विधियों की तुलना करें

	ऊष्मीय पवन	स्क्यू-टी लॉग-पी विश्लेषण
क्षेत्र	मौसम विज्ञान	मौसम विज्ञान
परिवार	Process / pipeline	Process / pipeline
उद्भव वर्ष	1920s	1960s
प्रवर्तक	Jacobbian insights from geostrophic flow	Reitan, Skamarock
प्रकार	Wind-temperature relationship	Graphical thermodynamic tool
मौलिक स्रोत	Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press.	Bluestein, H. B. (1992). Synoptic-dynamic meteorology in midlatitudes. Volume I: Principles of Kinematics and Dynamics. Oxford University Press.
उपनाम	Thermal wind, Vertical wind shear, Barotropic	Skew-T, Skew-T Log-P diagram, Tephigram, Stuve diagram
संबंधित	3	3
सारांश	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.	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.