Sammenlign metoder
Gennemgå dine valgte metoder side om side; rækker, der afviger, er fremhævet.
| Skew-T Log-P Analyse× | Monin-Obukhovs lighedsteori× | |
|---|---|---|
| Fagområde | Meteorologi | Meteorologi |
| Familie | Process / pipeline | Process / pipeline |
| Oprindelsesår≠ | 1960s | 1954 |
| Ophavsperson≠ | Reitan, Skamarock | Monin and Obukhov |
| Type≠ | Graphical thermodynamic tool | Similarity scaling framework |
| Oprindelig kilde≠ | Bluestein, H. B. (1992). Synoptic-dynamic meteorology in midlatitudes. Volume I: Principles of Kinematics and Dynamics. Oxford University Press. link ↗ | Monin, A. S., & Obukhov, A. M. (1954). Basic laws of turbulent mixing in the ground layer of the atmosphere. Tr. Akad. Nauk SSSR, 24, 163-187. link ↗ |
| Aliasser≠ | Skew-T, Skew-T Log-P diagram, Tephigram, Stuve diagram | Monin-Obukhov, Similarity theory, Monin-Obukhov length scale |
| Relaterede | 3 | 3 |
| Resumé≠ | 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. | Monin-Obukhov similarity theory is a fundamental framework in boundary layer meteorology that describes how wind speed, temperature, and humidity vary with height near the surface. Published in 1954, it shows that normalized vertical profiles depend on a single dimensionless parameter—the Monin-Obukhov stability parameter—which quantifies the balance between mechanical turbulence and buoyant convection. |
| ScholarGateDatasæt ↗ |
|
|