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 high75°F (24°C)76°F (24°C)78°F (26°C)80°F (27°C)80°F (27°C)79°F (26°C)77°F (25°C)76°F (25°C)77°F (25°C)76°F (25°C)76°F (25°C)75°F (24°C)
Average low58°F (15°C)59°F (15°C)61°F (16°C)63°F (17°C)65°F (18°C)65°F (18°C)64°F (18°C)65°F (18°C)64°F (18°C)63°F (17°C)62°F (17°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)
Rainfall0.4 in (9 mm)0.4 in (11 mm)1.9 in (49 mm)3.5 in (89 mm)8.5 in (216 mm)11.2 in (285 mm)7.6 in (194 mm)26.3 in (668 mm)16.9 in (428 mm)8.6 in (218 mm)5.1 in (129 mm)1.8 in (47 mm)
Rainy days11510202320292613105
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)
Sunshine193 h185 h225 h224 h168 h145 h109 h95 h112 h154 h174 h168 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.