ClimateSearch

Errachidia, Drâa-Tafilalet

Morocco · 101k people · 1033 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 high58°F (14°C)62°F (17°C)69°F (21°C)77°F (25°C)84°F (29°C)93°F (34°C)101°F (38°C)98°F (37°C)89°F (32°C)78°F (25°C)66°F (19°C)59°F (15°C)
Average low36°F (2°C)39°F (4°C)45°F (7°C)52°F (11°C)59°F (15°C)67°F (20°C)73°F (23°C)73°F (23°C)65°F (18°C)56°F (13°C)45°F (7°C)38°F (4°C)
Dew point27°F (-3°C)28°F (-2°C)28°F (-2°C)31°F (-1°C)34°F (1°C)36°F (2°C)35°F (2°C)39°F (4°C)41°F (5°C)40°F (4°C)34°F (1°C)31°F (0°C)
Rainfall0.4 in (10 mm)0.5 in (13 mm)0.4 in (11 mm)0.4 in (10 mm)0.4 in (10 mm)0.2 in (5 mm)0.1 in (2 mm)0.1 in (3 mm)0.4 in (9 mm)0.8 in (21 mm)0.6 in (15 mm)0.3 in (7 mm)
Rainy days223221012322
Snowfall0.7 in (1.7 cm)0.6 in (1.4 cm)0 in (0.1 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 (0.1 cm)0.3 in (0.7 cm)
Sunshine296 h293 h340 h363 h387 h389 h392 h381 h344 h320 h289 h287 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

+2.8°F (+1.6°C)

Models range from +2.6°F (+1.4°C) to +3.3°F (+1.8°C)

Days above 90°F (32°C) a year

106 121

About 1.1× as many

Warming by month
  • January: +1.9°F (+1.1°C)
  • February: +3.2°F (+1.8°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.9°F (+1.6°C)
  • May: +2.4°F (+1.4°C)
  • June: +3.0°F (+1.7°C)
  • July: +2.9°F (+1.6°C)
  • August: +2.6°F (+1.5°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.6°F (+1.5°C)
  • November: +2.3°F (+1.3°C)
  • December: +2.2°F (+1.2°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.