ClimateSearch

Sonārgaon, Dhaka Division

Bangladesh · 130k people · 6 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 high77°F (25°C)83°F (28°C)89°F (32°C)92°F (33°C)91°F (33°C)89°F (32°C)89°F (31°C)89°F (32°C)90°F (32°C)89°F (32°C)85°F (30°C)79°F (26°C)
Average low54°F (12°C)59°F (15°C)68°F (20°C)74°F (23°C)76°F (25°C)78°F (26°C)79°F (26°C)79°F (26°C)79°F (26°C)76°F (24°C)67°F (19°C)58°F (14°C)
Dew point55°F (13°C)58°F (15°C)65°F (18°C)73°F (23°C)77°F (25°C)78°F (26°C)77°F (25°C)77°F (25°C)77°F (25°C)74°F (23°C)65°F (19°C)58°F (15°C)
Rainfall0.3 in (7 mm)0.6 in (16 mm)2.7 in (68 mm)5.5 in (141 mm)12.5 in (317 mm)15.7 in (398 mm)17.1 in (434 mm)12.2 in (309 mm)11.6 in (295 mm)7.6 in (192 mm)1 in (25 mm)0.4 in (10 mm)
Rainy days124916212221181111
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)
Sunshine252 h240 h271 h232 h182 h98 h82 h93 h116 h199 h234 h243 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

+1.0°F (+0.6°C)

Models range from +0.2°F (+0.1°C) to +1.5°F (+0.9°C)

Days above 90°F (32°C) a year

64 → 78

About 1.2× as many

Warming by month
  • January: +0.4°F (+0.2°C)
  • February: +0.0°F (+0.0°C)
  • March: +0.3°F (+0.1°C)
  • April: +0.0°F (+0.0°C)
  • May: +0.0°F (+0.0°C)
  • June: +1.2°F (+0.7°C)
  • July: +0.9°F (+0.5°C)
  • August: +1.0°F (+0.5°C)
  • September: +1.0°F (+0.6°C)
  • October: +1.1°F (+0.6°C)
  • November: +0.9°F (+0.5°C)
  • December: +0.4°F (+0.2°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.