ClimateSearch

Skardu, Gilgit-Baltistan

Pakistan · 260k people · 2240 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 high21°F (-6°C)26°F (-3°C)33°F (1°C)41°F (5°C)49°F (10°C)61°F (16°C)75°F (24°C)76°F (25°C)66°F (19°C)46°F (8°C)31°F (-1°C)23°F (-5°C)
Average low10°F (-12°C)15°F (-9°C)20°F (-7°C)25°F (-4°C)33°F (1°C)42°F (6°C)56°F (14°C)58°F (15°C)47°F (9°C)26°F (-3°C)14°F (-10°C)10°F (-12°C)
Dew point3°F (-16°C)10°F (-12°C)16°F (-9°C)23°F (-5°C)32°F (0°C)41°F (5°C)53°F (12°C)54°F (12°C)45°F (7°C)26°F (-4°C)11°F (-12°C)4°F (-15°C)
Rainfall2.8 in (71 mm)3.8 in (97 mm)4.1 in (105 mm)4.1 in (103 mm)3.6 in (92 mm)3.2 in (82 mm)5.6 in (143 mm)5 in (127 mm)4.2 in (108 mm)2.2 in (57 mm)2 in (50 mm)2.3 in (58 mm)
Rainy days13141514141117181611911
Snowfall20.8 in (52.9 cm)27.8 in (70.5 cm)29.9 in (75.9 cm)27.5 in (69.9 cm)19.1 in (48.4 cm)4.5 in (11.5 cm)0.7 in (1.7 cm)0.2 in (0.4 cm)5 in (12.7 cm)12.3 in (31.2 cm)13.8 in (35.1 cm)17.2 in (43.6 cm)
Sunshine236 h221 h286 h313 h383 h390 h392 h360 h335 h317 h258 h244 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

+3.4°F (+1.9°C)

Models range from +2.4°F (+1.3°C) to +4.7°F (+2.6°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +3.2°F (+1.8°C)
  • February: +2.3°F (+1.3°C)
  • March: +3.1°F (+1.7°C)
  • April: +2.0°F (+1.1°C)
  • May: +1.7°F (+0.9°C)
  • June: +2.3°F (+1.3°C)
  • July: +4.3°F (+2.4°C)
  • August: +3.6°F (+2.0°C)
  • September: +3.6°F (+2.0°C)
  • October: +3.4°F (+1.9°C)
  • November: +3.0°F (+1.7°C)
  • December: +3.0°F (+1.6°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.