Sea-ice thermodynamics can determine waterbelt scenarios for Snowball Earth
<p>Snowball Earth refers to multiple periods in the Neoproterozoic during which geological evidence indicates that the Earth was largely covered in ice. A Snowball Earth results from a runaway ice–albedo feedback, but there is an ongoing debate about how the feedback stopped: with fully ice-co...
Main Authors: | J. Hörner, A. Voigt |
---|---|
Formato: | Artigo |
Idioma: | English |
Publicado: |
Copernicus Publications
2024-03-01
|
Series: | Earth System Dynamics |
Acceso en liña: | https://esd.copernicus.org/articles/15/215/2024/esd-15-215-2024.pdf |
Títulos similares
-
A conceptual model of oceanic heat transport in the Snowball Earth scenario
por: D. Comeau, et al.
Publicado: (2016-12-01) -
The Snowball Earth Episodes
por: Angelos Siozos, et al.
Publicado: (2023-08-01) -
The radiative feedback continuum from Snowball Earth to an ice-free hothouse
por: Ian Eisenman, et al.
Publicado: (2024-08-01) -
Resilience of Snowball Earth to Stochastic Events
por: Guillaume Chaverot, et al.
Publicado: (2024-07-01) -
Influence of Orbital Forcing on the Snowball Earth Deglaciation
por: Jiacheng Wu, et al.
Publicado: (2024-10-01)