Method evidence record
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.
Source record
Citations copied verbatim from the method’s source record. No claim-level verification is inferred from them.
Thermal Wind Relationship
Taxonomic method record · 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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Related methods
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