Rapid subduction in the deep North Western Mediterranean

Autor: C. Richardt, D. Dornic, D. Lo Presti, G.E. Păvălaş, M. Morganti, Oleg Kalekin, Isabelle Taupier-Letage, K. Lyons, M. Circella, Uli Katz, A. Mazure, G. Halladjian, D. Zaborov, M. Ardid, A. Radu, Francisco Camarena, J. Hößl, H. Laschinsky, C. Curtil, A. Albert, M. Neff, Gisela Anton, Robert Lahmann, Vincenzo Cavasinni, C. Distefano, C. Donzaud, B. Vallage, A. Brown, U. Fritsch, Antonio Capone, P. Payre, C. M. Reed, Annarita Margiotta, J. J. Aubert, Jürgen Brunner, J.-L. Fuda, Maurizio Spurio, Anne Deschamps, R. Pillet, U. Emanuele, A.J. Heijboer, J. Carr, F. M. Schoeck, M. P. Decowski, C. Racca, F. Salesa, L. Tasca, Thierry Pradier, G. Guillard, J.J. Hernández-Rey, Gregory David Hallewell, H. Loehner, G. Lelaizant, C. Picq, S. Loucatos, Dominique Lefèvre, S.F. Biagi, E. A. De Wolf, Holger Motz, S. Basa, Vincent Bertin, M. Marcelin, N. Picot-Clemente, R. Auer, Juanan Aguilar, R. Ostasch, G. Wijnker, Manuela Vecchi, Ciro Bigongiari, Heide Costantini, Alexander Kappes, G. Riccobene, D. Castel, G.V. Russo, V. Flaminio, G. De Bonis, Giuseppina Larosa, J.P. Gómez-González, I. Dekeyser, F. Lucarelli, Jos Steijger, V. Van Elewyck, F. Fehr, Gilles Maurin, P. Vernin, Rezo Shanidze, P. Coyle, J. Zúñiga, Thomas Eberl, V. Popa, W. Kretschmer, J. P. Schuller, M.C. Bouwhuis, M. Rujoiu, Stephanie Escoffier, M. Bazzotti, J.-P. Ernenwein, P. Piattelli, Simona Toscano, K. Fratini, Manuel Bou-Cabo, Francesco Simeone, N. Cottini, Patrick Lamare, A. C.S. Assis Jesus, Tri L. Astraatmadja, Th. Stolarczyk, S. Anvar, S. Mangano, Yann Hello, Guillaume Lambard, J.A. Martínez-Mora, H. van Haren, E. Castorina, Kay Graf, Christian Tamburini, Ph. Charvis, J. Petrovic, G. Giacomelli, C. Naumann, G. Palioselitis, B. Baret, Doriane Drouhin, Antoine Kouchner, M. Melissas, H. Yepes, E. Presani, Tommaso Chiarusi, C. Kopper, Teresa Montaruli, R. Coniglione, J.D. Zornoza, Nasser Kalantar-Nayestanaki, M. de Jong, M. Anghinolfi, J. Busto, L. Moscoso, S. Cecchini, G. Lim, P. Kooijman, G. Carminati
Přispěvatelé: Centre de Physique des Particules de Marseille (CPPM), Aix Marseille Université (AMU)-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Centre National de la Recherche Scientifique (CNRS), AstroParticule et Cosmologie (APC (UMR_7164)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS), Laboratoire d'Astrophysique de Marseille (LAM), Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS), Centre d'océanologie de Marseille (COM), Université de la Méditerranée - Aix-Marseille 2-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Université Paris Cité (UPCité), Institut Pluridisciplinaire Hubert Curien (IPHC), Université de Strasbourg (UNISTRA)-Université de Haute-Alsace (UHA) Mulhouse - Colmar (Université de Haute-Alsace (UHA))-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Centre National de la Recherche Scientifique (CNRS)
Jazyk: angličtina
Rok vydání: 2022
Předmět:
Zdroj: ResearcherID
ISSN: 1812-0792
Popis: An Acoustic Doppler Current Profiler (ADCP) moored at the deep-sea ANTARES neutrino telescope site near Toulon, France, measured downward vertical currents of amplitudes up to 0.03 m s−1 in spring 2006. The currents were accompanied by enhanced levels of acoustic reflection by a factor of about 10 and by horizontal currents reaching 0.35 m s−1. These observations coincided with high levels of bioluminescence detected by the telescope. Although during winter 2006 deep dense-water formation occurred in this area, episodes of high levels of suspended particles and large vertical currents continuing into the summer are not direct evidence of this process. It is hypothesized that the main process allowing for particles to be moved across the entire water column (2500 m) within a few days, is local convection, triggered by small-mesoscale phenomena, such as meanders including a bipolar vortex, linked with boundary current instabilities.
Databáze: OpenAIRE