm)4.7 in (120 mm)4.9 in (125 mm)8.6 in (217 mm)8.6 in (220 mm)8.9 in (226 mm)10.8 in (274 mm)7.2 in (183 mm)8.4 in (213 mm)6.4 in (162 mm)4.5 in (115 mm)
Rainy days999111819191916181410
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)
Sunshine170 h173 h204 h199 h162 h133 h139 h153 h146 h147 h154 h165 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.