Sammenlign metoder
Gjennomgå de valgte metodene side om side; rader som avviker, er uthevet.
| Skew-T Log-P-analyse× | Termisk vind× | |
|---|---|---|
| Fagfelt | Meteorologi | Meteorologi |
| Familie | Process / pipeline | Process / pipeline |
| Opprinnelsesår≠ | 1960s | 1920s |
| Opphavsperson≠ | Reitan, Skamarock | Jacobbian insights from geostrophic flow |
| Type≠ | Graphical thermodynamic tool | Wind-temperature relationship |
| Opprinnelig kilde≠ | Bluestein, H. B. (1992). Synoptic-dynamic meteorology in midlatitudes. Volume I: Principles of Kinematics and Dynamics. Oxford University Press. link ↗ | Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press. link ↗ |
| Alias≠ | Skew-T, Skew-T Log-P diagram, Tephigram, Stuve diagram | Thermal wind, Vertical wind shear, Barotropic |
| Relaterte | 3 | 3 |
| Sammendrag≠ | The Skew-T Log-P diagram is a thermodynamic chart used extensively in meteorology to visualize atmospheric profiles of temperature, dew point, and pressure. Developed in its modern form by Reitan in the 1960s, it allows forecasters and researchers to quickly assess atmospheric stability, convective potential, wind shear, and other properties critical for weather diagnosis and prediction. | 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. |
| ScholarGateDatasett ↗ |
|
|