Physical oceanography and ADCP measurements during Maria S. Merian cruise MSM13/2

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Détails bibliographiques
Auteur principal:	Hainbucher, Dagmar
Format:	Dataset Open Access
Langue:	en
Publié:	PANGAEA 2016
Accès en ligne:	Acceder al recurso
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author	Hainbucher, Dagmar
author_facet	Hainbucher, Dagmar
collection	Datos científicos de ciencias marinas y ambientales
contents	Up to the end of the eighties the main source of deep water masses in the Ionian Basin was the southern Adriatic Sea. However, during the nineties a dramatic climatic change took place in the eastern Mediterranean Sea: the Eastern Mediterranean Transient (EMT). Since then, deep water has been formed by waters originating in the Aegean Sea. Expeditions carried out in this region in recent years indicate that the process of deep water formation might reverse again. To what extent this assumption applies and what characteristics the deep water in the Ionian Sea exhibit nowadays, should be determined on the cruise. The process of a re-reversal of abyssal water production in the Ionian Sea is a long-term process and must therfore be monitored for several years. Hence, this cruise is part of a series of cruises investigating this question (POS98, M71/3, MSM13/1-2, MSM15/4). The investigations were carried out by means of CTD/lADCP measurements.
format	Dataset Open Access
id	pangaea_https___doi_org_10_1594_PANGAEA_856696
institution	PANGAEA
language	en
publishDate	2016
publisher	PANGAEA
record_format	pangaea
spellingShingle	Physical oceanography and ADCP measurements during Maria S. Merian cruise MSM13/2 Hainbucher, Dagmar Up to the end of the eighties the main source of deep water masses in the Ionian Basin was the southern Adriatic Sea. However, during the nineties a dramatic climatic change took place in the eastern Mediterranean Sea: the Eastern Mediterranean Transient (EMT). Since then, deep water has been formed by waters originating in the Aegean Sea. Expeditions carried out in this region in recent years indicate that the process of deep water formation might reverse again. To what extent this assumption applies and what characteristics the deep water in the Ionian Sea exhibit nowadays, should be determined on the cruise. The process of a re-reversal of abyssal water production in the Ionian Sea is a long-term process and must therfore be monitored for several years. Hence, this cruise is part of a series of cruises investigating this question (POS98, M71/3, MSM13/1-2, MSM15/4). The investigations were carried out by means of CTD/lADCP measurements.
title	Physical oceanography and ADCP measurements during Maria S. Merian cruise MSM13/2
topic
url	https://doi.org/10.1594/PANGAEA.856696

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