ClimateSearch

Tājūrā’, Tripoli

Libya · 100k people · 7 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 high62°F (16°C)63°F (17°C)68°F (20°C)73°F (23°C)79°F (26°C)85°F (29°C)88°F (31°C)90°F (32°C)87°F (31°C)81°F (27°C)72°F (22°C)64°F (18°C)
Average low51°F (11°C)51°F (11°C)54°F (12°C)58°F (15°C)64°F (18°C)69°F (21°C)73°F (23°C)75°F (24°C)74°F (23°C)69°F (20°C)60°F (16°C)54°F (12°C)
Dew point44°F (7°C)44°F (6°C)46°F (8°C)50°F (10°C)55°F (13°C)60°F (16°C)65°F (19°C)67°F (20°C)66°F (19°C)60°F (16°C)51°F (11°C)46°F (8°C)
Rainfall1.5 in (38 mm)1.2 in (31 mm)0.8 in (20 mm)0.5 in (12 mm)0.2 in (5 mm)0.1 in (1 mm)0 in (0 mm)0 in (1 mm)0.4 in (11 mm)0.7 in (19 mm)0.9 in (24 mm)1.2 in (31 mm)
Rainy days754211002456
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)
Sunshine279 h280 h331 h344 h374 h400 h411 h385 h347 h308 h278 h275 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 +1.9°F (+1.1°C) to +2.5°F (+1.4°C)

Days above 90°F (32°C) a year

42 68

About 1.6× as many

Warming by month
  • January: +1.9°F (+1.1°C)
  • February: +2.0°F (+1.1°C)
  • March: +1.8°F (+1.0°C)
  • April: +1.8°F (+1.0°C)
  • May: +1.5°F (+0.8°C)
  • June: +2.7°F (+1.5°C)
  • July: +2.1°F (+1.2°C)
  • August: +1.9°F (+1.1°C)
  • September: +2.6°F (+1.5°C)
  • October: +2.1°F (+1.2°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.