FN Archimer Export Format PT J TI Characterization of Internal Tide Incoherence: Eulerian versus Lagrangian Perspectives BT AF Caspar-Cohen, Zoe Ponte, Aurelien Lahaye, Noe Carton, Xavier Yu, Xiaolong LE GENTIL, Sylvie AS 1:1;2:1;3:2;4:4;5:3;6:1; FF 1:PDG-ODE-LOPS-OH;2:PDG-ODE-LOPS-OH;3:;4:;5:;6:PDG-ODE-LOPS-OH; C1 Ifremer, Université de Brest, CNRS, IRD, Laboratoire d’Océanographie Physique et Spatiale, IUEM, Brest, France Inria, IRMAR, Campus de Beaulieu, Rennes, France School of Marine Sciences, Sun Yat-sen University, Zhuhai, China Ifremer, Université de Brest, CNRS, IRD, Laboratoire d’Océanographie Physique et Spatiale, IUEM, Brest, France C2 IFREMER, FRANCE INRIA, FRANCE UNIV YAT-SEN, CHINA UBO, FRANCE SI BREST SE PDG-ODE-LOPS-OH UM LOPS IN WOS Ifremer UMR WOS Cotutelle UMR copubli-france copubli-univ-france copubli-int-hors-europe copubli-sud IF 3.5 TC 3 UR https://archimer.ifremer.fr/doc/00786/89755/95280.pdf LA English DT Article DE ;Internal waves;Tides;Surface observations;Idealized models AB The Lagrangian and Eulerian surface current signatures of a low-mode internal tide propagating through a turbulent balanced flow are compared in idealized numerical simulations. Lagrangian and Eulerian total (i.e., coherent plus incoherent) tidal amplitudes are found to be similar. Compared to Eulerian diagnostics, the Lagrangian tidal signal is more incoherent with comparable or smaller incoherence time scales and larger incoherent amplitudes. The larger level of incoherence in Lagrangian data is proposed to result from the deformation of an Eulerian internal tide signal induced by drifter displacements. Based on the latter hypothesis, a theoretical model successfully predicts Lagrangian autocovariances by relating Lagrangian and Eulerian autocovariances and the properties of the internal tides and jet. These results have implications for the separation of balanced flow and internal tides signals in the sea level data collected by the future Surface Water and Ocean Topography (SWOT) satellite mission. PY 2022 PD JUL SO Journal Of Physical Oceanography SN 0022-3670 PU American Meteorological Society VL 52 IS 6 UT 000839063900012 BP 1245 EP 1259 DI 10.1175/JPO-D-21-0088.1 ID 89755 ER EF