Hydrochemical features of the Kara Sea aquatic area in summer 2015


Cite item

Full Text

Open Access Open Access
Restricted Access Access granted
Restricted Access Subscription Access

Abstract

During cruise 65 of the R/V Akademik Mstislav Keldysh in the Kara Sea, three transects were executed: one eastwards from the Novaya Zemlya Archipelago and two in the St. Anna and Voronin troughs. It was noted that the continental runoff affected the entire surveyed aquatic area, even at the northern extremity of the Novaya Zemlya Archipelago. The transect along the St. Anna Trough showed the presence of a slope frontal zone overlaid at the surface by a desalinated layer. The Voronin Trough was characterized by sliding of slope waters. The hydrochemical parameters show that the surveys were carried out during a recession of biological activity of the waters and that the peak bloom was over by that time. The hydrochemical structure of waters conformed to early autumn conditions, but before the beginning of intense cooling of surface waters.

About the authors

P. N. Makkaveev

Shirshov Institute of Oceanology

Author for correspondence.
Email: makkaveev55@mail.ru
Russian Federation, Moscow

A. A. Polukhin

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
Russian Federation, Moscow

A. V. Kostyleva

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
Russian Federation, Moscow

E. A. Protsenko

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
Russian Federation, Moscow

S. V. Stepanova

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
Russian Federation, Moscow

Sh. Kh. Yakubov

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
Russian Federation, Moscow

Supplementary files

Supplementary Files
Action
1. JATS XML

Copyright (c) 2017 Pleiades Publishing, Inc.