Ice-shelf vibrations modeled by a full 3-D elastic model

Forced ice-shelf vibration modeling is performed using a full 3-D finite-difference elastic model, which also takes into account sub-ice seawater flow. The sea water flow is described by the wave equation. Ice-shelf flexure therefore results from hydrostatic pressure perturbations in the sub-ice sea...

詳細記述

書誌詳細
出版年:Annals of Glaciology
第一著者: Yuri V. Konovalov
フォーマット: 論文
言語:英語
出版事項: Cambridge University Press 2019-09-01
主題:
オンライン・アクセス:https://www.cambridge.org/core/product/identifier/S0260305519000090/type/journal_article

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