Jove
Visualize
Contáctanos

Videos de Conceptos Relacionados

Travelling Waves01:04

Travelling Waves

5.5K
A wave is a disturbance that propagates from its source, repeating itself periodically, and is typically associated with simple harmonic motion. Mechanical waves are governed by Newton's laws and require a medium to travel. A medium is a substance in which a mechanical wave propagates, and the medium produces an elastic restoring force when it is deformed.
Water waves, sound waves, and seismic waves are some examples of mechanical waves. For water waves, the wave propagation medium is...
5.5K
The Wave Nature of Light02:12

The Wave Nature of Light

50.3K
The nature of light has been a subject of inquiry since antiquity. In the seventeenth century, Isaac Newton performed experiments with lenses and prisms and was able to demonstrate that white light consists of the individual colors of the rainbow combined together. Newton explained his optics findings in terms of a "corpuscular" view of light, in which light was composed of streams of extremely tiny particles traveling at high speeds according to Newton's laws of motion. 
50.3K
Shock Waves01:16

Shock Waves

2.2K
While deriving the Doppler formula for the observed frequency of a sound wave, it is assumed that the speed of sound in the medium is greater than the source's speed through it. When this condition is breached, a shock wave occurs.
When the source's speed approaches the speed of sound, constructive interference between successive wavefronts emitted by the source occurs immediately behind it. Initially, scientists believed that this constructive interference would result in such high...
2.2K
Wave Parameters01:10

Wave Parameters

8.0K
The simplest mechanical waves are associated with simple harmonic motion and repeat themselves for several cycles. These simple harmonic waves can be modeled using a combination of sine and cosine functions. Consider a simplified surface water wave that moves across the water's surface. Unlike complex ocean waves, in surface water waves, water moves vertically, oscillating up and down, whereas the disturbance of the wave moves horizontally through the medium. If a seagull is floating on the...
8.0K
Propagation of Waves01:07

Propagation of Waves

2.4K
When a wave propagates from one medium to another, part of it may get reflected in the first medium, and part of it may get transmitted to the second medium. In such a case, the interface of the two mediums can be considered as a boundary that is neither fixed nor free.
Consider a scenario where a wave propagates from a string of low linear mass density to a string of high linear mass density. In such a case, the reflected wave is out of phase with respect to the incident wave, however the...
2.4K
Kinetic and Potential Energy of a Wave01:10

Kinetic and Potential Energy of a Wave

4.0K
All forms of waves carry energy; this is directly visualized in nature. For instance, the waves of earthquakes are so intense that they can shake huge concrete buildings, causing them to fall. Loud sounds can damage nerve cells in the inner ear, causing permanent hearing loss. The waves of the oceans can erode beaches. 
In mechanical waves, the amount of energy is related to their amplitude and frequency. In the context of the above examples, large-amplitude earthquakes produce large...
4.0K

También podría leer

Artículos Relacionados

Artículos vinculados a este trabajo por autores compartidos, revista y gráfico de citas.

Ordenar por
Same author

Asymmetric and Intermittent Supershear Rupture Mediated by Local Fault Complexity during the 2025 <i>M<sub>W</sub></i> 7.7 Myanmar Earthquake.

Proceedings of the National Academy of Sciences of the United States of America·2026
Same author

Simple unilateral rupture of the great <i>M</i><sub>w</sub> 8.8 2025 Kamchatka earthquake.

Science (New York, N.Y.)·2026
Same author

How earthquakes organize stress.

Proceedings of the National Academy of Sciences of the United States of America·2026
Same author

Earthquakes in the blind spot.

Science (New York, N.Y.)·2025
Same author

Competition between roughness and strength for scale-dependent surfaces.

Physical review. E·2025
Same author

The big impact of small quakes on tectonic tremor synchronization.

Science advances·2025
JoVE
x logofacebook logolinkedin logoyoutube logo
ACERCA DE JoVE
Visión GeneralLiderazgoBlogCentro de Ayuda JoVE
AUTORES
Proceso de PublicaciónConsejo EditorialAlcance y PolíticasRevisión por ParesPreguntas FrecuentesEnviar
BIBLIOTECARIOS
TestimoniosSuscripcionesAccesoRecursosConsejo Asesor de BibliotecasPreguntas Frecuentes
INVESTIGACIÓN
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchivo
EDUCACIÓN
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualCentro de Recursos para ProfesoresSitio de Profesores
Términos y Condiciones de Uso
Política de Privacidad
Políticas

Video Experimental Relacionado

Updated: Sep 6, 2025

Measurements of Waves in a Wind-wave Tank Under Steady and Time-varying Wind Forcing
08:54

Measurements of Waves in a Wind-wave Tank Under Steady and Time-varying Wind Forcing

Published on: February 13, 2018

8.8K

La ola que sopló alrededor del mundo

Emily E Brodsky1, Thorne Lay1

  • 1Department of Earth and Planetary Sciences, University of California Santa Cruz, CA, USA.

Science (New York, N.Y.)
|June 30, 2022
PubMed
Resumen

La erupción de Tonga generó una ola atmosférica, causando tsunamis inusualmente rápidos. Esta investigación investiga la conexión entre las perturbaciones atmosféricas y la velocidad del tsunami.

Área de la Ciencia:

  • Ciencias atmosféricas
  • La oceanografía
  • La geofísica

Sus antecedentes:

  • La erupción de Tonga de 2022 generó olas atmosféricas significativas.
  • Los tsunamis suelen ser causados por la actividad sísmica, pero las perturbaciones atmosféricas también pueden influir en ellos.

Objetivo del estudio:

  • Analizar el impacto de las ondas atmosféricas de la erupción de Tonga en la generación y propagación de tsunamis.
  • Para entender la relación entre las características de las ondas atmosféricas y la velocidad del tsunami.

Principales métodos:

  • Análisis de datos sísmicos e infrasonidos de la erupción de Tonga.
  • Modelado de tsunamis utilizando datos de las ondas atmosféricas observadas.
  • Comparación de velocidades de tsunami modeladas con observaciones del mundo real.

Más Videos Relacionados

Shock Wave Application to Cell Cultures
05:39

Shock Wave Application to Cell Cultures

Published on: April 8, 2014

12.9K
Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System
08:19

Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System

Published on: May 9, 2021

2.3K

Videos de Experimentos Relacionados

Last Updated: Sep 6, 2025

Measurements of Waves in a Wind-wave Tank Under Steady and Time-varying Wind Forcing
08:54

Measurements of Waves in a Wind-wave Tank Under Steady and Time-varying Wind Forcing

Published on: February 13, 2018

8.8K
Shock Wave Application to Cell Cultures
05:39

Shock Wave Application to Cell Cultures

Published on: April 8, 2014

12.9K
Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System
08:19

Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System

Published on: May 9, 2021

2.3K

Principales resultados:

  • La ola atmosférica influyó significativamente en la dinámica del tsunami.
  • Los tsunamis generados o afectados por la onda atmosférica viajaron más rápido de lo normal.
  • Las velocidades de tsunami observadas se correlacionan con los parámetros de las olas atmosféricas.

Conclusiones:

  • Las ondas atmosféricas pueden conducir tsunamis más rápidos de lo normal.
  • La erupción de Tonga proporciona un estudio de caso para comprender las interacciones entre la atmósfera y el tsunami.
  • Se necesita más investigación para cuantificar completamente este fenómeno.