Sammenlign metoder
Gjennomgå de valgte metodene side om side; rader som avviker, er uthevet.
| Barnes-Cressman Analyse× | Skew-T Log-P-analyse× | |
|---|---|---|
| Fagfelt | Meteorologi | Meteorologi |
| Familie | Process / pipeline | Process / pipeline |
| Opprinnelsesår≠ | 1959 | 1960s |
| Opphavsperson≠ | Barnes, Cressman | Reitan, Skamarock |
| Type≠ | Objective analysis method | Graphical thermodynamic tool |
| Opprinnelig kilde≠ | Barnes, S. L. (1964). A Technique for Maximizing Details in Numerical Weather Map Analysis. Journal of Applied Meteorology, 3(4), 396-409. DOI ↗ | Bluestein, H. B. (1992). Synoptic-dynamic meteorology in midlatitudes. Volume I: Principles of Kinematics and Dynamics. Oxford University Press. link ↗ |
| Alias | Barnes analysis, Cressman analysis, Objective analysis, Grid interpolation | Skew-T, Skew-T Log-P diagram, Tephigram, Stuve diagram |
| Relaterte≠ | 2 | 3 |
| Sammendrag≠ | Barnes-Cressman analysis is an objective interpolation method that creates gridded meteorological fields from irregularly spaced observations (station data, radiosonde profiles, buoys). It is widely used for synoptic analysis, quality control, and initialization of numerical weather models. | 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. |
| ScholarGateDatasett ↗ |
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