ClimateSearch

Al Miqdādīyah, Diyala

Iraq · 156k people · 61 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 high60°F (15°C)64°F (18°C)73°F (23°C)85°F (30°C)98°F (37°C)108°F (42°C)113°F (45°C)113°F (45°C)105°F (41°C)93°F (34°C)74°F (23°C)63°F (17°C)
Average low42°F (6°C)45°F (7°C)52°F (11°C)62°F (17°C)73°F (23°C)82°F (28°C)87°F (31°C)87°F (30°C)79°F (26°C)69°F (21°C)55°F (13°C)46°F (8°C)
Dew point40°F (4°C)40°F (4°C)40°F (5°C)43°F (6°C)41°F (5°C)39°F (4°C)42°F (6°C)43°F (6°C)41°F (5°C)41°F (5°C)43°F (6°C)41°F (5°C)
Rainfall2 in (50 mm)1.6 in (39 mm)1.7 in (43 mm)0.9 in (24 mm)0.2 in (6 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0.6 in (16 mm)1.6 in (41 mm)1.9 in (49 mm)
Rainy days765410000256
Snowfall0 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)0 in (0 cm)
Sunshine266 h265 h328 h337 h395 h415 h421 h386 h355 h323 h274 h262 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

+2.6°F (+1.4°C)

Models range from +2.3°F (+1.3°C) to +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

178 185

Roughly unchanged

Warming by month
  • January: +1.7°F (+1.0°C)
  • February: +1.2°F (+0.6°C)
  • March: +2.3°F (+1.3°C)
  • April: +2.3°F (+1.3°C)
  • May: +0.7°F (+0.4°C)
  • June: +2.7°F (+1.5°C)
  • July: +2.4°F (+1.4°C)
  • August: +2.6°F (+1.4°C)
  • September: +3.0°F (+1.7°C)
  • October: +2.1°F (+1.2°C)
  • November: +1.9°F (+1.1°C)
  • December: +2.6°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.