Compound dry and hot extremes and their implications for fire activity over the Orinoco River Basin in northern South America
Compound dry and hot extremes (CDHE) have gained a pronounced relevance due to the observed increase in their frequency and the severity of their impacts on natural and human systems. The Orinoco River Basin, an ecoregion of great importance given its high biodiversity and the third largest river ba...
- Autores:
-
Arias Gómez, Paola Andrea
Fernández Berrío, Alejandra
Bedoya Pineda, Valeria
Acevedo Ortiz, Marley Yurani
Martínez Agudelo, John Alejandro
- Tipo de recurso:
- Article of investigation
- Fecha de publicación:
- 2025
- Institución:
- Universidad de Antioquia
- Repositorio:
- Repositorio UdeA
- Idioma:
- eng
- OAI Identifier:
- oai:bibliotecadigital.udea.edu.co:10495/45640
- Acceso en línea:
- https://hdl.handle.net/10495/45640
- Palabra clave:
- Ecosistemas fluviales
Water current biotic communities
Sequía
Drought
Incendio
Fires
Precipitación atmosférica
Precipitation
Déficit hídrico
Water shortages
Río Orinoco
http://aims.fao.org/aos/agrovoc/c_2391
http://aims.fao.org/aos/agrovoc/c_2915
http://aims.fao.org/aos/agrovoc/c_6161
http://aims.fao.org/aos/agrovoc/c_29112865
ODS 13: Acción por el Clima. Adoptar medidas urgentes para combatir el cambio climático y sus efectos
- Rights
- openAccess
- License
- http://creativecommons.org/licenses/by/4.0/
| Summary: | Compound dry and hot extremes (CDHE) have gained a pronounced relevance due to the observed increase in their frequency and the severity of their impacts on natural and human systems. The Orinoco River Basin, an ecoregion of great importance given its high biodiversity and the third largest river basin in South America, is vulnerable to these compound extremes because its extensive savannas are highly prone to fire activity. Here, we analyzed the occurrence of CDHE in this basin during the period 1981–2021. We compared different surface and atmospheric variables during drought periods (dry extremes) and CDHE (defined as periods with abnormally hot conditions during a meteorological drought event). Our results show that CDHE exhibit a larger precipitation deficit than dry extremes, exacerbating the meteorological drought. This stronger precipitation deficit is a response of weaker trade winds transporting moisture toward the region, in addition to stronger mid-tropospheric anticyclonic structures over the north Atlantic Ocean and the Caribbean Sea that advect dry air masses, inducing a deficit in total column water vapor and relative humidity at the mid-levels over the Orinoco. The moisture deficit during CDHE is also felt over the landmass, not only at surface but also deep soil layers, exacerbating the agricultural and ecological drought. Moreover, the decreased cloud cover associated with the enhanced precipitation deficit during CDHE increases the solar radiation reaching the surface, raising land temperature and reinforcing the drought impacts. Therefore, fire activity over the basin is enhanced during CDHE, increasing their associated burned area. This is very relevant since the savannas of the Orinoco are highly flammable and prone to fire, being burned with high frequency due to the practice of extensive livestock farming. |
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