ClimateSearch

Midsayap, Soccsksargen

Philippines · 117k people · 21 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 high90°F (32°C)91°F (33°C)92°F (33°C)94°F (34°C)93°F (34°C)92°F (33°C)91°F (33°C)91°F (33°C)91°F (33°C)92°F (33°C)92°F (34°C)92°F (33°C)
Average low74°F (24°C)74°F (23°C)74°F (24°C)75°F (24°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)75°F (24°C)75°F (24°C)
Dew point72°F (22°C)71°F (22°C)71°F (22°C)72°F (22°C)74°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)
Rainfall5.4 in (138 mm)5.1 in (130 mm)6.1 in (154 mm)6 in (152 mm)11 in (278 mm)9.1 in (231 mm)7.5 in (190 mm)8 in (204 mm)7.4 in (189 mm)9.9 in (253 mm)7.9 in (201 mm)6.4 in (163 mm)
Rainy days101012132019151514181612
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)
Sunshine171 h176 h205 h199 h163 h133 h137 h149 h140 h145 h155 h167 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 (+1.0°C)

Models range from +1.4°F (+0.8°C) to +2.2°F (+1.2°C)

Days above 90°F (32°C) a year

76 → 129

About 1.7× as many

Warming by month
  • January: +1.5°F (+0.8°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.8°F (+1.0°C)
  • April: +1.7°F (+1.0°C)
  • May: +1.6°F (+0.9°C)
  • June: +1.7°F (+0.9°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.9°F (+1.1°C)
  • September: +1.7°F (+1.0°C)
  • October: +2.1°F (+1.2°C)
  • November: +1.9°F (+1.1°C)
  • December: +1.9°F (+1.0°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.