ClimateSearch

Catbalogan, Eastern Visayas

Philippines · 108k people · 9 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)82°F (28°C)84°F (29°C)85°F (30°C)88°F (31°C)89°F (32°C)89°F (32°C)89°F (32°C)88°F (31°C)86°F (30°C)84°F (29°C)82°F (28°C)
Average low70°F (21°C)70°F (21°C)72°F (22°C)73°F (23°C)74°F (24°C)76°F (24°C)76°F (25°C)76°F (25°C)75°F (24°C)74°F (23°C)73°F (23°C)72°F (22°C)
Dew point72°F (22°C)71°F (22°C)72°F (22°C)74°F (23°C)75°F (24°C)76°F (24°C)76°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)
Rainfall17.7 in (449 mm)11.2 in (283 mm)9.5 in (241 mm)6.7 in (170 mm)9.5 in (240 mm)9 in (229 mm)11 in (280 mm)8.3 in (211 mm)10.4 in (263 mm)13.2 in (335 mm)15.4 in (391 mm)22.4 in (569 mm)
Rainy days171212101517201618211818
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)
Sunshine157 h171 h207 h219 h203 h150 h125 h133 h124 h139 h153 h146 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

+1.4°F (+0.8°C)

Models range from +0.6°F (+0.4°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

11 → 21

About 1.9× as many

Warming by month
  • January: +1.1°F (+0.6°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.2°F (+0.7°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.2°F (+0.7°C)
  • June: +1.5°F (+0.8°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.5°F (+0.8°C)
  • October: +1.4°F (+0.8°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.