ClimateSearch

Geylang, Singapore

110k people · 10 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 (30°C)87°F (31°C)88°F (31°C)88°F (31°C)89°F (32°C)89°F (31°C)88°F (31°C)88°F (31°C)88°F (31°C)88°F (31°C)87°F (30°C)86°F (30°C)
Average low74°F (23°C)74°F (24°C)75°F (24°C)75°F (24°C)76°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)74°F (24°C)
Dew point73°F (23°C)73°F (23°C)75°F (24°C)76°F (24°C)76°F (25°C)76°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)
Rainfall11.6 in (295 mm)6.9 in (176 mm)8.1 in (205 mm)8.7 in (220 mm)7.5 in (190 mm)7.7 in (195 mm)7 in (177 mm)6.8 in (172 mm)5.8 in (148 mm)7.7 in (195 mm)11.9 in (302 mm)14.5 in (368 mm)
Rainy days161116191716161514182422
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)
Sunshine145 h159 h181 h174 h177 h173 h180 h180 h172 h152 h112 h115 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

+2.1°F (+1.2°C)

Models range from +1.4°F (+0.8°C) to +3.6°F (+2.0°C)

Days above 90°F (32°C) a year

1 → 2

About 3.0× as many

Warming by month
  • January: +1.7°F (+0.9°C)
  • February: +1.9°F (+1.1°C)
  • March: +2.0°F (+1.1°C)
  • April: +2.2°F (+1.2°C)
  • May: +2.1°F (+1.1°C)
  • June: +1.9°F (+1.1°C)
  • July: +1.9°F (+1.1°C)
  • August: +2.3°F (+1.3°C)
  • September: +2.1°F (+1.1°C)
  • October: +2.5°F (+1.4°C)
  • November: +2.7°F (+1.5°C)
  • December: +2.1°F (+1.2°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.