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Preliminary results of the relation between ice viscosity and water content using an inverse method
Citation
Otero García, Jaime and Navarro Valero, Francisco Jose and Lapazaran Izargain, Javier Jesús (2013). Preliminary results of the relation between ice viscosity and water content using an inverse method. In: "Congreso de Métodos Numéricos en Ingeniería (CMN 2013)", 25/07/2013 - 28/07/2013, Bilbao, Spain. p. 773.
Description
| Title: | Preliminary results of the relation between ice viscosity and water content using an inverse method |
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| Author/s: |
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| Item Type: | Presentation at Congress or Conference (Other) |
| Event Title: | Congreso de Métodos Numéricos en Ingeniería (CMN 2013) |
| Event Dates: | 25/07/2013 - 28/07/2013 |
| Event Location: | Bilbao, Spain |
| Title of Book: | Congreso de Métodos Numéricos en Ingeniería (CMN 2013) |
| Date: | 2013 |
| Subjects: | |
| Faculty: | E.T.S.I. Telecomunicación (UPM) |
| Department: | Matemática Aplicada a las Tecnologías de la Información [hasta 2014] |
| Creative Commons Licenses: | Recognition - No derivative works - Non commercial |
Abstract
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.
More information
| Item ID: | 29665 |
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| DC Identifier: | https://oa.upm.es/29665/ |
| OAI Identifier: | oai:oa.upm.es:29665 |
| Deposited by: | Memoria Investigacion |
| Deposited on: | 19 Jul 2014 07:27 |
| Last Modified: | 22 Apr 2016 00:04 |
