Rekodi ya ushahidi wa mbinu
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.
Rekodi ya chanzo
Nukuu zimehamishwa kwa uhalisi kutoka kwa rekodi ya chanzo cha mbinu. Hakuna uthibitisho wa kiwango cha dai unaodokezwa kutoka kwao.
Thermal Wind Relationship
Rekodi ya mbinu ya kiajenda · 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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Mbinu zinazohusiana
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