Magnetic Rossby waves in the stratified ocean of the core, and topographic core-mantle coupling
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- Braginsky Stanislav I.
- Institute of Geophysics and Planetary Physics, University of California Los Angeles
書誌事項
- タイトル別名
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- Magnetic Rossby waves in the stratified
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A new model of the stably stratified layer at the top of the core is proposed. The existence of a stably stratified layer (we name it the stratified ocean) at the top of the core makes possible the propagation of the waves akin to the Rossby waves (also named “planetary waves”), well known in oceanology and meteorology. These waves are modified and experience significant decay, due to the core's magnetic field. The “magnetic Rossby waves” are considered here, using a simple planar model, to reveal their qualitative features without going into significant mathematical complications. The core-mantle coupling, which originates from the interaction of the surface flow with the topography of the core-mantle boundary, is strongly influenced by the stably stratified layer. We consider the topographic core-mantle coupling arising due to generation of motion resembling the magnetic Rossby waves in the stably stratified layer. A simple expression is obtained for the topographic tangential stress on the core-mantle boundary.
収録刊行物
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- Earth, Planets and Space
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Earth, Planets and Space 50 (8), 641-649, 1998
地球電磁気・地球惑星圏学会 、公益社団法人 日本地震学会、特定非営利活動法人 日本火山学会、日本測地学会、日本惑星科学会
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詳細情報 詳細情報について
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- CRID
- 1390001206511484544
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- NII論文ID
- 10003735707
- 130003955923
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- NII書誌ID
- AA11211921
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- ISSN
- 18805981
- 13438832
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- NDL書誌ID
- 4573117
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- NDL
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