The best time to visit Kenyan Coast

Kenya · scored for a beach trip

A view of the shoreline during the competition days. The Kenya Kite Cup is famously held in aid of Diani Turtl
A view of the shoreline during the competition days. The Kenya Kite Cup is famously held in aid of Diani Turtl © Lebu Ayiga, CC BY 4.0 · cropped and resized · Wikimedia Commons

Swahili trading towns and a reef-sheltered Indian Ocean shore, on the same two-rains pattern as the interior. The kenyan coast barely has a temperature season: daytime highs move only about 5 °C across the whole year, from 27 °C in July to 31 °C in February. What changes instead is rain.

Measured against a beach trip, the conditions hold up January to February and July to September. January is the most consistent single month: highs near 31 °C, nights around 25 °C, and roughly 20 mm of rain across the month.

The binding constraint here is rainfall — that is what rules months out, not any composite judgement. Rainfall is sharply seasonal: May averages 167 mm against 9 mm in February, so the wet season is the real planning constraint rather than heat or cold. April is the weakest month on these criteria.

March, December sit just outside the window — part of the month works and part does not. These are usually the interesting weeks: conditions are close to the peak-season answer while prices and crowds are not. The map lets you check them fortnight by fortnight rather than trusting a monthly average.

What the Kenyan coast is known for

Month by month

MonthHigh °CLow °CPrecip mmWet days
January3125204.6
February312593.3
March31256914.3
April302514625.9
May282416724.8
June272310922.1
July27235921.1
August27234919.3
September28236217.6
October28247918.6
November29248521.1
December30257115.5

Ticked rows are months where every hard requirement for a beach trip is met across at least half the month.

Open Kenyan Coast on the map →

Nearby regions

Figures are 30-year climatology sampled at Mombasa, Diani Beach, Watamu, Lamu and Malindi, averaged across those locations, from ERA5-Land reanalysis fitted with a harmonic seasonal cycle and a trend term, evaluated for 2026. Sampling named towns rather than averaging the whole region avoids blending valley and mountain conditions into a figure true of neither. Cells are about 0.08° wide, from ERA5-Land's 0.1° grid, which is itself driven by a 0.25° (~28 km) atmospheric reanalysis — so individual valleys, sheltered bays and single summits are not resolved. In steep terrain read these as conditions for the wider area rather than for one village. They describe typical conditions, not a forecast. Read how the climatology is built.