Everything about Inertial wave
Inertial waves, also known as inertial oscillations, are a type of mechanical wave possible in rotating fluids. Unlike surface gravity waves commonly seen at the beach or in the bathtub, inertial waves flow through the interior of the fluid, not at the surface. Like any other kind of wave, an inertial wave is caused by a restoring force and characterized by its wavelength and frequency. Because the restoring force for inertial waves is the Coriolis force, their wavelengths and frequencies are related in a peculiar way. Inertial waves are transverse. Most commonly they are observed in atmospheres, oceans, lakes, and laboratory experiments. Rossby waves, geostrophic currents, and geostrophic winds are examples of inertial waves. Inertial waves are also likely to exist in the molten core of the rotating Earth. Wikipedia →
🧭 Start here: a 6-step reading path
- Read the overview: Inertial waveA 5-minute orientation
- Skim a recent paper: Bandgap merging and backward wave propagation in inertial amplification metamaterialsInfluential work since 2022
- Pick up a classic book: A Highrate Virtual Instrument Of Marine Vehicle Motions For Underwater Navigation And Ocean Remote SensingThe most-reprinted book on the subject
- Read the landmark paper: Detecting inertial effects with airborne matter-wave interferometryCited 380 times
- Go sideways: Rossby numberA closely related topic
- Go sideways: Coriolis forceA closely related topic
📖 Definitions
No dictionary entry for this exact phrase.
🗂️ The subject at a glance
🏆 Landmark papers (most cited)
Detecting inertial effects with airborne matter-wave interferometry
Near-Inertial Wave Propagation In Geostrophic Shear
Weak inertial-wave turbulence theory
Dual matter-wave inertial sensors in weightlessness
Wave‐driven inertial oscillations
Quantitative Experimental Observation of Weak Inertial-Wave Turbulence
Inertial Wave Turbulence Driven by Elliptical Instability
Generalized diffusion wave equation with inertial effects
🆕 Influential since 2022
Bandgap merging and backward wave propagation in inertial amplification metamaterials
Near-Inertial Wave Energetics Modulated by Background Flows in a Global Model Simulation
Multi-Axis Inertial Sensing with 2D Matter-Wave Arrays
Mechanical interactions modeling of inertial wave energy converters
New Regime of Inertial Alfvén Wave Turbulence in the Auroral Ionosphere
📚 Books worth reading
A Highrate Virtual Instrument Of Marine Vehicle Motions For Underwater Navigation And Ocean Remote SensingChrystel Gelin · 2012
Ranked by number of editions on Open Library, a rough measure of how lasting a book is.
🔗 Related topics
- Rossby number The Rossby number (Ro), named for Carl-Gustav Arvid Rossby, is a dimensionless number used in describing fluid flow. The Rossby number is the ratio of…
- Coriolis force In physics, the Coriolis force is a pseudo-force that acts on objects in motion within a frame of reference that rotates with respect to an inertial frame…
- Rotating reference frame A rotating frame of reference is a special case of a non-inertial reference frame that is rotating relative to an inertial reference frame. An everyday…
- Atmospheric circulation of exoplanets The atmospheric circulation on exoplanets refers to the large-scale movement of air masses on planets orbiting stars other than the Sun (exoplanets). This…
- Coriolis frequency The Coriolis frequency ƒ, also called the Coriolis parameter or Coriolis coefficient, is equal to twice the rotation rate Ω of the Earth multiplied by…
- Fictitious force A fictitious force, also known as an inertial force or pseudo-force, is a force that appears to act on an object when its motion is described or experienced…
- Topographic Rossby waves Topographic Rossby waves are geophysical waves that form due to bottom irregularities. For ocean dynamics, the bottom irregularities are on the ocean floor…
- Geostrophic current A geostrophic current is an oceanic current in which the pressure gradient force is balanced by the Coriolis effect. The direction of geostrophic flow…