ClimateSearch

Inda Silasē, Tigray

Ethiopia · 100k people · 1910 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 high80°F (27°C)84°F (29°C)86°F (30°C)87°F (31°C)86°F (30°C)81°F (27°C)73°F (23°C)73°F (23°C)76°F (25°C)79°F (26°C)79°F (26°C)79°F (26°C)
Average low55°F (13°C)57°F (14°C)60°F (16°C)64°F (18°C)64°F (18°C)62°F (17°C)59°F (15°C)59°F (15°C)58°F (15°C)58°F (15°C)57°F (14°C)55°F (13°C)
Dew point39°F (4°C)37°F (3°C)38°F (3°C)42°F (5°C)47°F (8°C)55°F (13°C)60°F (16°C)61°F (16°C)58°F (15°C)49°F (10°C)44°F (6°C)40°F (5°C)
Rainfall0.1 in (2 mm)0 in (1 mm)0.3 in (8 mm)0.6 in (15 mm)2.3 in (58 mm)7.5 in (189 mm)15.7 in (400 mm)18.9 in (481 mm)9.1 in (231 mm)1.1 in (28 mm)0.3 in (7 mm)0 in (1 mm)
Rainy days0024920303120410
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)
Sunshine341 h311 h342 h346 h361 h329 h291 h279 h316 h348 h331 h339 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

+2.0°F (+1.1°C)

Models range from +1.9°F (+1.1°C) to +2.4°F (+1.3°C)

Days above 90°F (32°C) a year

10 20

About 1.9× as many

Warming by month
  • January: +1.8°F (+1.0°C)
  • February: +1.5°F (+0.8°C)
  • March: +2.0°F (+1.1°C)
  • April: +1.8°F (+1.0°C)
  • May: +2.2°F (+1.2°C)
  • June: +2.7°F (+1.5°C)
  • July: +2.0°F (+1.1°C)
  • August: +1.5°F (+0.8°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.1°F (+0.6°C)
  • November: +1.6°F (+0.9°C)
  • December: +1.6°F (+0.9°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.