方法证据记录
Thermal Wind
The thermal wind relationship is a fundamental meteorological principle that links vertical wind shear to horizontal temperature gradients. It states that wind speed increases with height in the direction of warming—a direct consequence of hydrostatic and geostrophic balance combined with the ideal gas law.
源记录
引文逐字复制自方法源记录。这些引文不代表任何层级的验证。
Thermal Wind Relationship
分类方法记录 · process-pipeline / meteorology
- Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press. · URL
- Bluestein, H. B. (1993). Synoptic-dynamic meteorology in midlatitudes. Volume 2: Observations and Theory of Weather Systems. Oxford University Press. · URL
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