ClimateSearch

Kadoma, Mashonaland West

Zimbabwe · 117k people · 1171 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 high81°F (27°C)81°F (27°C)81°F (27°C)80°F (27°C)77°F (25°C)73°F (23°C)73°F (23°C)80°F (26°C)87°F (30°C)89°F (32°C)86°F (30°C)82°F (28°C)
Average low66°F (19°C)65°F (19°C)64°F (18°C)61°F (16°C)56°F (14°C)52°F (11°C)51°F (11°C)55°F (13°C)61°F (16°C)65°F (18°C)67°F (19°C)66°F (19°C)
Dew point62°F (17°C)62°F (17°C)59°F (15°C)54°F (12°C)47°F (8°C)42°F (6°C)40°F (4°C)39°F (4°C)40°F (5°C)47°F (8°C)55°F (13°C)61°F (16°C)
Rainfall7 in (178 mm)5.1 in (130 mm)3 in (77 mm)1 in (24 mm)0.2 in (5 mm)0.1 in (2 mm)0 in (1 mm)0 in (0 mm)0.1 in (2 mm)0.9 in (23 mm)3.2 in (81 mm)7.2 in (182 mm)
Rainy days18141041000141220
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)
Sunshine337 h312 h342 h330 h331 h303 h315 h343 h350 h363 h345 h338 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

+1.9°F (+1.0°C)

Models range from +1.5°F (+0.9°C) to +2.2°F (+1.2°C)

Days above 90°F (32°C) a year

36 58

About 1.6× as many

Warming by month
  • January: +1.9°F (+1.1°C)
  • February: +1.3°F (+0.7°C)
  • March: +2.4°F (+1.3°C)
  • April: +2.8°F (+1.6°C)
  • May: +2.4°F (+1.3°C)
  • June: +2.5°F (+1.4°C)
  • July: +2.0°F (+1.1°C)
  • August: +2.0°F (+1.1°C)
  • September: +2.6°F (+1.4°C)
  • October: +3.2°F (+1.8°C)
  • November: +2.7°F (+1.5°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.