Distribution and composition of suspended particulate matter in the Atlantic Ocean: Direct measurements and satellite data


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The main purpose of this work is to study the real distribution and spatial–temporal variations of suspended particulate matter and its main components in surface waters of the Atlantic Ocean on the basis of direct and satellite measurements for development of new and perfection of available algorithms for converting satellite data. The distribution fields of suspended particulate matter were calculated and plotted for the entire Atlantic Ocean. It is established that its distribution in the open ocean is subordinate to the latitudinal climatic zonality. The areas with maximum concentrations form latitudinal belts corresponding to high-productivity eutrophic and mesotrophic waters of the northern and southern temperate humid belts and with the equatorial humid zone. Phytoplankton, the productivity of which depends primarily on the climatic zonality, is the main producer of suspended particulate matter in the surface water layer.

Sobre autores

A. Lisitzin

Shirshov Institute of Oceanology

Email: klyuvitkin@ocean.ru
Rússia, Nakhimovskii pr. 36, Moscow, 117218

A. Klyuvitkin

Shirshov Institute of Oceanology

Autor responsável pela correspondência
Email: klyuvitkin@ocean.ru
Rússia, Nakhimovskii pr. 36, Moscow, 117218

V. Burenkov

Shirshov Institute of Oceanology

Email: klyuvitkin@ocean.ru
Rússia, Nakhimovskii pr. 36, Moscow, 117218

M. Kravchishina

Shirshov Institute of Oceanology

Email: klyuvitkin@ocean.ru
Rússia, Nakhimovskii pr. 36, Moscow, 117218

N. Politova

Shirshov Institute of Oceanology

Email: klyuvitkin@ocean.ru
Rússia, Nakhimovskii pr. 36, Moscow, 117218

A. Novigatsky

Shirshov Institute of Oceanology

Email: klyuvitkin@ocean.ru
Rússia, Nakhimovskii pr. 36, Moscow, 117218

V. Shevchenko

Shirshov Institute of Oceanology

Email: klyuvitkin@ocean.ru
Rússia, Nakhimovskii pr. 36, Moscow, 117218

T. Klyuvitkina

Department of Geography

Email: klyuvitkin@ocean.ru
Rússia, Moscow

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