ClimateSearch

Chimoio, Manica

Mozambique · 422k people · 708 m elevation · Southern 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 high82°F (28°C)81°F (27°C)80°F (27°C)78°F (25°C)76°F (24°C)73°F (23°C)72°F (22°C)77°F (25°C)82°F (28°C)84°F (29°C)85°F (29°C)82°F (28°C)
Average low68°F (20°C)68°F (20°C)66°F (19°C)62°F (17°C)58°F (14°C)55°F (13°C)54°F (12°C)56°F (13°C)59°F (15°C)63°F (17°C)66°F (19°C)67°F (20°C)
Dew point67°F (20°C)67°F (20°C)66°F (19°C)62°F (16°C)56°F (13°C)52°F (11°C)50°F (10°C)51°F (11°C)54°F (12°C)59°F (15°C)63°F (17°C)66°F (19°C)
Rainfall7.8 in (199 mm)6.3 in (159 mm)5.2 in (131 mm)1.7 in (43 mm)0.6 in (15 mm)0.4 in (10 mm)0.4 in (10 mm)0.4 in (9 mm)0.6 in (15 mm)1.3 in (32 mm)3.5 in (90 mm)7.5 in (191 mm)
Rainy days21181694343471218
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)
Sunshine322 h295 h330 h316 h320 h298 h296 h320 h319 h337 h326 h321 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

+1.6°F (+0.9°C)

Models range from +0.8°F (+0.5°C) to +2.1°F (+1.2°C)

Days above 90°F (32°C) a year

23 38

About 1.6× as many

Warming by month
  • January: +1.5°F (+0.9°C)
  • February: +0.8°F (+0.5°C)
  • March: +1.7°F (+0.9°C)
  • April: +2.1°F (+1.2°C)
  • May: +1.8°F (+1.0°C)
  • June: +2.2°F (+1.2°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.9°F (+1.0°C)
  • September: +2.2°F (+1.2°C)
  • October: +2.8°F (+1.6°C)
  • November: +3.0°F (+1.7°C)
  • December: +2.3°F (+1.3°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.