Sammenlign metoder
Gjennomgå de valgte metodene side om side; rader som avviker, er uthevet.
| Skew-T Log-P-analyse× | WRF-modellen× | |
|---|---|---|
| Fagfelt | Meteorologi | Meteorologi |
| Familie | Process / pipeline | Process / pipeline |
| Opprinnelsesår≠ | 1960s | 2000 |
| Opphavsperson≠ | Reitan, Skamarock | Skamarock and Klemp |
| Type≠ | Graphical thermodynamic tool | Atmospheric simulation system |
| Opprinnelig kilde≠ | Bluestein, H. B. (1992). Synoptic-dynamic meteorology in midlatitudes. Volume I: Principles of Kinematics and Dynamics. Oxford University Press. link ↗ | Skamarock, W. C., Klemp, J. B., Dudhia, J., et al. (2008). A Description of the Advanced Research WRF Version 3. NCAR Technical Note NCAR/TN-475+STR. link ↗ |
| Alias | Skew-T, Skew-T Log-P diagram, Tephigram, Stuve diagram | Weather Research and Forecasting, WRF, ARW, NMM |
| Relaterte≠ | 3 | 4 |
| 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 Weather Research and Forecasting (WRF) model is a mesoscale atmospheric simulation system used for weather forecasting, research, and climate applications. Developed cooperatively by NCAR, NOAA, and academic institutions, WRF became operational in 2004 and has become one of the most widely used atmospheric models worldwide. |
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