Climate of Venezuela
Venezuela’s climate is mainly tropical and warm because the country is near the Equator. But the landscape—coasts, plains, and especially tall mountains—creates a wide range of climates. Latitude matters less than altitude and terrain in shaping the weather across the country.
Hot and cold spots
- Coastal and lowland areas can be very hot, often over 38–42 C on hot days (examples: Maracaibo, Paraguaná, Porlamar).
- Cooler valleys, such as those in Caracas, Mérida, Los Teques, and San Cristóbal, are milder, usually in the 15–25 C range.
- The highest towns, like Mucuchíes and Apartaderos, have cold or tundra-like conditions, and the highest peaks can see frost or snow.
Temperature ranges by region
- Northwest and highlands: very hot at low elevations, cooler as you climb.
- Coastal Range and Guiana Highlands: average temperatures from about 11–25 C depending on elevation.
- Llanos (the plains): typically warm, averaging above 23 C.
- The hottest ever recorded in the country is about 42 C (Machiques); the coldest reported temperatures are around −11 C on very high, uninhabited mountaintops.
Climate types (simplified)
- The most common climate is warm and tropical with rain most of the year, and a distinct dry period in many areas.
- Lowland and coastal zones often have a pronounced wet season and a dry stretch, with annual rainfall generally ranging from about 600 to 1,500 mm.
- Higher elevations (guiana highlands foothills, coastal ranges) are cooler and wetter, with more variable rainfall.
- The montane regions (Cordillera de Mérida, Sierra de Perijá) are cooler and can be quite wet, with microclimates that vary with altitude.
- Páramo climate: on the highest peaks (roughly above 3,000 m), it is very cold year-round, with mean temperatures around 2–10 C and frost possible; Apartaderos is a well-known example.
- Desert-like and semi-arid zones exist in some northern coastal areas (like parts of Guajira and Paraguana) with relatively low rainfall.
In short, Venezuela blends tropical warmth with a striking variety of climates shaped by elevation and geography—from hot coasts and plains to cool valleys and cold, high-mountain regions.
This page was last edited on 3 February 2026, at 14:40 (CET).