ClimateSearch

Tarlac City, Central Luzon

Philippines · 402k people · 43 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 high85°F (29°C)87°F (30°C)90°F (32°C)93°F (34°C)92°F (33°C)89°F (31°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)85°F (29°C)
Average low69°F (20°C)69°F (21°C)71°F (22°C)75°F (24°C)76°F (25°C)76°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)72°F (22°C)71°F (21°C)
Dew point66°F (19°C)66°F (19°C)68°F (20°C)70°F (21°C)73°F (23°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)73°F (23°C)71°F (22°C)69°F (20°C)
Rainfall1 in (25 mm)0.9 in (23 mm)1.4 in (36 mm)1.9 in (47 mm)7 in (179 mm)9.1 in (230 mm)14 in (356 mm)13.5 in (342 mm)12 in (304 mm)7.2 in (182 mm)3.8 in (96 mm)2.7 in (70 mm)
Rainy days44710222629292820118
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)
Sunshine321 h306 h355 h350 h317 h286 h245 h227 h241 h288 h298 h301 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 (+0.9°C)

Models range from +1.0°F (+0.6°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

79 114

About 1.4× as many

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.3°F (+0.7°C)
  • March: +1.4°F (+0.8°C)
  • April: +2.2°F (+1.2°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.8°F (+1.0°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.5°F (+0.8°C)
  • September: +1.8°F (+1.0°C)
  • October: +1.5°F (+0.8°C)
  • November: +1.4°F (+0.8°C)
  • December: +1.5°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.