Titlebook: Changing Asia-Pacific Marginal Seas; Chen-Tung Arthur Chen,Xinyu Guo Book 2020 Springer Nature Singapore Pte Ltd. 2020 Asia-Pacific Margin

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R. Bianchi,G. Mariani,A. Pilo,M. G. Toni the interior of the sea. However, recent weakening of this overturning circulation has decreased the transport of anthropogenic CO. and O. from the surface to the interior of the sea, but accelerated the acidification of deep water in the basin; the rate of acidification in the deep water is higher

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Negative Ion Source Technology,Ss are?also changing rapidly which include the change of sea surface temperature (SST), water masses and sea level etc. These parameters are very sensitive to the global warming due to the shallow water depth of the BYSs. The SST in the BYSs shows an increasing trend of 0.8 to 2 °C per century, near

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,Charged Dust in the Earth’s Magnetosphere,ynthesizing literature data, basin-wide decadal changes in nutrients and bottom-water dissolved oxygen and carbonate system parameters in the two coastal oceans were investigated. Results showed that both of the two coastal oceans were subject to basin-wide increases in wintertime nitrate during the

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Impurity Problems in Fusion Experimentsoncentrations were mainly due to the increases of DIN and DIP in the Changjiang (Yangtze) River since 1980s. As a result, phytoplankton abundance increased dramatically between 1958 and 2016 in both the Changjiang Estuary and the East China Sea. Before 1980s, chain-forming diatoms were dominant, whi

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https://doi.org/10.1007/3-540-32149-7lated by the variation of ocean circulation, which is, in turn, governed by the geophysical fluid dynamics in the circulation. This chapter provides an overview and analysis on the predominant cyclonic-anticyclonic-cyclonic (CAC) circulation, and the associated processes and responses of the hydrogr

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https://doi.org/10.1007/3-540-32149-7on the Extreme Cold Water Events (ECWEs) that occur during winter–spring near the Japanese coast adjacent to the Oyashio. The southernmost latitude of the First Oyashio Intrusion migrated southward in response to the basin-scale wind stress from the mid-1960s to the mid-1980s, while it changed less

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Energy Problem and Related Safety Aspectsater mass formation, hence the transport of anthropogenic CO. into the interior North Pacific. Currently, it is unclear how the air-sea CO. fugacity gradient in the climatically sensitive Oyashio Region has been behaving in recent decades. Taking advantage of a community-based Surface Ocean CO. Atla

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