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  • 1
    Keywords: marine environment ; environmental pollution ; marine pollution
    Description / Table of Contents: Ecosystem Modeling of the Oregon Shelf: Everything but the Kitchen Sink / Y. H. Spitz / pp. 1-9 --- Marine Ecosystem Simulation in the Indonesian Seas / Y. Sasai, A. R. Kartadikaria, Y. Miyazawa and K. Nadaoka / pp. 11-17 --- Response of Nutrients and Primary Production over the Shelf in the East China Sea to the Reduction of Oceanic Nutrient Supply / X. Guo and L. Zhao / pp. 19-30 --- Introduction of the Ecological Connectivity Hypoxia Model: ECOHYM—Model Concept and Its Validation on a Study Applied to Tokyo Bay / A. Sohma / pp. 31-38 --- Ecosystem and Nutrient Dynamics in the Seto Inland Sea, Japan / N. Yoshie, X. Guo, N. Fujii and T. Komorita / pp. 39-49 --- A Numerical Modeling Study of Japanese Sardine (Sardinops melanostictus) Migrations in the Western North Pacific / T. Okunishi, D. Ambe, S. Ito, T. Kameda, T. Setou, K. Komatsu, A. Kawabata, A. Takasuka and H. Kubota / pp. 51-56 --- Investigating Alternate Trophic Pathways through Gelatinous Zooplankton and Planktivorous Fishes in an Upwelling Ecosystem Using End-to-End Models / R. D. Brodeur, J. J. Ruzicka and J. H. Steele / pp. 57-63 --- Establishing a Conceptual Design for Jellyfish Blooms in the Seto Inland Sea / N. Fujii, A. Kaneda, S. Magome and H. Takeoka / pp. 65-71 --- Fate Prediction Model of Organic Chemicals in Coastal Bay Estuaries / K. Nakata, F. Horiguchi and T. Eriguchi / pp. 73-77 --- Ecosystem Analysis of the Seto Inland Sea: Bioaccumulation Model on a Basis of an Energy Balance Model / K. Omori, J. Shibata, H. Hamaoka, K. Matsumoto, T. Nanko, T. Kunihiro, T. W. Miller and H. Onishi / pp. 79-83 --- Trophic Dynamics of Pelagic Nekton in the Southern Benguela Current Ecosystem: Calibrating Trophic Models with Stable Isotope Analysis / C. D. van der Lingen and T. W. Miller / pp. 85-94 --- Tracing Dynamics of Organic Material Flow in Coastal Marine Ecosystems: Results from Manila Bay (Philippines) and Kyucho Intrusion (Japan) / T. W. Miller, G. Jaquinto, M. McGlone, A. Isobe, J. Shibata, H. Hamaoka and K. Omori / pp. 95-104 --- Variations of Seawater Temperature and Coastal Winds from 2003 to 2009 at the Bungo Channel, Japan / R. Shi, X. Guo and H. Takeoka / pp. 105-115 --- Spatial Variation of Submarine Groundwater Discharge (SGD) in the Central Part of Seto Inland Sea, Japan / M. Saito, X. Guo, S. Onodera, Y. Shimizu, Y. Kato, M. Tokumasu and H. Takeoka / pp. 117-123 --- Understanding What Drives Food Web Structure in Marine Pelagic Ecosystems / T. W. Miller, C. van der Lingen, R. Brodeur, K. Omori, H. Hamaoka and T. Isobe / pp. 125-131 --- Study of Sediment Cleanup Using Polychaetes / K. Ito, M. Nozaki, T. Kunihiro, C. Miura and T. Miura / pp. 133-139 --- Regional Characteristics of Lower Trophic Level Food Web Structure in the Seto Inland Sea / J. Shibata, H. Hamaoka, R. Isonaka, K. Matsumoto, T. Nanko, T. W. Miller, H. Onishi, T. Kunihiro and K. Omori / pp. 141-149 --- Sources of Sedimentary Organic Carbon in Mangrove Ecosystems from Ba Lat Estuary, Red River, Vietnam / N. T. Tue, H. Hamaoka, A. Sogabe, T. D. Quy, M. T. Nhuan and K. Omori / pp. 151-157 --- The Fish Composition of Phan Thiet Bay, Binh Thuan Province, Vietnam in Connection with Environmental Quality / N. T. Nam, N. X. Huan, V. T. Tang, T. W. Miller and K. Omori / pp. 159-167 --- The Roles of Marine Phytoplankton and Ocean Circulation in Determining the Global Fate of Polychlorinated Biphenyls / T. Kawai, I. C. Handoh and N. Suzuki / pp. 169-178 --- Bayesian Uncertainty Analysis of the Global Dynamics of Persistent Organic Pollutants: Towards Quantifying the Planetary Boundaries for Chemical Pollution / I. C. Handoh and T. Kawai / pp. 179-187 --- What Drives the Fate of Persistent Organic Pollutants in the North Sea? Insights from a Regional Model / T. Ilyina / pp. 189-195 --- Process Study on Numerical Simulation for Persistent Organic Pollutants in the East China Sea / J. Ono, D. Takahashi, X. Guo, S. Takahashi and H. Takeoka / pp. 197-204 --- Monitoring of Contamination by Non-PBDE Brominated Flame Retardants in Asian Coastal Waters Using Mussels as a Bioindicator / S. Ogawa, T. Isobe, K. Ramu, A. Subramanian, S. Takahashi and S. Tanabe / pp. 205-211 --- Inter-species Differences of Hydroxylated Polychlorinated Biphenyls (OHPCBs) in