ClimateSearch

Sorsogon, Bicol Region

Philippines · 188k people · 11 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 high80°F (27°C)80°F (27°C)82°F (28°C)84°F (29°C)85°F (30°C)85°F (30°C)84°F (29°C)84°F (29°C)84°F (29°C)83°F (29°C)82°F (28°C)81°F (27°C)
Average low76°F (24°C)76°F (24°C)76°F (25°C)78°F (26°C)79°F (26°C)79°F (26°C)78°F (26°C)79°F (26°C)78°F (26°C)78°F (26°C)77°F (25°C)77°F (25°C)
Dew point72°F (22°C)72°F (22°C)73°F (23°C)75°F (24°C)76°F (25°C)77°F (25°C)76°F (25°C)76°F (25°C)76°F (25°C)76°F (24°C)75°F (24°C)74°F (24°C)
Rainfall11.5 in (292 mm)7.4 in (188 mm)6.3 in (160 mm)4 in (101 mm)5.6 in (143 mm)7.8 in (199 mm)10.2 in (260 mm)7.7 in (195 mm)8.8 in (224 mm)10.2 in (259 mm)11.4 in (291 mm)16.1 in (408 mm)
Rainy days262123202325282426272829
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)
Sunshine292 h293 h343 h345 h351 h317 h289 h293 h279 h291 h285 h282 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

+1.5°F (+0.8°C)

Models range from +1.2°F (+0.7°C) to +1.6°F (+0.9°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.5°F (+0.8°C)
  • March: +1.4°F (+0.8°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.3°F (+0.7°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.3°F (+0.7°C)
  • November: +1.3°F (+0.7°C)
  • December: +1.4°F (+0.8°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.