ClimateSearch

Kosti, White Nile

Sudan · 345k people · 386 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 high91°F (33°C)96°F (36°C)101°F (38°C)105°F (41°C)103°F (40°C)100°F (38°C)94°F (34°C)91°F (33°C)95°F (35°C)98°F (37°C)98°F (37°C)93°F (34°C)
Average low66°F (19°C)69°F (21°C)73°F (23°C)78°F (26°C)81°F (27°C)80°F (27°C)77°F (25°C)75°F (24°C)76°F (25°C)77°F (25°C)74°F (23°C)68°F (20°C)
Dew point37°F (3°C)34°F (1°C)30°F (-1°C)36°F (2°C)53°F (12°C)65°F (18°C)68°F (20°C)70°F (21°C)69°F (21°C)62°F (17°C)45°F (7°C)42°F (6°C)
Rainfall0 in (0 mm)0 in (0 mm)0 in (0 mm)0.1 in (2 mm)0.5 in (14 mm)0.8 in (21 mm)2.6 in (66 mm)2.6 in (67 mm)1.5 in (38 mm)0.6 in (16 mm)0 in (0 mm)0 in (0 mm)
Rainy days00014612139500
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)
Sunshine344 h325 h368 h358 h363 h340 h325 h319 h325 h338 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

+1.8°F (+1.0°C)

Models range from +1.5°F (+0.8°C) to +2.2°F (+1.2°C)

Days above 90°F (32°C) a year

313 323

Roughly unchanged

Warming by month
  • January: +1.0°F (+0.6°C)
  • February: +0.9°F (+0.5°C)
  • March: +1.6°F (+0.9°C)
  • April: +2.1°F (+1.2°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.3°F (+1.3°C)
  • July: +2.2°F (+1.2°C)
  • August: +1.0°F (+0.6°C)
  • September: +0.4°F (+0.2°C)
  • October: −0.2°F (−0.1°C)
  • November: +0.7°F (+0.4°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.