ClimateSearch

El Obeid, North Kordofan

Sudan · 393k people · 571 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 high84°F (29°C)89°F (32°C)95°F (35°C)100°F (38°C)101°F (39°C)99°F (37°C)93°F (34°C)90°F (32°C)94°F (34°C)97°F (36°C)92°F (33°C)86°F (30°C)
Average low59°F (15°C)62°F (17°C)68°F (20°C)73°F (23°C)77°F (25°C)78°F (25°C)75°F (24°C)74°F (23°C)74°F (24°C)74°F (24°C)68°F (20°C)61°F (16°C)
Dew point30°F (-1°C)26°F (-3°C)23°F (-5°C)27°F (-3°C)44°F (7°C)60°F (16°C)67°F (19°C)68°F (20°C)66°F (19°C)52°F (11°C)37°F (3°C)35°F (1°C)
Rainfall0 in (0 mm)0 in (0 mm)0 in (0 mm)0 in (1 mm)0.4 in (10 mm)0.8 in (21 mm)2.3 in (59 mm)2.8 in (72 mm)1.6 in (40 mm)0.4 in (10 mm)0 in (0 mm)0 in (0 mm)
Rainy days00003613149200
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)
Sunshine340 h316 h365 h359 h364 h347 h339 h333 h334 h343 h330 h337 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

+1.9°F (+1.0°C)

Models range from +1.6°F (+0.9°C) to +2.4°F (+1.3°C)

Days above 90°F (32°C) a year

256 275

About 1.1× as many

Warming by month
  • January: +1.2°F (+0.6°C)
  • February: +1.3°F (+0.7°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.5°F (+1.4°C)
  • May: +1.9°F (+1.0°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.0°F (+1.1°C)
  • August: +1.5°F (+0.9°C)
  • September: +0.7°F (+0.4°C)
  • October: +0.1°F (+0.1°C)
  • November: +1.1°F (+0.6°C)
  • December: +1.2°F (+0.7°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.