Cargando…
Wave propagation in the marginal ice zone: connections and feedback mechanisms within the air–ice–ocean system
The propagation of ocean surface waves within the marginal ice zone (MIZ) is a defining phenomenon of this dynamic zone. Over decades of study, a variety of methods have been developed to observe and model wave propagation in the MIZ, with a common focus of determining the attenuation of waves with...
Autor principal: | Thomson, Jim |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
The Royal Society
2022
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9464515/ https://www.ncbi.nlm.nih.gov/pubmed/36088921 http://dx.doi.org/10.1098/rsta.2021.0251 |
Ejemplares similares
-
Floes, the marginal ice zone and coupled wave-sea-ice feedbacks
por: Horvat, Christopher
Publicado: (2022) -
Evidence for ice-ocean albedo feedback in the Arctic Ocean shifting to a seasonal ice zone
por: Kashiwase, Haruhiko, et al.
Publicado: (2017) -
Modelling wave-induced sea ice break-up in the marginal ice zone
por: Montiel, F., et al.
Publicado: (2017) -
Heavy footprints of upper-ocean eddies on weakened Arctic sea ice in marginal ice zones
por: Manucharyan, Georgy E., et al.
Publicado: (2022) -
Marginal ice zone dynamics
por: Squire, Vernon A.
Publicado: (2022)