• विभव भ्रमिलता | |
potential: विभवमापी तनाव | |
vorticity: आवर्त भ्रमिलता | |
potential vorticity मीनिंग इन हिंदी
potential vorticity उदाहरण वाक्य
उदाहरण वाक्य
अधिक: आगे- The first assumption will be an initial potential vorticity anomaly somewhere in the upper troposphere.
- An equatorward heat flux is induced, decreasing potential vorticity and pressure anomalies and yielding cyclolysis.
- They found that changes in potential vorticity at the tropopause can cause changes in the wind field.
- Specifically, different schemes have different methods of parametrizing the potential vorticity which results in different tracks.
- The deviations are caused by the Coriolis force and conservation of potential vorticity which leads to changes of relative vorticity.
- The tropopause lowers the further towards the pole you go in general and you have higher stratospheric potential vorticity poleward.
- The potential vorticity is absolute vorticity divided by the vertical spacing between levels of constant entropy ( or potential temperature ).
- Atmospheric Rossby waves are the result of conservation of potential vorticity and are influenced by the Coriolis force and pressure gradient.
- Such upper-level positive potential vorticity will induce a flow non-local to where the potential vorticity anomaly is.
- Such upper-level positive potential vorticity will induce a flow non-local to where the potential vorticity anomaly is.