Порівняння методів

	Термічний вітер	Рівняння квазі-геострофічної Омеги
Галузь	Метеорологія	Метеорологія
Родина	Process / pipeline	Process / pipeline
Рік появи	1920s	1970s
Автор методу	Jacobbian insights from geostrophic flow	Trenberth, Omaga
Тип	Wind-temperature relationship	Diagnostic equation for vertical motion
Основоположне джерело	Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press.	Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press.
Інші назви	Thermal wind, Vertical wind shear, Barotropic	QG omega equation, Quasi-geostrophic dynamics, Vertical motion prediction
Пов'язані	3	3
Підсумок	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 quasi-geostrophic (QG) omega equation is a fundamental diagnostic equation in synoptic meteorology that relates vertical motion (omega = dP/dt) to horizontal temperature and vorticity fields. It predicts where air rises and sinks based on the geostrophic flow structure without explicitly solving for vertical velocity.