ClimateSearch

Kitale, Trans Nzoia

Kenya · 162k people · 1898 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 high81°F (27°C)82°F (28°C)81°F (27°C)77°F (25°C)75°F (24°C)74°F (23°C)73°F (23°C)73°F (23°C)75°F (24°C)76°F (24°C)76°F (24°C)78°F (26°C)
Average low52°F (11°C)53°F (12°C)54°F (12°C)55°F (13°C)55°F (13°C)53°F (12°C)53°F (12°C)53°F (11°C)52°F (11°C)53°F (12°C)53°F (12°C)53°F (12°C)
Dew point46°F (8°C)45°F (7°C)48°F (9°C)52°F (11°C)53°F (12°C)52°F (11°C)51°F (11°C)51°F (11°C)51°F (10°C)52°F (11°C)51°F (11°C)48°F (9°C)
Rainfall0.9 in (24 mm)1.3 in (33 mm)2.8 in (70 mm)6.5 in (165 mm)6 in (153 mm)4.6 in (117 mm)5.9 in (151 mm)6.4 in (163 mm)4 in (101 mm)3.6 in (92 mm)2.9 in (75 mm)1.9 in (48 mm)
Rainy days551019201819201516169
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)
Sunshine240 h222 h223 h164 h182 h175 h177 h183 h200 h186 h177 h223 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

+2.1°F (+1.2°C)

Models range from +1.5°F (+0.9°C) to +2.8°F (+1.5°C)

Days above 90°F (32°C) a year

0 → 0

Warming by month
  • January: +1.2°F (+0.7°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.1°F (+1.1°C)
  • May: +2.6°F (+1.4°C)
  • June: +2.4°F (+1.3°C)
  • July: +1.9°F (+1.0°C)
  • August: +1.9°F (+1.1°C)
  • September: +1.9°F (+1.1°C)
  • October: +1.3°F (+0.7°C)
  • November: +0.8°F (+0.5°C)
  • December: +1.5°F (+0.8°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.