ClimateSearch

Ţimā, Sohag

Egypt · 101k people · 64 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 high68°F (20°C)72°F (22°C)80°F (27°C)89°F (32°C)97°F (36°C)101°F (39°C)102°F (39°C)102°F (39°C)98°F (37°C)91°F (33°C)80°F (27°C)71°F (22°C)
Average low45°F (7°C)47°F (9°C)53°F (12°C)61°F (16°C)69°F (21°C)74°F (23°C)76°F (24°C)76°F (24°C)72°F (22°C)65°F (19°C)56°F (13°C)48°F (9°C)
Dew point36°F (2°C)35°F (2°C)35°F (2°C)35°F (2°C)39°F (4°C)44°F (7°C)48°F (9°C)50°F (10°C)50°F (10°C)48°F (9°C)44°F (7°C)39°F (4°C)
Rainfall0 in (1 mm)0 in (1 mm)0.1 in (2 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0 in (1 mm)0 in (0 mm)
Rainy days000000000000
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)
Sunshine303 h294 h357 h355 h389 h399 h398 h373 h353 h340 h314 h303 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

+2.6°F (+1.5°C)

Models range from +2.2°F (+1.2°C) to +3.2°F (+1.8°C)

Days above 90°F (32°C) a year

183 195

About 1.1× as many

Warming by month
  • January: +1.7°F (+1.0°C)
  • February: +1.5°F (+0.9°C)
  • March: +2.3°F (+1.3°C)
  • April: +1.9°F (+1.1°C)
  • May: +1.7°F (+1.0°C)
  • June: +2.6°F (+1.5°C)
  • July: +2.8°F (+1.5°C)
  • August: +2.6°F (+1.4°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.3°F (+1.3°C)
  • November: +1.6°F (+0.9°C)
  • December: +1.7°F (+1.0°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.