Drifter Lagrangian Analysis
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.
Kilderegister
Siteringer kopiert ordrett fra metodens kilderegister. Ingen påstandsnivåverifisering er underforstått fra dem.
- 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. · DOI 10.1029/JC090iC03p04741
- Lumpkin, R., & Pazos, M. (2007). Measuring surface currents with Surface Velocity Program drifters: the instrument, its data, and its applications. In A. Griffa, A. D. Kirwan, A. J. Mariano, T. M. Ozgokmen, & H. T. Rossby (Eds.), Lagrangian Analysis and Prediction of Coastal and Ocean Dynamics (pp. 39-67). Cambridge University Press. · DOI 10.1017/CBO9780511535901.003
Kuraterte påstander
Påstander lagret i bevishovedboken, hver med sin egen vurdering.
Denne visningen finner ikke opp en påstandsvurdering når hovedboken ikke har noen.
Relaterte metoder
Generert fra metodegrafen og vist som maskinforslåtte relasjoner – ingen bevispåstand er underforstått.