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What does the Rossby radius of deformation tell us?

By Matthew Harrington

What does the Rossby radius of deformation tell us?

The radius of deformation gives us the length scale at which the geostrophic balance (between the Coriolis and the horizontal pressure gradient forces) will become important.

What causes Rossby waves?

Rossby waves, also known as planetary waves, naturally occur in rotating fluids. Within the Earth’s ocean and atmosphere, these waves form as a result of the rotation of the planet. Oceanic and atmospheric Rossby waves — also known as planetary waves — naturally occur largely due to the Earth’s rotation.

How is Rossby number calculated?

The only way to combine the three variables U with dimensions of length/time), L (with dimensions of length), and f (with dimensions of 1/length) is U/fL, which is one form of what is called the Rossby number.

What is the difference between baroclinic and barotropic?

As adjectives the difference between baroclinic and barotropic. is that baroclinic is describing an atmospheric system in which the isobars are at an angle to the isopycnals or isotherms while barotropic is (meteorology) in which the pressure of the atmosphere is dependent upon its density only.

What are Rossby waves in the atmosphere?

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What are Rossby waves in meteorology?

Rossby wave, in meteorology, large horizontal atmospheric undulation that is associated with the polar-front jet stream and separates cold polar air from warm tropical air. These waves are named for Carl-Gustaf Arvid Rossby, who first identified them and explained their movement.

What is the meaning of Rossby number?

A dimensionless number relating the ratio of inertial to Coriolis forces for a given flow of a rotating fluid. Explicitly, the Rossby number is. where U is the velocity scale, f is the Coriolis parameter, and L is the horizontal length scale.

What is Cyclostrophic balance?

The balance of the horizontal pressure gradient and centrifugal forces is called cyclostrophic balance – cyclo meaning “cyclone” or low-pressure system and strophic meaning “turning.” In other words, this balance describes situations in which the turning of the wind, not the Earth, is the dominant effect.

What is a baroclinic system?

Baroclinic Zone A region in which a temperature gradient exists on a constant pressure surface. Baroclinic zones are favored areas for strengthening and weakening systems; barotropic systems, on the other hand, do not exhibit significant changes in intensity. Also, wind shear is characteristic of a baroclinic zone.

What is baroclinic and barotropic atmosphere?

In meteorology a baroclinic flow is one in which the density depends on both temperature and pressure (the fully general case). A simpler case, barotropic flow, allows for density dependence only on pressure, so that the curl of the pressure-gradient force vanishes.

Where do Rossby waves occur?

Rossby waves, also known as planetary waves, are a type of inertial wave naturally occurring in rotating fluids. They were first identified by Sweden-born American meteorologist Carl-Gustaf Arvid Rossby. They are observed in the atmospheres and oceans of planets owing to the rotation of the planet.

What is a Rossby wave train?

Rossby wave trains (RWTs) are coherent envelopes of baroclinic waves that propagate on the midlatitude waveguide and are capable of producing downstream development. The waveguide is a region of heightened potential vorticity gradient along steeply sloping isentropic surfaces defining the mid-latitude jet stream.