ClimateSearch

Pātan, Bagmati Province

Nepal · 299k people · 1329 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 high63°F (17°C)68°F (20°C)75°F (24°C)81°F (27°C)83°F (29°C)84°F (29°C)82°F (28°C)82°F (28°C)81°F (27°C)79°F (26°C)72°F (22°C)66°F (19°C)
Average low38°F (4°C)42°F (6°C)49°F (10°C)56°F (13°C)62°F (17°C)67°F (19°C)68°F (20°C)68°F (20°C)66°F (19°C)58°F (14°C)48°F (9°C)41°F (5°C)
Dew point43°F (6°C)45°F (7°C)47°F (8°C)51°F (10°C)60°F (16°C)67°F (20°C)69°F (21°C)69°F (21°C)67°F (19°C)59°F (15°C)51°F (11°C)46°F (8°C)
Rainfall0.6 in (16 mm)0.9 in (23 mm)1.4 in (36 mm)2.7 in (68 mm)5.6 in (143 mm)10.5 in (266 mm)16.1 in (408 mm)15 in (382 mm)9.4 in (238 mm)2.5 in (63 mm)0.3 in (7 mm)0.4 in (11 mm)
Rainy days346111521282719612
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)
Sunshine215 h207 h250 h258 h250 h143 h62 h79 h130 h223 h215 h215 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

+1.5°F (+0.8°C)

Models range from +1.4°F (+0.8°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

0 → 0

Warming by month
  • January: +2.4°F (+1.4°C)
  • February: +1.5°F (+0.9°C)
  • March: +1.5°F (+0.9°C)
  • April: +1.1°F (+0.6°C)
  • May: +1.6°F (+0.9°C)
  • June: +1.9°F (+1.0°C)
  • July: +1.1°F (+0.6°C)
  • August: +1.5°F (+0.9°C)
  • September: +1.2°F (+0.7°C)
  • October: +1.6°F (+0.9°C)
  • November: +1.7°F (+1.0°C)
  • December: +1.9°F (+1.0°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.