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Inverzija potencijalnog vrtloga×Toplinski vjetar×
PodručjeMeteorologijaMeteorologija
ObiteljProcess / pipelineProcess / pipeline
Godina nastanka19851920s
TvoracHaynes, McIntyre, HoskinsJacobbian insights from geostrophic flow
VrstaDiagnostic inversion methodWind-temperature relationship
Temeljni izvorHaynes, 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 ↗
Drugi naziviPV inversion, Potential vorticity, PV thinkingThermal wind, Vertical wind shear, Barotropic
Srodne33
SažetakPotential 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.The thermal wind relationship is a fundamental meteorological principle that links vertical wind shear to horizontal temperature gradients. It states that wind speed increases with height in the direction of warming—a direct consequence of hydrostatic and geostrophic balance combined with the ideal gas law.
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ScholarGateUsporedite metode: Potential Vorticity Inversion · Thermal Wind. Preuzeto 2026-06-18 s https://scholargate.app/hr/compare