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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Oceanography. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (467 pages)
    Edition: 1st ed.
    ISBN: 9783319227207
    DDC: 551.461454
    Language: English
    Note: Intro -- Preface -- Contents -- Contributors -- Abbreviations -- 1 General Introduction -- Abstract -- 1.1 Geography and Topography -- 1.2 History of Hydrographic Surveys -- 1.3 CREAMS Program -- 1.3.1 Important Findings Before CREAMS -- 1.3.2 CREAMS Studies -- 1.3.2.1 Important Discovery I: Oceanic Structures -- 1.3.2.2 Important Discovery II: Dramatic Structural Changes in the East Sea -- 1.3.3 Globalization of East Sea Studies -- 1.3.3.1 The Birth of CREAMS-II -- 1.3.3.2 CREAMSPICES EAST (East Asian Seas Time Series)-I Program -- 1.3.3.3 IPCC 4th Report and Nobel Peace Prize, 2007 -- 1.3.4 Concluding Remarks -- 1.4 Recent Observational Programs -- 1.4.1 Surface Drifters -- 1.4.2 Argo (Array for Real-Time Geostrophic Oceanography) -- 1.4.3 Moored Current Observations -- 1.4.4 Satellite Oceanography -- References -- 2 Forcings -- Abstract -- 2.1 Introduction -- 2.2 Surface Wind -- 2.2.1 Accuracy of Satellite Scatterometer Wind Vectors -- 2.2.2 Spatial and Temporal Variability of Near-Surface Winds -- 2.2.3 Wind Stress and Its Curl -- 2.3 Surface Heat Flux -- 2.3.1 Comparison of Heat Flux Estimates -- 2.3.2 Temporal Variations -- 2.3.3 Spatial Distribution -- 2.4 Boundary Flux -- 2.4.1 Korea Strait -- 2.4.2 Tsugaru Strait and Soya Strait -- 2.4.3 Long-Term Variability -- 2.5 Summary and Discussion -- References -- 3 Water Masses and Their Long-Term Variability -- Abstract -- 3.1 Introduction -- 3.2 Sea Surface Temperature and Mixed Layer Depth -- 3.2.1 Sea Surface Temperature -- 3.2.2 Surface Front -- 3.2.3 Mixed Layer Depth -- 3.3 Water Masses -- 3.3.1 Upper Ocean Water Masses -- 3.3.1.1 Tsushima Warm Water -- 3.3.2 Intermediate Waters -- 3.3.2.1 East Sea Intermediate Water -- 3.3.2.2 High Salinity Intermediate Water -- 3.3.2.3 North Korea Cold Water -- 3.3.2.4 Korea Strait Bottom Cold Water -- 3.3.3 Central Water, Deep Water, and Bottom Water. , 3.4 Long-Term Variability of Water Properties -- 3.4.1 Water Masses in Change -- 3.4.2 Interannual and Decadal Variation of the Upper Ocean -- 3.4.2.1 Upper Ocean Temperature -- 3.4.2.2 Sea Surface Height -- 3.5 Summary and Remaining Questions -- References -- 4 Circulation -- Abstract -- 4.1 Introduction -- 4.2 Near-Surface Circulation -- 4.2.1 Mean Surface Current -- 4.2.2 Variability of the Surface Current and the Subpolar Front -- 4.2.3 Coastal Upwelling -- 4.3 Mesoscale Eddies -- 4.3.1 Characteristics of Eddies -- 4.3.2 Evolution of the Ulleung Warm Eddy -- 4.4 Thermohaline Circulation -- 4.4.1 Rates of Water Mass Formation -- 4.4.2 Deep Currents and Circulation -- 4.4.2.1 Mean Currents -- 4.4.2.2 Temporal Variability -- 4.5 Dynamical Aspects -- 4.5.1 How Is the Tsushima Warm Current Driven? -- 4.5.2 How Are the Branches of the Tsushima Warm Current Formed? -- 4.5.3 What Is the Role of Local Forcing? -- 4.5.4 How Is the Deep Layer Circulation Driven? -- 4.6 Numerical Modeling Studies of Circulation -- 4.6.1 Numerical Simulations -- 4.6.2 Data Assimilation and Forecasting Systems -- 4.7 Summary and Discussion -- References -- 5 High-Frequency Variability: Basin-Scale Oscillations and Internal WavesTides -- Abstract -- 5.1 Introduction -- 5.2 Basin-Scale Oscillations -- 5.2.1 Observations -- 5.2.2 Analytic Model and Applications -- 5.3 Surface and Internal Tides -- 5.3.1 Observations -- 5.3.2 Models and Applications -- 5.4 Near-Inertial Oscillations -- 5.4.1 Observations -- 5.4.2 Generation and Propagation of Near-Inertial Waves -- 5.5 Nonlinear Internal Waves -- 5.5.1 Observations -- 5.5.2 Generation and PropagationRefraction of Nonlinear Internal Waves -- 5.6 Conclusion and Remaining Issues -- References -- 6 Dissolved Oxygen and Nutrients -- Abstract -- 6.1 Introduction -- 6.2 Dissolved Oxygen -- 6.2.1 History of DO Measurements. , 6.2.2 Vertical Structure of DO Profile -- 6.2.3 Trend of DO Inventory in the Bottom Layer -- 6.2.4 Projecting DO Inventory in Relation to Climate