the Blood of Small Cetaceans / M. Ochiai, K. Nomiyama, T. Isobe, T. Matsuishi, T. K. Yamada and S. Tanabe / pp. 213-220 --- Accumulation of Brominated Flame Retardants in Harbour and Dall's Porpoises from Hokkaido / A. Saito, T. Isobe, T. Matsuishi, T. K. Yamada, Y. Tajima and S. Tanabe / pp. 221-228 --- Contamination by Brominated Flame Retardants (BFRs) in Common Cormorants from Lake Biwa / R. Hashikawa, T. Isobe, S. Yano, T. Kunisue, K. Nakayama, A. Sudo, S. Takahashi and S. Tanabe / pp. 229-238 --- Formulation of Leeway-Drift Velocities for Sea-Surface Drifting-Objects Based on a Wind-Wave Flume Experiment / A. Isobe, H. Hinata, S. Kako and S. Yoshioka / pp. 239-249 --- Investigating the Accumulation of Plastic Debris in the North Pacific Gyre / J. J. Leichter / pp. 251-259 --- Deep-Sea Litter Study Using Deep-Sea Observation Tools / H. Miyake, H. Shibata and Y. Furushima / pp. 261-269 --- Toxic Metals in Polyethylene Plastic Litter / E. Nakashima, A. Isobe, S. Kako, S. Magome, N. Deki, T. Itai and S. Takahashi / pp. 271-277
    Pages: Online-Ressource (IX, 277 Seiten)
    ISBN: 9784887041547
    Language: English
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2006. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 111 (2006): C03012, doi:10.1029/2005JC003290.
    Description: The Finite Volume Coastal Ocean Model (FVCOM) is used to estimate the onshore cross-frontal transport at the shelf break of the East China Sea. Boundary conditions of FVCOM are provided by the Princeton Ocean Model simulating ocean currents in the Yellow Sea and East China Sea realistically. One advantage of this study is that the unstructured triangular cell grid of FVCOM resolves complex bottom topography that may trigger Kuroshio frontal waves. It is anticipated that these nonlinear frontal waves enhance the exchange of seawater between the Kuroshio and shelf regions. Kuroshio frontal waves in the model are excited around the location where the bottom slope changes abruptly, and have the phase speed and amplitude consistent with those observed in the East China Sea. In addition, the model reproduces the onshore transport associated with growing frontal waves in the upper and lower layers. On the basis of passive tracer experiments, the annually averaged onshore-transport integrated along the shelf break is estimated to be 0.85 × 106 m3/s.
    Description: This study was carried out when A. I. stayed at WHOI with the grant of Overseas Advanced Educational Research Practice Support Program supported by the Ministry of Education, Science and Culture, Japan. In addition, the Japan Society for the Promotion of Science supported this study through Grant-in-Aid for Scientific Research.
    Keywords: East China Sea ; Kuroshio frontal wave ; Cross-frontal transport ; FVCOM
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 3
    Publication Date: 2022-05-25
    Description: Author Posting. © American Meteorological Society, 2007. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Climate 20 (2007): 5707–5714, doi:10.1175/2007JCLI1779.1.
    Description: The interannual variation in cold-air outbreak activity over the Japan Sea is investigated using Japan Meteorological Agency buoy 21002 and Quick Scatterometer (QuikSCAT) wind data, Japan Oceanographic Data Center sea surface temperature (SST) data, NCEP–NCAR reanalysis surface wind and sea level pressure (SLP) data, and the winter Arctic Oscillation (AO) index of Thompson and Wallace. Cold-air outbreaks occur during the “winter” November–March period, and wind data for this season for the 19-winter period 1981–2000 were analyzed. Wavelet spectra averaged between 5- and 15-day periods were used to evaluate the intensity of cold-air outbreaks quantitatively. The winter mean wavelet spectra exhibited a clear interannual variation and a significant positive correlation with the AO index, indicating that intensive cold-air outbreaks frequently occur during relatively warm winters caused by a quasi-decadal AO. Based on the SST and SLP data, the low atmospheric surface pressure disturbances tend to develop over the warm East China Sea in warm winters in the positive AO phase. As these low SLP disturbances advance toward the northern Japan islands during the positive AO phase, they intensify more, leading to stronger cold-air outbreaks over the Japan Sea and increased sea surface cooling over the northern Japan Sea.
