Titlebook: Antarctic Peninsula Region of the Southern Ocean; Oceanography and Eco Eugene G. Morozov,Mikhail V. Flint,Vassily A. Spir Book 2021 The Edi

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https://doi.org/10.1007/3-8350-5716-2Strait and Powell Basin) based on the data collected during cruise 79 of the R/V “Akademik Mstislav Keldysh” in the austral summer of 2020 (January 11–February 4). Chlorophyll . concentration, spectral light absorption coefficients of phytoplankton, non-algal particles (NAP), and colored dissolved o

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https://doi.org/10.1007/3-8350-5716-2la (Bransfield Strait and Antarctic Sound) are presented. It was found that bio-optical parameters in the main stream of the Falkland (Malvinas) Current are lower than in the surrounding waters. Upwelling was observed in the western periphery of the current, which contributes to the ascent of nutrie

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Antarctic Peninsula Region of the Southern Ocean978-3-030-78927-5Series ISSN 2468-5712 Series E-ISSN 2468-5720

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https://doi.org/10.1007/978-3-531-90178-7etected, and an intense mixing zone of waters from the Weddell Sea and Bransfield Strait was distinguished. Water inflow from the Weddell Sea to the Antarctic Sound occurs less frequently than the flow from the Bransfield Strait. The main flow of water is directed to the south.

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https://doi.org/10.1007/978-3-531-90178-7ated. Differentiating storm waves and rogue waves is often difficult. This article provides information about the observations of rogue waves and possible mechanisms for their generation in the Antarctic Circumpolar Current. It has been noted that such anomalous waves can also occur in the depths of the ocean, due to water stratification.

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Advances in Polar Ecologyhttp://image.papertrans.cn/a/image/158189.jpg

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