ClimateSearch

Sātkhira, Khulna Division

Bangladesh · 129k 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 high76°F (25°C)83°F (28°C)90°F (32°C)93°F (34°C)92°F (34°C)89°F (32°C)87°F (31°C)87°F (31°C)87°F (31°C)86°F (30°C)83°F (28°C)78°F (25°C)
Average low57°F (14°C)63°F (17°C)71°F (22°C)77°F (25°C)80°F (27°C)80°F (27°C)79°F (26°C)79°F (26°C)78°F (26°C)75°F (24°C)67°F (19°C)60°F (15°C)
Dew point55°F (13°C)59°F (15°C)66°F (19°C)74°F (23°C)78°F (25°C)79°F (26°C)78°F (26°C)78°F (25°C)77°F (25°C)74°F (23°C)65°F (18°C)57°F (14°C)
Rainfall0.4 in (10 mm)0.8 in (20 mm)1.4 in (36 mm)3.8 in (97 mm)6.5 in (165 mm)11.5 in (291 mm)14.6 in (371 mm)11.8 in (299 mm)9.7 in (246 mm)5.4 in (137 mm)1.3 in (32 mm)0.5 in (13 mm)
Rainy days1351114232929251421
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)
Sunshine309 h295 h345 h337 h325 h243 h226 h239 h243 h285 h290 h298 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

+1.4°F (+0.8°C)

Models range from +0.6°F (+0.4°C) to +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

87 105

About 1.2× as many

Warming by month
  • January: +0.6°F (+0.4°C)
  • February: +0.5°F (+0.3°C)
  • March: +1.1°F (+0.6°C)
  • April: +0.9°F (+0.5°C)
  • May: +0.6°F (+0.4°C)
  • June: +2.2°F (+1.2°C)
  • July: +0.8°F (+0.4°C)
  • August: +1.2°F (+0.6°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.2°F (+0.6°C)
  • November: +0.9°F (+0.5°C)
  • December: +0.5°F (+0.3°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.