ClimateSearch

Āsela, Oromiya

Ethiopia · 140k people · 2433 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 high69°F (21°C)71°F (22°C)72°F (22°C)71°F (21°C)69°F (21°C)66°F (19°C)63°F (17°C)63°F (17°C)64°F (18°C)67°F (19°C)68°F (20°C)69°F (20°C)
Average low47°F (8°C)48°F (9°C)51°F (11°C)52°F (11°C)51°F (11°C)51°F (11°C)51°F (11°C)51°F (11°C)50°F (10°C)49°F (10°C)47°F (8°C)46°F (8°C)
Dew point40°F (4°C)40°F (4°C)43°F (6°C)49°F (9°C)50°F (10°C)51°F (11°C)51°F (11°C)52°F (11°C)51°F (11°C)47°F (8°C)43°F (6°C)40°F (4°C)
Rainfall0.7 in (17 mm)1.1 in (27 mm)2.9 in (73 mm)5.6 in (142 mm)6.8 in (173 mm)5.4 in (138 mm)10.7 in (273 mm)14.8 in (377 mm)14.2 in (360 mm)4.7 in (119 mm)0.8 in (22 mm)0.4 in (10 mm)
Rainy days45101719233030281443
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)
Sunshine337 h310 h337 h329 h345 h317 h300 h309 h320 h350 h341 h342 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 (+1.3°C)

Models range from +2.2°F (+1.2°C) to +2.6°F (+1.5°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +1.6°F (+0.9°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.7°F (+1.0°C)
  • April: +1.5°F (+0.9°C)
  • May: +2.1°F (+1.2°C)
  • June: +2.7°F (+1.5°C)
  • July: +2.4°F (+1.4°C)
  • August: +2.1°F (+1.1°C)
  • September: +1.5°F (+0.8°C)
  • October: +1.3°F (+0.7°C)
  • November: +1.6°F (+0.9°C)
  • December: +1.8°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.