The semi-humid tropical savanna climate is characterized for being between 24 and 27 °C (75.2 and 80.6 °F) with a variation in climate of two seasons; a rainy season and a dry season (produced by the trade winds from the northeast) each enduring a period of six months. Regions in Colombia with this climate characteristic are the Llanos (eastern plains), some section of the Caribbean plains near the coast, sections of the Magdalena and Cauca river valleys.
The steppe climate is characterized for having a very few vegetation limits and minimum precipitations and can also include the desert climate for a period of 5 months of dry season. This type of weather is characteristic of the plains of Bolívar and the northern Guajira (Serranía de Macuira), the central area of the Orinoquía region and the higher grounds of the Andes mountain range.
The tropical desert climate in Colombia is present in the Guajira and Tatacoa deserts characterized for their high temperatures and scarce precipitations. The trade winds from the northeast carry humidity from the oceans and without a mountain barrier nearby continue flowing without dropping any rainfall and eventually creating droughts.
Mountain climate is one of the unique features of the Andes, the Sierra Nevada de Santa Marta and other high altitude reliefs where climate is determined by elevation. These variations in climate depending on its altitude are called thermal floors (Spanish: Pisos termicos), a classification used in some countries but with variations in the classification of each floor.
Warm climate thermal floor
The warm thermal floor oscillate between sea level and 1,000 meters (3,281 ft) above sea level with a temperature over 24 °C (75.2 °F). Climate in this step is characterized for its similarities with the equatorial and tropical plains, heavy rains and high temperatures. Temperatures can reach over 29 °C (84.2 °F) as it is the case of the Magdalena river valley, which has many areas with jungles. This thermal floor is present in the cities like Santa Marta, Neiva, Cali and Cúcuta.
Representation of the "thermal Floors" present in a mountain climate.
Temperate climate thermal floor
Between 1,000 and 2,000 meters (3,281 and 6,562 ft) above sea level the temperature drops oscillating between 17 and 22 °C (62.6 and 71.6 °F) defining it as a temperate climate. Rainfall becomes variable at 1,700 meters (5,577 ft) above sea level and rains between 2,000 and 2,500 mm (78.7 and 98.4 in) . This climate is a characteristic in the cities like Pereira, Armenia, IbaguéPopayán and Medellín.
Cold climate thermal floor
The cold climate is present between 2,000 and 3,000 meters (6,562 and 9,843 ft) above sea level and is characterized for having Andean or cloud forests. This thermal floor is characterized for presenting an average temperature ranging between 10 and 17 °C (50.0 and 62.6 °F) while rainfall reaches a yearly average of 2,000 mm (78.7 in). The Colombian capital city Bogotá is located within this thermal floor. Other cities like San Juan de Pasto and Tunja are in this location.
Páramo climate thermal floor
The Páramo climate is present between 3,000 and 4,000 meters (9,843 and 13,123 ft) above sea level and the temperature is lower than 10 °C (50 °F) with icy winds, rare rainfall but frequent snowfall. Colombia has one of the largest páramo areas in the world; the Sumapaz Páramo located in central Colombia, over the Andean Cordillera Oriental branch. In Colombia páramos are further classified as subpáramo, páramo and superpáramo. Most of the rivers in Colombia are born here since páramos tend to hold water from precipitations and deglaciations coming from the peaks.
Glacial climate thermal floor
The glaciers in Colombia are located at 4,000 meters (13,123 ft) above sea level and up and with average temperatures ranging between 10 °C (50 °F) and less. Glaciers in Colombia began retreating in the 20th century due to global warming and are in danger of disappearing, if this occurs water supply would be scarce in the near future. Most of the glaciers are located in the Andes mountains and are inhabited by very few living species due to its severe weather.