ClimateSearch

Ifakara, Morogoro

Tanzania · 206k people · 256 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 high88°F (31°C)87°F (30°C)86°F (30°C)84°F (29°C)83°F (28°C)81°F (27°C)80°F (27°C)81°F (27°C)84°F (29°C)87°F (30°C)90°F (32°C)89°F (32°C)
Average low75°F (24°C)74°F (23°C)73°F (23°C)72°F (22°C)69°F (21°C)66°F (19°C)63°F (17°C)66°F (19°C)69°F (20°C)72°F (22°C)75°F (24°C)75°F (24°C)
Dew point71°F (22°C)72°F (22°C)72°F (22°C)71°F (22°C)67°F (19°C)61°F (16°C)58°F (15°C)60°F (15°C)60°F (16°C)63°F (17°C)66°F (19°C)69°F (21°C)
Rainfall7.2 in (182 mm)6.1 in (155 mm)12.3 in (311 mm)14.2 in (360 mm)3.3 in (83 mm)0.6 in (15 mm)0.4 in (11 mm)0.2 in (5 mm)0.3 in (8 mm)1 in (25 mm)2.9 in (74 mm)5.8 in (148 mm)
Rainy days13122121711002511
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)
Sunshine188 h166 h161 h168 h219 h230 h236 h237 h242 h255 h238 h217 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

+1.7°F (+1.0°C)

Models range from +0.8°F (+0.5°C) to +3.2°F (+1.8°C)

Days above 90°F (32°C) a year

65 → 91

About 1.4× as many

Warming by month
  • January: +1.7°F (+1.0°C)
  • February: +1.7°F (+1.0°C)
  • March: +0.8°F (+0.4°C)
  • April: +1.7°F (+0.9°C)
  • May: +1.7°F (+1.0°C)
  • June: +1.9°F (+1.1°C)
  • July: +1.7°F (+1.0°C)
  • August: +1.8°F (+1.0°C)
  • September: +1.9°F (+1.1°C)
  • October: +2.1°F (+1.2°C)
  • November: +1.2°F (+0.7°C)
  • December: +1.8°F (+1.0°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.