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Contribución de los bosques semiáridos al sistema climático
1Environmental Sciences and Energy Research, Weizmann Institute of Science, Rehovot 76100, Israel.
Resumen
Los bosques secuestran carbono, ofreciendo un efecto de enfriamiento, pero esto es compensado por la radiación de calentamiento. La desertificación también afecta a la temperatura de la superficie de la Tierra, moderando las tendencias de calentamiento.
Área de la Ciencia:
- Ciencias del clima Ciencias del clima Ciencias del clima Ciencias del clima
- Ecología Forestal Ecología Forestal
- Ciencias del Sistema Terrestre Ciencias del Sistema Terrestre
Sus antecedentes:
- Los bosques influyen en la temperatura global a través del secuestro de carbono y la absorción de la radiación solar.
- Los efectos radiativos contrastantes (enfriamiento frente al calentamiento) complican los impactos forestales en el clima.
Objetivo del estudio:
- Investigar el efecto climático neto de los bosques en las zonas de línea de madera seca.
- Cuantificar el equilibrio entre el secuestro de carbono y el forzamiento radiativo en estos ecosistemas.
Principales métodos:
- Un estudio de 9 años en las zonas de bosque de línea de madera seca (200-600 mm de precipitación).
- Análisis de las tasas de secuestro de carbono y los efectos radiativos (albedo de onda corta y radiación de onda larga).
Principales resultados:
- Se produce un secuestro sustancial de carbono debido a los cambios en la actividad fotosintética a principios de la primavera.
- Este efecto de enfriamiento es contrarrestado por un efecto de calentamiento de la supresión de la radiación de onda larga.
- El efecto radiativo combinado de onda corta y onda larga duplica el impacto de albedo, lo que requiere décadas de acumulación de carbono para equilibrarse.
Conclusiones:
- Los bosques en las zonas de transición seca presentan un complejo ciclo de retroalimentación climática.
- La desertificación tiene un efecto forzante negativo significativo, moderando las tendencias de calentamiento.
- La acumulación de carbono a largo plazo es crucial para compensar los efectos de calentamiento inducidos por los bosques.
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