Travel time: Year-round
Nairobi sits at an elevation of approximately 1,795 meters (5,889 feet), which fundamentally dictates its weather. Unlike the sweltering tropical heat often associated with East Africa, Nairobi enjoys a subtropical highland climate. This altitude keeps the air crisp and the temperatures moderate throughout the year, earning it the nickname "The City of Cool Waters."
Nairobi’s weather follows a predictable diurnal pattern. Mornings are often brisk and occasionally misty, particularly between June and August. As the sun rises over the equator, the temperature climbs steadily, peaking in the mid-afternoon. Because of the high altitude, the sun feels significantly more intense than the thermometer suggests. Even on the hottest days, high humidity is rare; the heat is typically dry and sharp. Once the sun sets, the temperature drops rapidly. Locals often describe the climate as having "four seasons in one day," as you can transition from a chilly morning to a warm, sun-drenched afternoon and back to a cold night within twelve hours.
Nairobi does not have traditional spring, summer, autumn, or winter. Instead, the year is divided by rainfall patterns governed by the Intertropical Convergence Zone (ITCZ).
Nairobi’s topography creates distinct weather variations across the city. The western highlands (areas like Karen, Dagoretti, and Limuru) are significantly cooler and wetter due to higher elevation and denser vegetation. In contrast, the eastern and southern plains (near Jomo Kenyatta International Airport and the Embakasi area) are lower, flatter, and noticeably hotter and drier. The city center also experiences an "urban heat island" effect, where paved surfaces and dense buildings keep night temperatures a few degrees higher than the leafy suburbs.
Historically, Nairobi’s seasons were so regular that locals used the onset of the long rains to time their agricultural cycles. However, in recent decades, climate change has introduced more variability. The rains now occasionally "fail," leading to extended dry spells, or arrive with such intensity that they cause localized flash flooding.
One specific phenomenon is the August transition. Locals look for the "break" in the clouds toward the end of August; when the persistent grey veil finally lifts to reveal a deep blue sky, it signals the definitive end of the cold season. High-altitude winds are also common during the transition months (February and September), often bringing dust from the northern deserts before the rains wash the air clean.