Σύγκριση μεθόδων
Εξετάστε τις επιλεγμένες μεθόδους δίπλα-δίπλα· οι γραμμές που διαφέρουν επισημαίνονται.
| Μεταφορά Ekman× | Αρμονική Ανάλυση Παλιρροιών× | |
|---|---|---|
| Πεδίο | Ωκεανογραφία | Ωκεανογραφία |
| Οικογένεια | Process / pipeline | Process / pipeline |
| Έτος προέλευσης≠ | 1905 | 1867 |
| Δημιουργός≠ | Vagn Walfrid Ekman | William Thomson |
| Τύπος≠ | theoretical-method | fourier-analysis |
| Θεμελιώδης πηγή≠ | 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. link ↗ | Godin, G. (1972). The Analysis of Tides. University of Toronto Press. link ↗ |
| Εναλλακτικές ονομασίες | Ekman Spiral, Wind-driven Transport | Tidal Constituents, Harmonic Tidal Prediction |
| Συναφείς | 3 | 3 |
| Σύνοψη≠ | 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. |
| ScholarGateΣύνολο δεδομένων ↗ |
|
|