विधियों की तुलना करें
चुनी हुई विधियों की आमने-सामने समीक्षा करें; भिन्नता वाली पंक्तियाँ रेखांकित हैं।
| बार्न्स-क्रेसमैन विश्लेषण× | स्क्यू-टी लॉग-पी विश्लेषण× | |
|---|---|---|
| क्षेत्र | मौसम विज्ञान | मौसम विज्ञान |
| परिवार | Process / pipeline | Process / pipeline |
| उद्भव वर्ष≠ | 1959 | 1960s |
| प्रवर्तक≠ | Barnes, Cressman | Reitan, Skamarock |
| प्रकार≠ | Objective analysis method | Graphical thermodynamic tool |
| मौलिक स्रोत≠ | 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 ↗ |
| उपनाम | Barnes analysis, Cressman analysis, Objective analysis, Grid interpolation | Skew-T, Skew-T Log-P diagram, Tephigram, Stuve diagram |
| संबंधित≠ | 2 | 3 |
| सारांश≠ | 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. |
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