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 high65°F (18°C)66°F (19°C)72°F (22°C)77°F (25°C)82°F (28°C)87°F (31°C)91°F (33°C)92°F (34°C)90°F (32°C)86°F (30°C)77°F (25°C)68°F (20°C)
Average low50°F (10°C)50°F (10°C)54°F (12°C)58°F (14°C)63°F (17°C)69°F (21°C)74°F (23°C)75°F (24°C)73°F (23°C)68°F (20°C)60°F (15°C)52°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)
Rainfall2.1 in (52 mm)1.2 in (31 mm)0.7 in (18 mm)0.3 in (7 mm)0.1 in (3 mm)0 in (1 mm)0 in (0 mm)0 in (0 mm)0.4 in (9 mm)1.1 in (29 mm)0.9 in (24 mm)2 in (52 mm)
Rainy days753100001347
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)
Sunshine212 h211 h253 h265 h292 h339 h379 h335 h286 h236 h206 h204 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.