方法对比
并排查看您选择的方法；存在差异的行会高亮显示。
| Barnes-Cressman 分析× | Skew-T Log-P 分析× | |
|---|---|---|
| 领域 | 气象学 | 气象学 |
| 方法族 | Process / pipeline | Process / pipeline |
| 起源年份≠ | 1959 | 1960s |
| 提出者≠ | Barnes, Cressman | Reitan, Skamarock |
| 类型≠ | Objective analysis method | Graphical thermodynamic tool |
| 开创性文献≠ | 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 ↗ |
| 别名 | Barnes analysis, Cressman analysis, Objective analysis, Grid interpolation | Skew-T, Skew-T Log-P diagram, Tephigram, Stuve diagram |
| 相关≠ | 2 | 3 |
| 摘要≠ | 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. |
| ScholarGate数据集 ↗ |
|
|