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  • 1
    Publication Date: 2023-08-08
    Description: Through the Cooperative Study of the Kuroshio and Adjacent Regions (CSK) program during 1965–1979, the capacities of current member states (MSs) of the Sub-Commission for the Western Pacific (WESTPAC) of the Intergovernmental Oceanographic Commission (IOC) were enhanced with regard to regional ocean science and data management. Following the termination of the CSK in 1979, each MS continued the work to advance ocean science. The results of scientific studies of the Kuroshio and its adjacent regions have been published by various experts including many from the MSs of the WESTPAC; however, to-date, there has been no systematic approach to the research of the Kuroshio and its adjacent regions. This review considered the Kuroshio from the regional perspective of experts of the MSs, that is, from the perspectives of MSs, science, and the future prospects. Experts from each MS reviewed past activities and con tributions and reviewed the knowledge gaps in the fields of physical, biological, and biogeochemical science. Many scientific questions remain regarding the path of the Kuroshio from south to north, as well as associated phenomena, including mesoscale eddies and fronts, the important roles of ocean variations in adjacent regions, and the different roles and mechanisms of air–sea interactions in low- and mid-latitude areas. Despite consid erable effort by many biologists, substantial gaps remain in our biological knowledge of the region. The Kuroshio and its adjacent regions comprise one of the areas of the world with high biodiversity; however, there has been insufficient research into what is the cause of this high biodiversity. From a biogeochemical aspect, high resolution spatiotemporal observations will be required to understand interactions with physical processes both in the Kuroshio region and in the marginal seas. It has been highlighted that long-term fixed-location observations will be needed to understand the key mechanisms of biogeochemical processes, particularly in relation to climate change.
    Description: From Decade Action UN24. Explore the strongest ocean current in the Western Pacific: the 2nd Cooperative Study of Kuroshio and Adjacent Regions – from its sciences to human well beings (CSK-2)
    Description: Published
    Description: Refereed
    Keywords: Marginal seas ; CSK ; IOC ; WESTPAC
    Repository Name: AquaDocs
    Type: Journal Contribution
    Format: 35pp.
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  • 2
    Publication Date: 2013-11-26
    Description: [1]  We investigated the impacts of the preceding Arctic Oscillation (AO) on winter East Asian temperature (T EA ) and the possible mechanisms. It was found that the correlation of the November AO (Nov AO) with the following January T EA is more significant than that with the following December and February T EA . Moreover, the January T EA is also closely related to the preceding December AO (Dec AO). Further analysis revealed that a Rossby wave associated with the Nov AO is confined to high latitudes in December, but shifts southeastward to East Asia in January. Similarly, the Dec AO-related wave activities propagating southeastward to East Asia could persist into the following January. Consequently, the signals of the Nov/Dec AO could be transmitted to the following January. Besides, an air–sea interaction might exist over the North Pacific (NP). The sea surface temperature (SST) over the central subtropical NP (west coast of North America) often rapidly rises (drops) a month later and peaks in the following January when the preceding Nov/Dec AO is in positive phase, causing horseshoe SST anomalies (SSTAs) to form in the NP, with positive SSTAs located in the central subtropical NP, and surrounded by negative ones. Such a horseshoe SSTAs could lead to a strengthening of the air temperature gradient in the north and a weakening in the south due to effective turbulent mixing in the boundary layer. A huge anomalous anticyclone therefore emerges in the NP and favors a weaker East Asian winter monsoon. Warmer January T EA is eventually generated.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
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