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Variaciones naturales y antropogénicas en las fuentes de metano durante los últimos dos milenios
C J Sapart1, G Monteil, M Prokopiou
1Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Princetonplein 5, 3584CC Utrecht, The Netherlands. c.j.sapart@uu.nl
Nature
|October 6, 2012
Resumen
Los núcleos de hielo de Groenlandia revelan que las variaciones pasadas de metano fueron impulsadas por cambios climáticos naturales y actividades humanas. El análisis de isótopos ayuda a identificar estas fuentes en los últimos 2000 años.
Área de la Ciencia:
- Paleoclimatología Paleoclimatología
- Química de la atmósfera química de la atmósfera
- La geoquímica de los isótopos es la geoquímica de los isótopos.
Sus antecedentes:
- El metano (CH4) es un potente gas de efecto invernadero con diversas fuentes naturales y antropogénicas.
- Comprender las variaciones pasadas del metano atmosférico es crucial para el modelado climático.
- Las firmas isotópicas de las fuentes de metano ofrecen un método para rastrear sus orígenes.
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