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 high73°F (23°C)74°F (24°C)74°F (23°C)71°F (22°C)69°F (21°C)67°F (19°C)65°F (19°C)66°F (19°C)68°F (20°C)69°F (21°C)69°F (21°C)71°F (22°C)
Average low53°F (12°C)54°F (12°C)54°F (12°C)55°F (13°C)54°F (12°C)53°F (11°C)51°F (11°C)51°F (11°C)52°F (11°C)53°F (12°C)53°F (11°C)52°F (11°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)
Rainfall2 in (51 mm)1.7 in (44 mm)3.6 in (92 mm)7.2 in (184 mm)8.2 in (207 mm)7.3 in (186 mm)6.4 in (162 mm)8.1 in (206 mm)6.2 in (157 mm)6 in (153 mm)5.3 in (136 mm)2.6 in (66 mm)
Rainy days7612202322222318201911
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)
Sunshine346 h321 h339 h287 h301 h289 h298 h300 h306 h310 h298 h330 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.