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Waves in fluids

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TLDR
One-dimensional waves in fluids as discussed by the authors were used to describe sound waves and water waves in the literature, as well as the internal wave and the water wave in fluids, and they can be classified into three classes: sound wave, water wave, and internal wave.
Abstract
Preface Prologue 1. Sound waves 2. One-dimensional waves in fluids 3. Water waves 4. Internal waves Epilogue Bibliography Notation list Author index Subject index.

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Book ChapterDOI

Inversion of Infrasound Signals for Passive Atmospheric Remote Sensing

TL;DR: In this paper, the authors review the early history of infrasound remote sensing, including basic geophysical remote sensing theory and linear acoustic wave propagation, and review the capabilities and limitations of current global atmospheric specification models used in propagation studies.
Journal ArticleDOI

Intrusive gravity currents and internal gravity wave generation in stratified fluid

TL;DR: In this article, the excitation of internal gravity waves by fluid intrusions that propagate along the interface between a uniform upper layer and a uniformly stratified lower layer is examined by way of laboratory experiments.
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Lower atmospheric anomalies following the 2008 Wenchuan Earthquake observed by GPS measurements

TL;DR: In this article, the lower atmospheric (tropospheric) variations are investigated using the total zenith tropospheric delay (ZTD) from GPS measurements around the Wenchuan earthquake.
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Swelling of a lava plug associated with a Vulcanian eruption at Sakurajima Volcano, Japan, as revealed by infrasound record: case study of the eruption on January 2, 2007

TL;DR: In order to clarify the time relation of the expansion of a gas pocket and failure of its overlying plug of lava during Vulcanian eruptions, infrasound records and video images of the Sakurajima volcano on January 2, 2007 were analyzed with respect to their origin times.
Journal ArticleDOI

Sea ice thickness measurement using episodic infragravity waves from distant storms

TL;DR: In this paper, small amplitude, long period waves (called infragravity waves) are used to measure ice thickness at basin scales by determining their travel time between measurement sites, the difference being a sensitive function of ice thickness.