ClimateSearch

Bagong Silangan, National Capital Region

Philippines · 107k people · 58 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 high82°F (28°C)84°F (29°C)87°F (31°C)91°F (33°C)90°F (32°C)87°F (30°C)84°F (29°C)84°F (29°C)84°F (29°C)85°F (29°C)84°F (29°C)83°F (28°C)
Average low72°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 (24°C)76°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)73°F (23°C)
Dew point69°F (20°C)68°F (20°C)70°F (21°C)72°F (22°C)74°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)73°F (23°C)71°F (21°C)
Rainfall1.3 in (33 mm)1.1 in (27 mm)1.3 in (33 mm)1.6 in (41 mm)7.9 in (201 mm)11.4 in (290 mm)18.4 in (468 mm)17.8 in (453 mm)16 in (407 mm)9.5 in (241 mm)4.1 in (105 mm)4.2 in (106 mm)
Rainy days4358202629302921108
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)
Sunshine318 h301 h351 h352 h334 h305 h267 h265 h261 h289 h295 h291 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

+0.9°F (+0.5°C)

Models range from −1.3°F (−0.7°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

42 61

About 1.4× as many

Warming by month
  • January: +0.9°F (+0.5°C)
  • February: +0.8°F (+0.5°C)
  • March: +1.0°F (+0.6°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.1°F (+0.6°C)
  • June: +1.3°F (+0.7°C)
  • July: +1.0°F (+0.5°C)
  • August: +0.6°F (+0.3°C)
  • September: +1.2°F (+0.7°C)
  • October: +1.0°F (+0.6°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.