ClimateSearch

Banhā, Qalyubia

Egypt · 182k people · 21 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 high67°F (19°C)69°F (21°C)76°F (24°C)83°F (29°C)91°F (33°C)96°F (36°C)98°F (36°C)97°F (36°C)94°F (35°C)88°F (31°C)78°F (26°C)70°F (21°C)
Average low47°F (8°C)48°F (9°C)51°F (11°C)56°F (13°C)62°F (17°C)67°F (20°C)70°F (21°C)71°F (22°C)69°F (21°C)65°F (18°C)58°F (14°C)51°F (10°C)
Dew point41°F (5°C)41°F (5°C)43°F (6°C)46°F (8°C)51°F (11°C)57°F (14°C)63°F (17°C)65°F (18°C)62°F (16°C)57°F (14°C)51°F (11°C)44°F (7°C)
Rainfall0.2 in (5 mm)0.2 in (6 mm)0.2 in (5 mm)0.1 in (2 mm)0 in (1 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0.1 in (2 mm)0.1 in (3 mm)0.1 in (3 mm)
Rainy days221100000011
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)
Sunshine287 h273 h339 h348 h391 h409 h410 h370 h348 h330 h289 h281 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

+2.4°F (+1.4°C)

Models range from +2.0°F (+1.1°C) to +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

151 169

About 1.1× as many

Warming by month
  • January: +2.0°F (+1.1°C)
  • February: +1.6°F (+0.9°C)
  • March: +2.3°F (+1.3°C)
  • April: +2.0°F (+1.1°C)
  • May: +1.6°F (+0.9°C)
  • June: +2.4°F (+1.4°C)
  • July: +2.4°F (+1.3°C)
  • August: +2.5°F (+1.4°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.4°F (+1.3°C)
  • November: +2.0°F (+1.1°C)
  • December: +2.0°F (+1.1°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.