Surface water waves and tsunamis
devastating tsunami which followed, I have chosen the focus of my mini-course lectures at this year's PASI to be on two topics which involve the dynamics of surface water waves. These topics are of interest to mathematicians interested in wave propagation, and particularly to Chilean scientists...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.644.8142 2023-05-15T13:50:51+02:00 Surface water waves and tsunamis Walter Craig The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.644.8142 http://ms.mcmaster.ca/craig/PASI-VI-2_JDDE1133.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.644.8142 http://ms.mcmaster.ca/craig/PASI-VI-2_JDDE1133.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://ms.mcmaster.ca/craig/PASI-VI-2_JDDE1133.pdf text ftciteseerx 2016-01-08T16:07:33Z devastating tsunami which followed, I have chosen the focus of my mini-course lectures at this year's PASI to be on two topics which involve the dynamics of surface water waves. These topics are of interest to mathematicians interested in wave propagation, and particularly to Chilean scientists, I believe, because of Chile's presence on the tectonically active Pacic Rim. My rst lecture will describe the equations of uid dynamics for the free surface above a body of uid (the ocean surface), and the linearized equations of motion. From this we can predict the travel time of the recent tsunami from its epicenter o of the north Sumatra coast to the coast of nearby Thailand, the easy coasts of Sri Lanka and south India, and to Africa. In fact the signal given by ocean waves generated by the Sumatra earthquake was felt globally; within 48 hours distinguishable tsunami waves were measured by wave gages in Antarctica, Chile, Rio di Janeiro, the west coast of Mexico, the east coast of the United States, and at Halifax, Nova Scotia. To describe ocean waves we will formulate the full nonlinear uid dynamical Text Antarc* Antarctica Unknown |
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devastating tsunami which followed, I have chosen the focus of my mini-course lectures at this year's PASI to be on two topics which involve the dynamics of surface water waves. These topics are of interest to mathematicians interested in wave propagation, and particularly to Chilean scientists, I believe, because of Chile's presence on the tectonically active Pacic Rim. My rst lecture will describe the equations of uid dynamics for the free surface above a body of uid (the ocean surface), and the linearized equations of motion. From this we can predict the travel time of the recent tsunami from its epicenter o of the north Sumatra coast to the coast of nearby Thailand, the easy coasts of Sri Lanka and south India, and to Africa. In fact the signal given by ocean waves generated by the Sumatra earthquake was felt globally; within 48 hours distinguishable tsunami waves were measured by wave gages in Antarctica, Chile, Rio di Janeiro, the west coast of Mexico, the east coast of the United States, and at Halifax, Nova Scotia. To describe ocean waves we will formulate the full nonlinear uid dynamical |
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The Pennsylvania State University CiteSeerX Archives |
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Walter Craig |
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Walter Craig Surface water waves and tsunamis |
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Walter Craig |
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Walter Craig |
title |
Surface water waves and tsunamis |
title_short |
Surface water waves and tsunamis |
title_full |
Surface water waves and tsunamis |
title_fullStr |
Surface water waves and tsunamis |
title_full_unstemmed |
Surface water waves and tsunamis |
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surface water waves and tsunamis |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.644.8142 http://ms.mcmaster.ca/craig/PASI-VI-2_JDDE1133.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.644.8142 http://ms.mcmaster.ca/craig/PASI-VI-2_JDDE1133.pdf |
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