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Preliminary results of the relation between ice viscosity and water content using an inverse method
Cita
Otero García, Jaime 
ORCID: https://orcid.org/0000-0002-3518-7763, Navarro Valero, Francisco José ORCID: https://orcid.org/0000-0002-5147-0067 and Lapazaran Izargain, Javier Jesús ORCID: https://orcid.org/0000-0003-1820-4960
(2013).
Preliminary results of the relation between ice viscosity and water content using an inverse method.
En: "Congreso de Métodos Numéricos en Ingeniería (CMN 2013)", 25/07/2013 - 28/07/2013, Bilbao, Spain. p. 773.
ORCID: https://orcid.org/0000-0002-3518-7763, Navarro Valero, Francisco José ORCID: https://orcid.org/0000-0002-5147-0067 and Lapazaran Izargain, Javier Jesús ORCID: https://orcid.org/0000-0003-1820-4960
(2013).
Preliminary results of the relation between ice viscosity and water content using an inverse method.
En: "Congreso de Métodos Numéricos en Ingeniería (CMN 2013)", 25/07/2013 - 28/07/2013, Bilbao, Spain. p. 773.
Descripción
| Título: | Preliminary results of the relation between ice viscosity and water content using an inverse method |
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| Autor/es: |
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| Tipo de Documento: | Ponencia en Congreso o Jornada (Otro) |
| Título del Evento: | Congreso de Métodos Numéricos en Ingeniería (CMN 2013) |
| Fechas del Evento: | 25/07/2013 - 28/07/2013 |
| Lugar del Evento: | Bilbao, Spain |
| Título del Libro: | Congreso de Métodos Numéricos en Ingeniería (CMN 2013) |
| Fecha: | 2013 |
| Materias: | |
| ODS: | |
| Escuela: | E.T.S.I. Telecomunicación (UPM) |
| Departamento: | Matemática Aplicada a las Tecnologías de la Información [hasta 2014] |
| Licencias Creative Commons: | Reconocimiento - Sin obra derivada - No comercial |
Resumen
One of the outstanding problems of the modelling of temperate ice dynamics is the limited knowledge on the rheology of temperate ice and, in particular, on how the rate factor depends on the liquid water content. Though it is well known that the rate factor depends strongly on the water content, in practice the only available experimentally-based relationship is that by Duval (1977), which is only valid for water contents up to 1%. However, actual water contents found in temperate and polythermal glaciers are sometimes substantially larger.
Más información
| ID de Registro: | 29665 |
|---|---|
| Identificador DC: | https://oa.upm.es/29665/ |
| Identificador OAI: | oai:oa.upm.es:29665 |
| Depositado por: | Memoria Investigacion |
| Depositado el: | 19 Jul 2014 07:27 |
| Ultima Modificación: | 13 Abr 2023 18:14 |
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