Fires in Columbia and Venezuela ,17 March 2000

Fires in Columbia and Venezuela

17 March 2000

Several active fire signals in Venezuela and Columbia are recorded by NOAA/OSEI with the NOAA AVHRR Sensor on 15 March 2000.

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Fig.1. NOAA image of the vegetation fires in Venezuela and Columbia 15 March 2000
(Source: NOAA/OSEI)

The fires are currently burning in the Llanos of the Orinoco (Colombia and Venezuela). Although spread over most of the Llanos, an accumulation can be observed in two sub-regions: along the Meta river (covered by small clouds, in the center of the image above; Colombia) and north of Arauca (Venezuela).

The main vegetation type affected by the fires in this region is a mosaic of “savannah woodland and xeromorphic forest”, with patches of “lowland dense moist forest”. The forest ecosystem affected by the fires is far from being adapted to the burning practices and the soil degradation and erosion can be enhanced in the region.

Most of the fires in South America must been seen in the context of intensive land development. Fire is used as a tool in forest conversion. This is done by small farmers as well as large agro-industrial companies. The careless use of fire often allow the “prescribed” burnings to escape and become forest fires in the adjacent forests. These wildfires are of global importance because they threaten global biodiversity as well as the livelihood and cultural identity of the indigenous people in South America.

Almost all fires in the Venezuela and Columbia are human-caused, natural fires play a minor role in the tropical rain forest of South America. In the seasonally dry forests and bush formations (cerrado) lightning fires are observed occasionally.

Under normal weather conditions the primary forest in the humid tropics does not catch fire. The hydrological cycle in the closed forests produces a very humid microclimate where unfavourable conditions for forest fire exist. But in forests where selective logging already took place the former closed canopy is disturbed. This allows more light to penetrate through the canopy and thereby changing the energy balance within the forest – the forest becomes more susceptible to drought and consequently to fire.

For a detailed report on the fire activities in the region refer to the IFFN article “Fire Activity in the Guyana Shield, the Orinoco and Amazon Basins During March 1998

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