ClimateSearch

Khardah, West Bengal

India · 128k people · 9 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 high78°F (26°C)85°F (30°C)92°F (33°C)97°F (36°C)97°F (36°C)94°F (35°C)91°F (33°C)91°F (33°C)91°F (33°C)90°F (32°C)86°F (30°C)80°F (27°C)
Average low55°F (13°C)62°F (17°C)70°F (21°C)76°F (25°C)79°F (26°C)80°F (27°C)80°F (26°C)80°F (27°C)79°F (26°C)76°F (24°C)66°F (19°C)58°F (14°C)
Dew point54°F (12°C)58°F (15°C)65°F (18°C)73°F (23°C)77°F (25°C)79°F (26°C)78°F (26°C)78°F (25°C)77°F (25°C)73°F (23°C)64°F (18°C)56°F (13°C)
Rainfall0.7 in (18 mm)0.7 in (18 mm)1 in (26 mm)2.1 in (54 mm)4.4 in (113 mm)11.7 in (298 mm)13.1 in (334 mm)13.1 in (332 mm)12 in (304 mm)6.6 in (168 mm)0.9 in (24 mm)0.2 in (4 mm)
Rainy days2224717212219911
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)
Sunshine258 h244 h278 h259 h231 h115 h85 h92 h115 h199 h229 h245 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 +0.8°F (+0.5°C) to +2.2°F (+1.2°C)

Days above 90°F (32°C) a year

108 → 130

About 1.2× as many

Warming by month
  • January: +0.5°F (+0.3°C)
  • February: +0.2°F (+0.1°C)
  • March: +0.8°F (+0.4°C)
  • April: +0.5°F (+0.3°C)
  • May: +0.5°F (+0.3°C)
  • June: +2.2°F (+1.2°C)
  • July: +0.8°F (+0.5°C)
  • August: +1.2°F (+0.7°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.1°F (+0.6°C)
  • November: +0.6°F (+0.4°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.