Linganisha mbinu

	Uchambuzi wa Lagrangian wa Drifter	Usafirishaji wa Ekman	Kasi ya Kijiografia
Nyanja	Oseanografia	Oseanografia	Oseanografia
Familia	Process / pipeline	Process / pipeline	Process / pipeline
Mwaka wa asili	1985	1905	1942
Mwanzilishi	Robert Davis	Vagn Walfrid Ekman	Harald Sverdrup
Aina	instrumental	theoretical-method	theoretical-method
Chanzo asilia	Davis, R. E. (1985). Drifter observations of coastal surface currents during CODE: The method and descriptive view. Journal of Geophysical Research, 90(C3), 4741-4755.	Ekman, V. W. (1905). On the influence of the Earth's rotation on ocean currents. Arkiv for Matematik, Astronomi och Fysik, 2(11), 1-52.	Sverdrup, H. U., Johnson, M. W., & Fleming, R. H. (1942). The Oceans: Their Physics, Chemistry, and General Biology. Prentice-Hall.
Majina mbadala	Lagrangian Tracking, Drifter Analysis	Ekman Spiral, Wind-driven Transport	Geostrophic Current, Thermal Wind Equation
Zinazohusiana	3	3	3
Muhtasari	Drifter Lagrangian analysis tracks the motion of water parcels using surface drifters (buoys with attached drogues) to measure ocean currents directly. Developed by Robert Davis in the 1980s, this method provides direct observation of water parcel trajectories and enables estimation of eddy diffusivity, transport pathways, and mixing. Drifter data complement Eulerian (fixed-point) observations by capturing the Lagrangian perspective of fluid motion.	Ekman transport is the net volume flux of water driven by wind stress balanced with Coriolis force in the surface boundary layer. Derived by Vagn Walfrid Ekman in 1905 from the principle that wind stress is transmitted through the water column in a spiral pattern, Ekman transport is responsible for coastal upwelling and important oceanographic transports. The theory links surface wind patterns directly to ocean circulation.	Geostrophic velocity is the current driven by balance between the pressure gradient force and the Coriolis force, derived from the thermal wind equation. In most of the ocean away from the equator and coastal boundaries, geostrophic balance is an excellent approximation to the actual flow. Developed by Harald Sverdrup and colleagues in the 1940s, geostrophic velocity calculation from hydrographic data enables estimation of ocean currents without direct current measurements.