An Acoustic Doppler Current Profiler (ADCP) was moored at the deep-sea site of the ANTARES neutrino telescope near Toulon, France, thus providing a unique opportunity to compare high-resolution acoustic and optical observations between 70 and 170 m above the sea bed at 2475 m. The ADCP measured downward vertical currents of magnitudes up to 0.03 m s(-1) in late winter and early spring 2006. In the same period, observations were made of enhanced levels of acoustic reflection, interpreted as suspended particles including zooplankton, by a factor of about 10 and of horizontal currents reaching 0.35 m s(-1). These observations coincided with high light levels detected by the telescope, interpreted as increased bioluminescence. During winter 2006 deep dense-water formation occurred in the Ligurian subbasin, thus providing a possible explanation for these observations. However, the 10-20 days quasi-periodic episodes of high levels of acoustic reflection, light and large vertical currents continuing into the summer are not direct evidence of this process. It is hypothesized that the main process allowing for suspended material to be moved vertically later in the year is local advection, linked with topographic boundary current instabilities along the rim of the 'Northern Current'. (C) 2011 Elsevier Ltd. All rights reserved.

Acoustic and optical variations during rapid downward motion episodes in the deep north-western Mediterranean Sea / H., Van Haren; I., Taupier Letage; J. A., Aguilar; A., Albert; M., Anghinolfi; G., Anton; S., Anvar; M., Ardid; A. C., Assisjesus; A. C., Assis Jesus; Aca, Jesus; T., Astraatmadja; J. J., Aubert; R., Auer; B., Baret; S., Basa; M., Bazzotti; V., Bertin; S., Biagi; C., Bigongiari; M., Bou Cabo; M. C., Bouwhuis; A., Brown; J., Brunner; J., Busto; F., Camarena; Capone, Antonio; G., Carminati; J., Carr; D., Castel; E., Castorina; V., Cavasinni; S., Cecchini; Ph, Charvis; T., Chiarusi; M., Circella; R., Coniglione; H., Costantini; N., Cottini; P., Coyle; C., Curtil; DE BONIS, Giulia; M. P., Decowski; I., Dekeyser; A., Deschamps; C., Distefano; C., Donzaud; D., Dornic; D., Drouhin; T., Eberl; U., Emanuele; J. P., Ernenwein; S., Escoffier; F., Fehr; V., Flaminio; K., Fratini; U., Fritsch; J. L., Fuda; G., Giacomelli; J. P., Gomez Gonzalez; K., Graf; G., Guillard; G., Halladjian; G., Hallewell; A. J., Heijboer; Y., Hello; J. J., Hernandez Rey; J., Hossl; M., Dejong; M., De Jong; N., Kalantar Nayestanaki; O., Kalekin; A., Kappes; U., Katz; P., Kooijman; C., Kopper; A., Kouchner; W., Kretschmer; R., Lahmann; P., Lamare; G., Lambard; G., Larosa; H., Laschinsky; D., Lefevre; G., Lelaizant; G., Lim; D., Lopresti; D., Lo Presti; H., Loehner; S., Loucatos; Lucarelli, Fabrizio; K., Lyons; S., Mangano; M., Marcelin; A., Margiotta; J. A., Martinez Mora; G., Maurin; A., Mazure; M., Melissas; T., Montaruli; M., Morganti; L., Moscoso; H., Motz; C., Naumann; M., Neff; R., Ostasch; G., Palioselitis; G. E., Pavalas; P., Payre; J., Petrovic; P., Piattelli; N., Picot Clemente; C., Picq; R., Pillet; V., Popa; T., Pradier; E., Presani; C., Racca; A., Radu; C., Reed; G., Riccobene; C., Richardt; M., Rujoiu; G. V., Russo; F., Salesa; F., Schoeck; J. P., Schuller; R., Shanidze; Simeone, Francesco; M., Spurio; J. J. M., Steijger; Th, Stolarczyk; C., Tamburini; L., Tasca; S., Toscano; B., Vallage; V., Vanelewyck; V., Van Elewyck; Vecchi, Manuela; P., Vernin; G., Wijnker; E., Dewolf; E., De Wolf; H., Yepes; D., Zaborov; J. D., Zornoza; J., Zuniga. - In: DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS. - ISSN 0967-0637. - STAMPA. - 58:8(2011), pp. 875-884. [10.1016/j.dsr.2011.06.006]

Acoustic and optical variations during rapid downward motion episodes in the deep north-western Mediterranean Sea

CAPONE, Antonio;DE BONIS, Giulia;LUCARELLI, FABRIZIO;SIMEONE, Francesco;VECCHI, MANUELA;
2011

