ClimateSearch

Norzagaray, Central Luzon

Philippines · 141k people · 42 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 high83°F (28°C)85°F (29°C)88°F (31°C)91°F (33°C)90°F (32°C)87°F (31°C)85°F (29°C)84°F (29°C)84°F (29°C)85°F (30°C)85°F (30°C)83°F (29°C)
Average low71°F (22°C)72°F (22°C)73°F (23°C)76°F (25°C)78°F (25°C)77°F (25°C)76°F (25°C)76°F (25°C)76°F (24°C)75°F (24°C)75°F (24°C)73°F (23°C)
Dew point68°F (20°C)68°F (20°C)69°F (21°C)72°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)73°F (23°C)70°F (21°C)
Rainfall1.4 in (36 mm)1.2 in (31 mm)1.5 in (39 mm)1.6 in (40 mm)7.5 in (192 mm)11 in (281 mm)16.4 in (417 mm)14.7 in (374 mm)13.4 in (340 mm)8.6 in (219 mm)4.3 in (110 mm)4.4 in (111 mm)
Rainy days4458202629302819119
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)
Sunshine316 h300 h350 h351 h331 h300 h260 h257 h255 h286 h292 h289 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

+1.1°F (+0.6°C)

Models range from −0.5°F (−0.3°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

50 70

About 1.4× as many

Warming by month
  • January: +1.0°F (+0.5°C)
  • February: +0.8°F (+0.5°C)
  • March: +0.9°F (+0.5°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.5°F (+0.9°C)
  • June: +1.5°F (+0.8°C)
  • July: +1.1°F (+0.6°C)
  • August: +0.6°F (+0.4°C)
  • September: +1.2°F (+0.7°C)
  • October: +1.2°F (+0.7°C)
  • November: +1.2°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.