ClimateSearch

Dharān, Koshi

Nepal · 173k people · 375 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 high73°F (23°C)78°F (25°C)86°F (30°C)89°F (32°C)90°F (32°C)89°F (32°C)88°F (31°C)89°F (31°C)88°F (31°C)87°F (31°C)82°F (28°C)75°F (24°C)
Average low51°F (10°C)55°F (13°C)63°F (17°C)71°F (22°C)74°F (24°C)77°F (25°C)78°F (25°C)77°F (25°C)75°F (24°C)70°F (21°C)61°F (16°C)53°F (12°C)
Dew point50°F (10°C)51°F (11°C)53°F (11°C)58°F (15°C)68°F (20°C)74°F (23°C)75°F (24°C)75°F (24°C)73°F (23°C)67°F (19°C)58°F (14°C)52°F (11°C)
Rainfall0.5 in (12 mm)0.6 in (15 mm)1.2 in (31 mm)2.5 in (65 mm)7.4 in (188 mm)11.2 in (283 mm)16.9 in (428 mm)11.9 in (302 mm)10.8 in (275 mm)4.6 in (116 mm)0.4 in (10 mm)0.3 in (8 mm)
Rainy days22461316211914511
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)
Sunshine234 h228 h269 h260 h244 h141 h81 h97 h144 h241 h242 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

+1.2°F (+0.7°C)

Models range from +1.2°F (+0.7°C) to +1.3°F (+0.7°C)

Days above 90°F (32°C) a year

17 → 19

About 1.1× as many

Warming by month
  • January: +1.3°F (+0.7°C)
  • February: +0.5°F (+0.3°C)
  • March: +0.3°F (+0.2°C)
  • April: −0.1°F (+0.0°C)
  • May: +1.0°F (+0.6°C)
  • June: +1.4°F (+0.8°C)
  • July: +0.9°F (+0.5°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.3°F (+0.7°C)
  • November: +1.1°F (+0.6°C)
  • December: +1.2°F (+0.6°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.