ClimateSearch

Cabanatuan City, Central Luzon

Philippines · 344k people · 34 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)86°F (30°C)89°F (32°C)92°F (34°C)92°F (33°C)89°F (31°C)86°F (30°C)85°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)85°F (29°C)
Average low69°F (21°C)70°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)74°F (24°C)73°F (23°C)72°F (22°C)71°F (22°C)
Dew point67°F (20°C)67°F (20°C)69°F (21°C)71°F (22°C)74°F (24°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)69°F (21°C)
Rainfall1.2 in (32 mm)1.1 in (28 mm)1.3 in (34 mm)1.7 in (44 mm)8 in (202 mm)10.8 in (275 mm)16.4 in (418 mm)15.8 in (402 mm)13.9 in (352 mm)9 in (229 mm)4.1 in (104 mm)3.3 in (84 mm)
Rainy days4358212630302820108
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)
Sunshine319 h304 h355 h351 h327 h301 h262 h250 h257 h290 h296 h296 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

+1.7°F (+0.9°C)

Models range from +1.5°F (+0.9°C) to +1.9°F (+1.0°C)

Days above 90°F (32°C) a year

73 112

About 1.5× as many

Warming by month
  • January: +1.3°F (+0.7°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.6°F (+0.9°C)
  • April: +2.4°F (+1.3°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.1°F (+1.2°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.3°F (+0.7°C)
  • September: +1.7°F (+0.9°C)
  • October: +1.5°F (+0.8°C)
  • November: +1.3°F (+0.7°C)
  • December: +1.3°F (+0.7°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.