ClimateSearch

Tacurong, Soccsksargen

Philippines · 117k people · 50 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 (35°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 (33°C)92°F (33°C)
Average low74°F (23°C)74°F (23°C)74°F (23°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)75°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)
Dew point71°F (22°C)70°F (21°C)70°F (21°C)71°F (22°C)72°F (22°C)73°F (23°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)
Rainfall4.1 in (105 mm)3.7 in (95 mm)4.7 in (118 mm)4.6 in (117 mm)8.5 in (216 mm)8.9 in (226 mm)8.5 in (217 mm)11.4 in (290 mm)6.7 in (169 mm)7.9 in (200 mm)6.2 in (159 mm)4.5 in (115 mm)
Rainy days9911101819181915171511
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)
Sunshine165 h170 h202 h198 h160 h131 h137 h151 h144 h146 h151 h162 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

+1.9°F (+1.0°C)

Models range from +1.5°F (+0.8°C) to +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

26 → 73

About 2.8× as many

Warming by month
  • January: +1.8°F (+1.0°C)
  • February: +2.0°F (+1.1°C)
  • March: +2.0°F (+1.1°C)
  • April: +1.9°F (+1.1°C)
  • May: +1.9°F (+1.0°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.9°F (+1.0°C)
  • August: +2.1°F (+1.2°C)
  • September: +1.9°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.