ClimateSearch

Tabuk, Cordillera

Philippines · 123k people · 138 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 high76°F (25°C)78°F (26°C)82°F (28°C)86°F (30°C)88°F (31°C)88°F (31°C)87°F (30°C)86°F (30°C)85°F (29°C)83°F (28°C)81°F (27°C)77°F (25°C)
Average low66°F (19°C)66°F (19°C)68°F (20°C)72°F (22°C)74°F (23°C)75°F (24°C)74°F (24°C)74°F (24°C)74°F (23°C)72°F (22°C)71°F (21°C)68°F (20°C)
Dew point66°F (19°C)67°F (19°C)68°F (20°C)71°F (22°C)73°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)74°F (23°C)72°F (22°C)70°F (21°C)68°F (20°C)
Rainfall6.7 in (170 mm)5.8 in (147 mm)4.4 in (111 mm)3.7 in (95 mm)10.7 in (272 mm)9.8 in (248 mm)11.7 in (297 mm)13.3 in (337 mm)10.7 in (271 mm)7.9 in (199 mm)8.9 in (225 mm)12.4 in (316 mm)
Rainy days211714121920222422191922
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)
Sunshine255 h253 h325 h338 h323 h314 h283 h267 h269 h279 h257 h221 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 +0.8°F (+0.4°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

21 41

About 1.9× as many

Warming by month
  • January: +1.1°F (+0.6°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.3°F (+0.7°C)
  • April: +1.8°F (+1.0°C)
  • May: +1.7°F (+0.9°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.3°F (+0.7°C)
  • August: +1.2°F (+0.7°C)
  • September: +1.5°F (+0.8°C)
  • October: +1.6°F (+0.9°C)
  • November: +1.3°F (+0.7°C)
  • December: +1.5°F (+0.9°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.