Võrdle meetodeid

	Geostrophic Velocity	Akustiline Doppleri voolukiirusprofiilide mõõtur	Ekmani transport	Tõusuanalüüs harmooniliste komponentide alusel
Valdkond	Okeanograafia	Okeanograafia	Okeanograafia	Okeanograafia
Perekond	Process / pipeline	Process / pipeline	Process / pipeline	Process / pipeline
Tekkeaasta	1942	1983	1905	1867
Looja	Harald Sverdrup	RD Instruments	Vagn Walfrid Ekman	William Thomson
Tüüp	theoretical-method	instrumental	theoretical-method	fourier-analysis
Algallikas	Sverdrup, H. U., Johnson, M. W., & Fleming, R. H. (1942). The Oceans: Their Physics, Chemistry, and General Biology. Prentice-Hall.	RD Instruments. (1996). Acoustic Doppler Current Profiler Principles of Operation. A Practical Primer. RD Instruments Technical Note.	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.	Godin, G. (1972). The Analysis of Tides. University of Toronto Press.
Rööpnimetused	Geostrophic Current, Thermal Wind Equation	ADCP	Ekman Spiral, Wind-driven Transport	Tidal Constituents, Harmonic Tidal Prediction
Seotud	3	3	3	3
Kokkuvõte	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.	The Acoustic Doppler Current Profiler (ADCP) is an instrument that uses Doppler-shifted acoustic backscatter to measure water velocity profiles along a vertical profile. Developed by RD Instruments in the 1980s, it has become the standard method for high-resolution current profiling in oceanographic research. ADCPs provide unprecedented spatial and temporal resolution of ocean circulation patterns.	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.	Tidal harmonic analysis is a mathematical method that decomposes observed sea level or current time series into a sum of sinusoidal components with specific frequencies, amplitudes, and phases corresponding to astronomical tidal constituents. Developed by William Thomson (Lord Kelvin) in 1867, harmonic analysis enables prediction of tides and understanding of tidal dynamics in coastal regions.