ClimateSearch

Zliten, Misratah

Libya · 204k people · 12 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 high63°F (17°C)65°F (18°C)70°F (21°C)76°F (24°C)82°F (28°C)88°F (31°C)92°F (33°C)92°F (34°C)89°F (32°C)83°F (28°C)73°F (23°C)65°F (19°C)
Average low50°F (10°C)50°F (10°C)53°F (12°C)57°F (14°C)62°F (17°C)68°F (20°C)72°F (22°C)73°F (23°C)72°F (22°C)67°F (20°C)59°F (15°C)53°F (11°C)
Dew point44°F (7°C)43°F (6°C)46°F (8°C)49°F (10°C)54°F (12°C)59°F (15°C)64°F (18°C)67°F (19°C)65°F (18°C)60°F (15°C)51°F (11°C)45°F (7°C)
Rainfall1 in (26 mm)0.8 in (19 mm)0.7 in (18 mm)0.4 in (9 mm)0.2 in (5 mm)0 in (1 mm)0 in (1 mm)0 in (1 mm)0.4 in (10 mm)0.7 in (17 mm)0.7 in (17 mm)0.9 in (23 mm)
Rainy days654210002345
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)
Sunshine286 h280 h334 h343 h373 h403 h415 h380 h347 h312 h279 h279 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

+2.3°F (+1.3°C)

Models range from +1.7°F (+1.0°C) to +2.4°F (+1.4°C)

Days above 90°F (32°C) a year

73 97

About 1.3× as many

Warming by month
  • January: +1.8°F (+1.0°C)
  • February: +2.0°F (+1.1°C)
  • March: +1.7°F (+0.9°C)
  • April: +1.9°F (+1.0°C)
  • May: +1.4°F (+0.8°C)
  • June: +2.7°F (+1.5°C)
  • July: +2.2°F (+1.2°C)
  • August: +1.9°F (+1.0°C)
  • September: +2.8°F (+1.5°C)
  • October: +2.4°F (+1.3°C)
  • November: +1.6°F (+0.9°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.