Increased methane emissions from deep osmotic and buoyant convection beneath submarine seeps as climate warms
Large methane hydrates reserves are found in mud volcanoes, but climate change may lead to methane release. Here, the authors show that methane adsorption creates overpressures leading to rapid recirculation of seawater, thus reducing the melting timescales of methane hydrates from millennia to deca...
Guardado en:
Autores principales: | Silvana S. S. Cardoso, Julyan H. E. Cartwright |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2016
|
Materias: | |
Acceso en línea: | https://doaj.org/article/9602382a500f44b1992b0fe70aa36914 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Conjugate buoyant convective transport of nanofluids in an enclosed annular geometry
por: M. Sankar, et al.
Publicado: (2021) -
Prompt rewetting of drained peatlands reduces climate warming despite methane emissions
por: Anke Günther, et al.
Publicado: (2020) -
Microbial communities of deep-sea methane seeps at Hikurangi continental margin (New Zealand).
por: S Emil Ruff, et al.
Publicado: (2013) -
Methane Seep Carbonates Host Distinct, Diverse, and Dynamic Microbial Assemblages
por: David H. Case, et al.
Publicado: (2015) -
Contrasting Pathways for Anaerobic Methane Oxidation in Gulf of Mexico Cold Seep Sediments
por: Adrien Vigneron, et al.
Publicado: (2019)