    Keywords: Air-sea interactions ; Interannual variation ; Arctic Oscillation ; Remote sensing ; Buoy observations
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Journal of oceanography 55 (1999), S. 185-195 
    ISSN: 1573-868X
    Keywords: Taiwan-Tsushima Warm Current System ; East China Sea
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Using a temperature data set from 1961 to 1990, we estimated the monthly distribution of the vertically integrated heat content in the East China Sea. We then drew the monthly map of the horizontal heat transport, which is obtained as the difference between the vertically integrated heat content and the surface heat flux. We anticipate that its distribution pattern is determined mainly due to the advection by the ocean current if it exists stably in the East China Sea. The monthly map of the horizontal heat transport showed the existence of the Taiwan-Tsushima Warm Current System (TTWCS) at least from April to August. The T-S (temperature-salinity) analysis along the path of TTWCS indicated that the TTWCS changes its T-S property as it flows in the East China Sea forming the Tsushima Warm Current water. The end members of the Tsushima Warm Current water detected in this study are water masses in the Taiwan Strait and the Kuroshio surface layer, the fresh water from the mainland of China, and the southern tip of the Yellow Sea Cold Water extending in the northern part of the East China Sea.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Journal of oceanography 50 (1994), S. 617-633 
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The seasonal variation in the barotropic mode of motion caused by joint effect of the baroclinicity and bottom relief (Jebar effect) in the Tsushima Strait is investigated with the use of the diagnostic numerical model in this study. The Jebar effect in the Tsushima Strait is mainly caused by the intrusion of the Bottom Cold Water along the Korean coast in summer. This Jebar effect along the Korean coast locally supplies the negative vorticity in situ, and it forces the coastal current to be intensified. In summer, the volume transport of the Tsushima Warm Current entering the Tsushima Strait is biassed to the western part of the strait comparing with the flow pattern calculated in winter.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1573-868X
    Keywords: Mixed warm water mass ; low-salinity water ; Tsushima Straits ; East China Sea
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Sea surface temperature (SST) and sea surface salinity variations at Fukue Island (located southwest of the Tsushima Straits) were investigated. In spring, low-frequency SST fluctuations with periods of 10–20 days predominate. Synthetic analysis of in situ observation and satellite infrared image reveals that these SST fluctuations are caused by movement of mixed warm water masses which have a temperature intermediate between those of the Kuroshio and the East China Sea (ECS) shelf waters. Since these fluctuations do not correspond with those in the Tsushima Straits, it is indicated that these water masses can hardly pass the Tsushima Straits while retaining their original water properties. In July, SST fluctuations with a period of several days are also found at Fukue Island. Since these SST fluctuations show an opposite correspondence with its salinity fluctuations and a good correspondence with the SST fluctuations at Okinoshima in the Tsushima Straits, it is inferred that warm and low-salinity water originated from the ECS shelf water causes these fluctuations and intrudes into the Tsushima Straits.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Journal of oceanography 50 (1994), S. 223-238 
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The aim of this study is to elucidate the seasonal variation in the volume transport through the Tsushima-Korea Strait using the sea level difference across the Strait. The sea level difference associated with the baroclinic motion is estimated from the geostrophic current profile, which is calculated as its vertical integrated transport is zero, using the CTD data from 1988 to 1990. The sea level difference associated with the barotropic motion is estimated by subtracting the sea level difference associated with the baroclinic motion from the observed one. The range (maximum-minimum) of the seasonal variation in the volume transport is evaluated about 0.7 Sv on the average, using the sea level difference associated with the barotropic motion. It is one third of the seasonal variation in the volume transport which is estimated from observed sea level difference on the assumption that no baroclinic component exists. Such analyses also indicate that the volume transport was at a maximum in early winter and at a minimum in early spring from 1988 to 1990. The negative correlation is also found between the volume transport through the eastern channel and that through the western channel. Moreover, it is noticed that the seasonal variation in the surface current velocity in the Strait largely contains baroclinic motions which are locally caused in the Tsushima-Korea Strait.
    Type of Medium: Electronic Resource
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  • 8
    Publication Date: 2004-01-01
    Print ISSN: 0916-8370
    Electronic ISSN: 1573-868X
    Topics: Geosciences , Physics
    Published by Springer
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  • 9
    Publication Date: 2008-08-01
    Print ISSN: 0916-8370
    Electronic ISSN: 1573-868X
    Topics: Geosciences , Physics
    Published by Springer
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  • 10
    Publication Date: 2010-03-25
    Print ISSN: 0916-8370
    Electronic ISSN: 1573-868X
    Topics: Geosciences , Physics
    Published by Springer
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