Abstract The Kara and Laptev seas receive about one half of total freshwater runoff to the
Arctic Ocean from the Ob, Yenisei, and Lena rivers. Discharges of these large rivers form …

This work is focused on the seasonal and interannual variability of the freshened surface
layer (FSL) in the Kara Sea during ice‐free periods. The majority of annual freshwater runoff …

Water and sediment supply are essential to the health of deltaic ecosystems. Diverse
datasets were integrated to better understand how climate change is shifting the supply of …

This study presents detailed suspended sediment budget for the four Siberian river deltas,
representing contrasting conditions between Northern and Southern environments. Two of …

This work is focused on the structure and inter-annual variability of the freshened surface
layer (FSL) in the Laptev and East-Siberian seas during ice-free periods. This layer is …

The Northeast Caucasian Current (NCC) is the northeastern part of the cyclonic Rim Current
(RC) in the Black Sea. As it sometimes approaches the narrow shelf very closely …

The Yenisei and Khatanga rivers are among the largest estuarine rivers that inflow to the
Arctic Ocean. Discharge of the Yenisei River is one order of magnitude larger than that of the …

The major Siberian rivers form large river plumes in the Arctic Ocean, which govern structure
of the sea surface layer at the Arctic shelf. These river plumes were explicitly studied during …

Unprecedented rates of climate change in the Arctic are causing altered land to ocean
transport of dissolved organic matter (DOM) and subsequent processing in the Arctic Ocean …

Wind forcing is the main driver of river plume dynamics. Direction and magnitude of wind
determine position, shape, and size of a river plume. The response of river plumes on wind …