Structure of the buoyant plume formed by Ob and Yenisei river discharge in the southern part of the Kara Sea during summer and autumn

Alexander Osadchiev1, Alexander Izhitskiy2, Peter O Zavialov2, Viacheslav Kremenetskiy2, Alexander Polukhin3, Vadim Pelevin2 and Zhamal Toktamysova4, (1)Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia, (2)Shirshov Institute of Oceanology, Physical Oceanography, Moscow, Russia, (3)Shirshov Institute of Oceanology, Marine Ecology, Moscow, Russia, (4)National Research University Higher School of Economics, Moscow, Russia
Back to: The Dynamics of Estuaries and Coastal Buoyancy-Driven Flows II