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 high68°F (20°C)72°F (22°C)82°F (28°C)87°F (30°C)86°F (30°C)85°F (29°C)83°F (29°C)83°F (29°C)83°F (28°C)81°F (27°C)76°F (25°C)71°F (21°C)
Average low49°F (10°C)53°F (12°C)59°F (15°C)65°F (19°C)71°F (22°C)75°F (24°C)75°F (24°C)75°F (24°C)73°F (23°C)67°F (19°C)58°F (15°C)52°F (11°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)
Rainfall0.4 in (10 mm)0.5 in (13 mm)0.6 in (15 mm)1.6 in (42 mm)5 in (128 mm)12.7 in (321 mm)20.1 in (510 mm)14 in (357 mm)11.2 in (284 mm)2.9 in (74 mm)0.3 in (8 mm)0.2 in (4 mm)
Rainy days23391926303024811
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)
Sunshine299 h290 h338 h341 h341 h264 h211 h235 h260 h310 h292 h297 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.