Abstract

An Acoustic Doppler Current Profiler (ADCP) was moored at the deep-sea site of the ANTARES neutrino telescope near Toulon, France, thus providing a unique opportunity to compare high-resolution acoustic and optical observations between 70 and 170 m above the sea bed at 2475 m. The ADCP measured downward vertical currents of magnitudes up to 0.03 m s(-1) in late winter and early spring 2006. In the same period, observations were made of enhanced levels of acoustic reflection, interpreted as suspended particles including zooplankton, by a factor of about 10 and of horizontal currents reaching 0.35 m s(-1). These observations coincided with high light levels detected by the telescope, interpreted as increased bioluminescence. During winter 2006 deep dense-water formation occurred in the Ligurian subbasin, thus providing a possible explanation for these observations. However, the 10-20 days quasi-periodic episodes of high levels of acoustic reflection, light and large vertical currents continuing into the summer are not direct evidence of this process. It is hypothesized that the main process allowing for suspended material to be moved vertically later in the year is local advection, linked with topographic boundary current instabilities along the rim of the 'Northern Current'. (C) 2011 Elsevier Ltd. All rights reserved.
2011
antares neutrino telescope; deep mediteranean; northern boundary current; acoustic adcp observations; episodic downward current; dense water formation; bioluminescence; optical photo-multiplier observations
01 Pubblicazione su rivista::01a Articolo in rivista
Acoustic and optical variations during rapid downward motion episodes in the deep north-western Mediterranean Sea / H., Van Haren; I., Taupier Letage; J. A., Aguilar; A., Albert; M., Anghinolfi; G., Anton; S., Anvar; M., Ardid; A. C., Assisjesus; A. C., Assis Jesus; Aca, Jesus; T., Astraatmadja; J. J., Aubert; R., Auer; B., Baret; S., Basa; M., Bazzotti; V., Bertin; S., Biagi; C., Bigongiari; M., Bou Cabo; M. C., Bouwhuis; A., Brown; J., Brunner; J., Busto; F., Camarena; Capone, Antonio; G., Carminati; J., Carr; D., Castel; E., Castorina; V., Cavasinni; S., Cecchini; Ph, Charvis; T., Chiarusi; M., Circella; R., Coniglione; H., Costantini; N., Cottini; P., Coyle; C., Curtil; DE BONIS, Giulia; M. P., Decowski; I., Dekeyser; A., Deschamps; C., Distefano; C., Donzaud; D., Dornic; D., Drouhin; T., Eberl; U., Emanuele; J. P., Ernenwein; S., Escoffier; F., Fehr; V., Flaminio; K., Fratini; U., Fritsch; J. L., Fuda; G., Giacomelli; J. P., Gomez Gonzalez; K., Graf; G., Guillard; G., Halladjian; G., Hallewell; A. J., Heijboer; Y., Hello; J. J., Hernandez Rey; J., Hossl; M., Dejong; M., De Jong; N., Kalantar Nayestanaki; O., Kalekin; A., Kappes; U., Katz; P., Kooijman; C., Kopper; A., Kouchner; W., Kretschmer; R., Lahmann; P., Lamare; G., Lambard; G., Larosa; H., Laschinsky; D., Lefevre; G., Lelaizant; G., Lim; D., Lopresti; D., Lo Presti; H., Loehner; S., Loucatos; Lucarelli, Fabrizio; K., Lyons; S., Mangano; M., Marcelin; A., Margiotta; J. A., Martinez Mora; G., Maurin; A., Mazure; M., Melissas; T., Montaruli; M., Morganti; L., Moscoso; H., Motz; C., Naumann; M., Neff; R., Ostasch; G., Palioselitis; G. E., Pavalas; P., Payre; J., Petrovic; P., Piattelli; N., Picot Clemente; C., Picq; R., Pillet; V., Popa; T., Pradier; E., Presani; C., Racca; A., Radu; C., Reed; G., Riccobene; C., Richardt; M., Rujoiu; G. V., Russo; F., Salesa; F., Schoeck; J. P., Schuller; R., Shanidze; Simeone, Francesco; M., Spurio; J. J. M., Steijger; Th, Stolarczyk; C., Tamburini; L., Tasca; S., Toscano; B., Vallage; V., Vanelewyck; V., Van Elewyck; Vecchi, Manuela; P., Vernin; G., Wijnker; E., Dewolf; E., De Wolf; H., Yepes; D., Zaborov; J. D., Zornoza; J., Zuniga. - In: DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS. - ISSN 0967-0637. - STAMPA. - 58:8(2011), pp. 875-884. [10.1016/j.dsr.2011.06.006]
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11573/381456
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