Examples of 'geostrophic' in a sentence
Meaning of "geostrophic"
geostrophic (adjective) - a term used in meteorology to describe a balance between the pressure gradient force and the Coriolis force in the atmosphere
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- Relating to the balance, in the atmosphere, between the horizontal Coriolis forces and the horizontal pressure forces.
- Relating to or arising from the deflective force exerted on the atmosphere due to the rotation of the earth.
How to use "geostrophic" in a sentence
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geostrophic
Geostrophic flow may be either barotropic or baroclinic.
This condition is called geostrophic balance.
Geostrophic wind scale.
Balance between these two forces is referred to as geostrophic.
This is known as geostrophic flow.
The geostrophic wind is directed parallel to isobars lines of constant pressure at a given height.
The transports are estimated from geostrophic velocities.
A possible correlation between geostrophic flows and internal waves is considered in the main thermocline.
Barotropic conditions with no geostrophic flow ;.
The data were compared to geostrophic flows predicted from oceanographic models.
Geostrophic flow in air or water is a zero-frequency inertial wave.
Modifications to the standard scenario of geostrophic adjustment are highlighted.
Rossby waves, geostrophic currents, and geostrophic winds are examples of inertial waves.
This is known as a geostrophic wind.
The geostrophic equations are a simplified form of the Navier-Stokes equations in a rotating reference frame.
See also
This Ekman transport is superimposed on geostrophic flow associated with horizontal gradients of density.
Their associated meso - and large scale circulation is in geostrophic equilibrium.
The direction of the geostrophic flow in the disc interspace is shown by an arrow G.
Instead, we show that the majority of the energy goes in a geostrophic mode.
In the free atmosphere, geostrophic wind relationships should be used.
The cor - responding meso - and large scale circulation is in geostrophic equilibrium.
To forecast such storm and geostrophic wind intensities, scientists invented datasets.
The effect of friction, between the air and the land, breaks the geostrophic balance.
The perturbations of the geostrophic equilibrium leading to quasi-geostrophic motion come from thermodynamical atmospheric phenomena.
In a barotropic atmosphere, where temperature is uniform, the geostrophic wind is independent of height.
Abstract, Nonlinear geostrophic adjustment of rectilinear jets is examined analytically.
In contrast, the circulation in the Earth 's atmosphere is governed by the geostrophic balance.
The centripetal force alters the original two-force geostrophic balance and creates a non-geostrophic gradient wind.
As shown, the ribs 12 form obstacles to a substantially circular geostrophic flow.
It 's called the geostrophic wind.
S3130 Subgeostrophic wind Wind with a speed less than the corresponding geostrophic wind speed.
The station data included in the analysis were used to estimate geostrophic flows referenced to 1 000 m.
S3530 Supergeostrophic wind Wind with a speed greater than the corresponding geostrophic wind speed.
The large-scale atmospheric flows are essentially nearly hydrostatic, nearly geostrophic and wave-like in appearance.
Surface geostrophic flow was calculated from oceanographic data recorded since 1925.
Naganobu ( Japan ) which were used to calculate geostrophic current velocities.
G0310 Geostrophic advection Advection produced by the geostrophic component of the wind.
A flow line for part of this geostrophic flow is shown in Fig . 2 and designated 13.
