ClimateSearch

Narayanganj, Dhaka Division

Bangladesh · 224k people · 16 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 high75°F (24°C)81°F (27°C)89°F (32°C)90°F (32°C)89°F (32°C)88°F (31°C)86°F (30°C)87°F (30°C)87°F (31°C)86°F (30°C)82°F (28°C)77°F (25°C)
Average low57°F (14°C)62°F (17°C)70°F (21°C)76°F (24°C)78°F (26°C)79°F (26°C)79°F (26°C)78°F (26°C)78°F (25°C)75°F (24°C)67°F (19°C)60°F (15°C)
Dew point55°F (13°C)59°F (15°C)65°F (18°C)74°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)66°F (19°C)59°F (15°C)
Rainfall0.3 in (7 mm)0.8 in (19 mm)2.6 in (67 mm)6 in (153 mm)11.6 in (295 mm)13.3 in (339 mm)14.2 in (362 mm)11.1 in (281 mm)10.3 in (262 mm)5.6 in (142 mm)1.1 in (27 mm)0.3 in (9 mm)
Rainy days1361321263029251521
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)
Sunshine304 h291 h343 h320 h286 h228 h220 h237 h245 h284 h296 h299 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

58 70

About 1.2× as many

Warming by month
  • January: +0.4°F (+0.2°C)
  • February: +0.0°F (+0.0°C)
  • March: +0.2°F (+0.1°C)
  • April: +0.1°F (+0.0°C)
  • May: −0.1°F (+0.0°C)
  • June: +1.3°F (+0.7°C)
  • July: +0.8°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: +0.8°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.