ClimateSearch

Lipa City, Calabarzon

Philippines · 212k people · 321 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 high80°F (27°C)82°F (28°C)84°F (29°C)88°F (31°C)87°F (31°C)85°F (29°C)82°F (28°C)82°F (28°C)82°F (28°C)82°F (28°C)82°F (28°C)80°F (27°C)
Average low70°F (21°C)70°F (21°C)71°F (22°C)73°F (23°C)74°F (24°C)74°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)71°F (22°C)
Dew point67°F (20°C)67°F (19°C)68°F (20°C)70°F (21°C)72°F (22°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)71°F (22°C)69°F (21°C)
Rainfall1.7 in (43 mm)1.5 in (38 mm)1.8 in (46 mm)2 in (52 mm)6.8 in (172 mm)9.6 in (244 mm)15.2 in (387 mm)12.4 in (314 mm)13.9 in (354 mm)9.6 in (244 mm)5.1 in (130 mm)6.2 in (157 mm)
Rainy days979102126292727241714
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)
Sunshine315 h302 h351 h353 h343 h314 h282 h289 h275 h293 h294 h290 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

+1.3°F (+0.7°C)

Models range from +0.2°F (+0.1°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

13 28

About 2.1× as many

Warming by month
  • January: +1.1°F (+0.6°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.2°F (+0.7°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.3°F (+0.7°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.1°F (+0.6°C)
  • August: +1.1°F (+0.6°C)
  • September: +1.7°F (+0.9°C)
  • October: +1.4°F (+0.8°C)
  • November: +1.2°F (+0.6°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.