ClimateSearch

La Trinidad, Cordillera

Philippines · 143k people · 1313 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 high71°F (21°C)72°F (22°C)74°F (23°C)75°F (24°C)75°F (24°C)74°F (23°C)73°F (23°C)72°F (22°C)72°F (22°C)73°F (23°C)73°F (23°C)71°F (22°C)
Average low59°F (15°C)59°F (15°C)60°F (16°C)62°F (17°C)64°F (18°C)64°F (18°C)63°F (17°C)64°F (18°C)63°F (17°C)62°F (17°C)62°F (16°C)60°F (16°C)
Dew point58°F (14°C)58°F (15°C)60°F (15°C)62°F (17°C)64°F (18°C)65°F (18°C)64°F (18°C)64°F (18°C)64°F (18°C)63°F (17°C)62°F (16°C)60°F (15°C)
Rainfall1.6 in (41 mm)2.2 in (56 mm)4 in (101 mm)6.5 in (165 mm)13.1 in (332 mm)15.6 in (397 mm)24.8 in (630 mm)24.7 in (628 mm)18 in (457 mm)13.3 in (339 mm)4.8 in (123 mm)3.4 in (85 mm)
Rainy days91116212729303029231411
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)
Sunshine303 h289 h343 h343 h312 h293 h254 h235 h252 h285 h284 h273 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 (+0.5°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

0 0

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