ClimateSearch

Moro, Sindh

Pakistan · 143k people · 43 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 high74°F (23°C)79°F (26°C)90°F (32°C)101°F (39°C)110°F (43°C)111°F (44°C)105°F (41°C)101°F (38°C)100°F (38°C)96°F (36°C)86°F (30°C)77°F (25°C)
Average low50°F (10°C)54°F (12°C)63°F (17°C)74°F (23°C)81°F (27°C)85°F (30°C)85°F (30°C)82°F (28°C)79°F (26°C)72°F (22°C)61°F (16°C)53°F (12°C)
Dew point44°F (6°C)44°F (7°C)48°F (9°C)50°F (10°C)57°F (14°C)67°F (20°C)73°F (23°C)74°F (23°C)69°F (21°C)58°F (14°C)51°F (11°C)46°F (8°C)
Rainfall0.2 in (4 mm)0.1 in (3 mm)0.1 in (3 mm)0.1 in (4 mm)0.2 in (5 mm)0.3 in (8 mm)2 in (51 mm)2.6 in (65 mm)1 in (26 mm)0.1 in (3 mm)0.1 in (2 mm)0.1 in (3 mm)
Rainy days111122442100
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)
Sunshine315 h299 h337 h365 h394 h381 h365 h343 h327 h336 h306 h308 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 +1.3°F (+0.7°C) to +1.9°F (+1.0°C)

Days above 90°F (32°C) a year

231 233

Roughly unchanged

Warming by month
  • January: +0.9°F (+0.5°C)
  • February: +0.6°F (+0.3°C)
  • March: +0.8°F (+0.5°C)
  • April: +0.7°F (+0.4°C)
  • May: +1.2°F (+0.6°C)
  • June: +1.6°F (+0.9°C)
  • July: +2.3°F (+1.3°C)
  • August: +0.9°F (+0.5°C)
  • September: −0.7°F (−0.4°C)
  • October: −0.6°F (−0.4°C)
  • November: +0.6°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.