So sánh phương pháp

	Gió Nhiệt	Gió địa chuyển
Lĩnh vực	Khí tượng học	Khí tượng học
Họ	Process / pipeline	Process / pipeline
Năm ra đời	1920s	1857
Người khởi xướng	Jacobbian insights from geostrophic flow	Buys Ballot, Coriolis
Loại	Wind-temperature relationship	Wind balance principle
Công trình gốc	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.
Tên gọi khác	Thermal wind, Vertical wind shear, Barotropic	Geostrophic wind, Geostrophic balance, Geostrophic approximation
Liên quan	3	3
Tóm tắt	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.	Geostrophic wind balance is a fundamental concept in meteorology that describes the balance between the pressure gradient force and the Coriolis force in large-scale atmospheric flow. When this balance is achieved, wind blows parallel to isobars without acceleration—a condition observed in the free atmosphere away from the equator and surface boundary layer.