ClimateSearch

Ash Sharqāt, Salah ad Din

Iraq · 160k people · 164 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 high55°F (13°C)60°F (15°C)69°F (21°C)81°F (27°C)93°F (34°C)103°F (40°C)109°F (43°C)109°F (43°C)100°F (38°C)87°F (31°C)69°F (21°C)58°F (15°C)
Average low38°F (3°C)40°F (5°C)47°F (8°C)57°F (14°C)68°F (20°C)78°F (25°C)83°F (29°C)83°F (28°C)74°F (24°C)64°F (18°C)50°F (10°C)41°F (5°C)
Dew point38°F (4°C)39°F (4°C)41°F (5°C)43°F (6°C)42°F (6°C)40°F (5°C)44°F (7°C)45°F (7°C)42°F (6°C)42°F (6°C)42°F (6°C)40°F (4°C)
Rainfall1.8 in (45 mm)1.5 in (38 mm)1.5 in (39 mm)0.8 in (21 mm)0.3 in (9 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0.5 in (13 mm)1.1 in (29 mm)1.6 in (40 mm)
Rainy days876420000256
Snowfall0 in (0.1 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 cm)0 in (0 cm)0 in (0 cm)
Sunshine250 h262 h320 h339 h402 h416 h422 h394 h357 h317 h275 h245 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

+2.5°F (+1.4°C)

Models range from +2.4°F (+1.3°C) to +2.7°F (+1.5°C)

Days above 90°F (32°C) a year

159 166

Roughly unchanged

Warming by month
  • January: +2.1°F (+1.2°C)
  • February: +1.3°F (+0.7°C)
  • March: +2.7°F (+1.5°C)
  • April: +2.4°F (+1.3°C)
  • May: +0.8°F (+0.5°C)
  • June: +2.7°F (+1.5°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.5°F (+1.4°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.2°F (+1.2°C)
  • November: +1.5°F (+0.8°C)
  • December: +2.7°F (+1.5°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.