High salinity winter outflow from a mega inverse-estuary—the Great Australian Bight

Conductivity-temperature-depth (CTD) observations taken in the Great Australian Bight (GAB) during ORV Franklin cruise Fr 07/94 in July 1994 indicated the presence of a dense bottom layer at the head of the GAB, which flowed along the sea floor towards the shelf-break as a gravity current The north...

Ausführliche Beschreibung

Bibliographische Detailangaben

Veröffentlicht in:	Continental shelf research 2009-02, Vol.29 (2), p.371-380
Hauptverfasser:	Petrusevics, P., Bye, J.A.T., Fahlbusch, V., Hammat, J., Tippins, D.R., van Wijk, E.
Format:	Artikel
Sprache:	eng
Schlagworte:	Brackish Great Australian Bight Inverse-estuary Marine Mass budgets Winter density outflow
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!