Hydrochemical features of the Kara Sea aquatic area in summer 2015


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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.

作者简介

P. Makkaveev

Shirshov Institute of Oceanology

编辑信件的主要联系方式.
Email: makkaveev55@mail.ru
俄罗斯联邦, Moscow

A. Polukhin

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
俄罗斯联邦, Moscow

A. Kostyleva

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
俄罗斯联邦, Moscow

E. Protsenko

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
俄罗斯联邦, Moscow

S. Stepanova

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
俄罗斯联邦, Moscow

Sh. Yakubov

Shirshov Institute of Oceanology

Email: makkaveev55@mail.ru
俄罗斯联邦, Moscow

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