Vertaile menetelmiä
Tarkastele valitsemiasi menetelmiä rinnakkain; eroavat rivit korostetaan.
| Potentiaalisen pyörteisyyden inversio× | Geostrofinen tuuli× | |
|---|---|---|
| Tieteenala | Meteorologia | Meteorologia |
| Menetelmäperhe | Process / pipeline | Process / pipeline |
| Syntyvuosi≠ | 1985 | 1857 |
| Kehittäjä≠ | Haynes, McIntyre, Hoskins | Buys Ballot, Coriolis |
| Tyyppi≠ | Diagnostic inversion method | Wind balance principle |
| Alkuperäislähde≠ | Haynes, P., & McIntyre, M. E. (1987). On the evolution of vorticity and potential vorticity in the atmosphere. Journal of the Atmospheric Sciences, 44(5), 828-841. link ↗ | Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press. link ↗ |
| Rinnakkaisnimet | PV inversion, Potential vorticity, PV thinking | Geostrophic wind, Geostrophic balance, Geostrophic approximation |
| Liittyvät | 3 | 3 |
| Tiivistelmä≠ | Potential vorticity (PV) inversion is a diagnostic technique that reconstructs atmospheric wind and pressure fields from the spatial distribution of potential vorticity. This method assumes that, in a geostrophically balanced atmosphere, the PV field uniquely determines the balanced circulation around anomalies. | Geostrophic wind balance is a fundamental concept in meteorology that describes the balance between the pressure gradient force and the Coriolis force in large-scale atmospheric flow. When this balance is achieved, wind blows parallel to isobars without acceleration—a condition observed in the free atmosphere away from the equator and surface boundary layer. |
| ScholarGateAineisto ↗ |
|
|