Titlebook: Atlantic Water in the Nordic Seas; Properties, Variabil Waldemar Walczowski Book 2014 Springer International Publishing Switzerland 2014 Ar

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Introduction,ent of the system. For it is the ocean and life that originated there that created the atmosphere and has shaped its composition for billions of years. It is particularly important to speak about it now—in time of increased concern about the climate, when the out-of-control human impact upon the condition of the atmosphere is visible.

Prognosis

Methodology of Measurements and Data Analysis,vessel ‘Oceania’ sails out for an expedition. The cruises are held under an original research program of the Institute of Oceanology—AREX. After years of experience, an optimum pattern of research seems to have been developed.

Osmosis

Dynamics of the West Spitsbergen Current,ge errors. It is affected by several factors. The first of them is the point of reference. Measurements are performed from an observation platform which moves in all planes, and vertical accelerations are sometimes significant.

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Changes in the Ocean Climate,mate, and due to the specific nature of the studied area, also the global climate. It was described in Chapter 7. In situ observed currents are more intense and variable. It results in oceanic transport and ocean–atmosphere heat fluxes larger than described. We have witnessed important climate change in recent years.

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Roza Aseeva,Boris Serkov,Andrey Sivenkov Seas, as well. In the 1980s, American oceanographic literature made unsuccessful attempts to call them “The GIN Seas” (from the first letters of the seas). Although they cover only a small part of the world ocean, the Nordic Seas play unusual role in its circulation and the dynamics of the northern

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Springer Series in Wood Sciencevessel ‘Oceania’ sails out for an expedition. The cruises are held under an original research program of the Institute of Oceanology—AREX. After years of experience, an optimum pattern of research seems to have been developed.

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Kaivon Sobhani,Jinlei Li,Milaurise Cortesmate, and due to the specific nature of the studied area, also the global climate. It was described in Chapter 7. In situ observed currents are more intense and variable. It results in oceanic transport and ocean–atmosphere heat fluxes larger than described. We have witnessed important climate chang

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