ClimateSearch

Digri, Sindh

Pakistan · 235k people · 17 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 high76°F (25°C)82°F (28°C)92°F (33°C)101°F (38°C)105°F (41°C)104°F (40°C)98°F (37°C)95°F (35°C)96°F (36°C)96°F (36°C)88°F (31°C)79°F (26°C)
Average low52°F (11°C)56°F (13°C)65°F (18°C)73°F (23°C)79°F (26°C)82°F (28°C)82°F (28°C)80°F (26°C)77°F (25°C)72°F (22°C)63°F (17°C)54°F (12°C)
Dew point43°F (6°C)45°F (7°C)50°F (10°C)56°F (13°C)66°F (19°C)72°F (22°C)74°F (23°C)74°F (23°C)71°F (22°C)60°F (15°C)51°F (10°C)44°F (7°C)
Rainfall0.1 in (2 mm)0.1 in (2 mm)0 in (1 mm)0.1 in (2 mm)0.3 in (8 mm)0.3 in (8 mm)2.4 in (61 mm)2.9 in (74 mm)1.3 in (33 mm)0.3 in (9 mm)0 in (1 mm)0 in (1 mm)
Rainy days110111553100
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)
Sunshine323 h304 h338 h363 h394 h372 h321 h297 h319 h335 h304 h314 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

+1.6°F (+0.9°C)

Models range from +0.7°F (+0.4°C) to +2.3°F (+1.3°C)

Days above 90°F (32°C) a year

237 243

Roughly unchanged

Warming by month
  • January: +0.9°F (+0.5°C)
  • February: +0.8°F (+0.4°C)
  • March: +0.7°F (+0.4°C)
  • April: +0.7°F (+0.4°C)
  • May: +0.8°F (+0.5°C)
  • June: +1.1°F (+0.6°C)
  • July: +2.5°F (+1.4°C)
  • August: +1.2°F (+0.7°C)
  • September: +0.2°F (+0.1°C)
  • October: −0.2°F (−0.1°C)
  • November: +0.5°F (+0.3°C)
  • December: +1.1°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.