Change -- 6.3 Nutrients -- 6.3.1 History of Nutrient Studies -- 6.3.2 Spatial and Temporal Distribution of Nutrients -- 6.3.3 Factors Controlling Nutrient Concentrations in the Surface Layer -- 6.3.4 Major Research Topics Involving Nutrients -- 6.4 Summary and Future Challenges -- References -- 7 Natural and Anthropogenic Carbon Cycling -- Abstract -- 7.1 Inorganic Carbon Cycling -- 7.1.1 Introduction -- 7.1.2 Ocean Carbonate Chemistry -- 7.1.3 Methods for Estimation of the Oceanic Anthropogenic CO2 Content -- 7.1.4 Distribution of CO2 Variables (TA, DIC, and pH) -- 7.1.5 Dynamics of Anthropogenic CO -- 7.1.6 Acidification of Seawater and Saturation State of Aragonite and Calcite -- 7.2 Organic Carbon Cycling -- 7.2.1 Introduction -- 7.2.2 Primary Production -- 7.2.3 Particulate Organic Carbon Flux -- 7.2.4 Particulate Organic Carbon Budget in the Water Column -- 7.2.5 Dissolved Organic Carbon Cycling -- 7.3 Summary and Remaining Issues -- References -- 8 Uranium Series Radionuclides -- Abstract -- 8.1 Introduction -- 8.2 Thorium Isotopes -- 8.3 Radium Isotopes -- 8.4 Lead and Polonium Isotopes -- References -- 9 Distribution of Chemical Elements in Sediments -- Abstract -- 9.1 Introduction -- 9.2 Organic and Inorganic Carbon and Silica -- 9.2.1 Distribution of Organic Carbon -- 9.2.2 Distributions of Calcium Carbonate and Silica -- 9.3 Metals -- 9.3.1 Aluminum -- 9.3.2 Iron -- 9.3.3 Manganese and Other Trace Elements -- 9.3.4 Redox Cycling of Manganese and Iron -- 9.3.5 Sources and Geochemical Features of Sediments -- 9.4 Summary -- References -- 10 Phytoplankton and Primary Production -- Abstract -- 10.1 Introduction -- 10.2 Chlorophyll a. , 10.2.1 Spatial and Seasonal Variability Based on SeaWiFS Observations -- 10.2.2 Shipboard Measurements -- 10.2.3 Measurements of Algal Pigments -- 10.3 Distribution of Micro- and Nano-Phytoplankton Abundance and Harmful Algal Blooms -- 10.3.1 Korean Coastal Waters -- 10.3.2 Russian Coastal Waters -- 10.3.3 Japanese Coastal Waters -- 10.3.4 Offshore Waters -- 10.3.5 Harmful Algal Blooms -- 10.4 Distribution of Picophytoplankton -- 10.4.1 Picophytoplankton Abundance -- 10.4.2 Picocyanobacterial Diversity -- 10.5 Species Composition -- 10.6 The Relationship Between Phytoplankton and Environmental Factors -- 10.7 Overview of Primary Production Studies -- References -- 11 Microbial Ecology and Biogeochemical Processes in the Ulleung Basin -- Abstract -- 11.1 Introduction -- 11.2 Microbiological Oceanography -- 11.2.1 Microbiological Parameters Associated with Coastal Upwelling and UWE -- 11.2.2 Role of Bacteria in Biogeochemical Carbon Cycles -- 11.3 Benthic Biogeochemical Processes -- 11.3.1 High Benthic Carbon Oxidation Rates in the Ulleung Basin -- 11.3.2 Major Carbon Oxidation Pathways -- 11.4 Composition of Prokaryotes -- 11.4.1 Composition of Culture-Dependent Prokaryotes -- 11.4.2 Composition of Culture-Independent Prokaryotes -- References -- 12 Zooplankton -- Abstract -- 12.1 Introduction -- 12.2 Species Composition of Mesozooplankton -- 12.2.1 Cnidaria and Mollusca -- 12.2.2 Arthropoda -- 12.2.2.1 Branchiopoda and Ostracoda -- 12.2.2.2 Copepoda -- 12.2.2.3 Malacostraca -- 12.2.3 Chaetognatha -- 12.2.4 Chordata-Tunicata -- 12.3 Abundance Distribution -- 12.3.1 Spatio-Temporal Distributions of Zooplankton Abundance -- 12.3.2 Abundance Distributions of Major Zooplankton Taxa -- 12.3.3 Distribution of Major Zooplankton Taxa in Local Areas -- 12.4 Patterns of Interest and Trophic Role of Microzooplankton -- 12.4.1 Subpolar Front. , 12.4.2 Upwelling Area -- 12.4.3 Korea Strait -- 12.4.4 Diel Vertical Migration -- 12.4.5 Trophic Role of Microzooplankton -- References -- 13 Fish and Fisheries -- Abstract -- 13.1 Introduction -- 13.2 Fish Species and Habitat -- 13.2.1 Species -- 13.2.2 Distribution and Habitat -- 13.3 Fisheries -- 13.3.1 Korean Commercial Fisheries -- 13.3.1.1 Yields -- 13.3.1.2 Types of Fisheries -- 13.3.1.3 Species Composition -- 13.3.1.4 Mean Trophic Level -- 13.3.1.5 Important Fisheries -- 13.3.2 Japanese Commercial Fisheries -- 13.3.3 Climate Change and Its Impacts on Fish and Fisheries -- 13.3.3.1 Capture Fishery in Korean Waters -- 13.3.3.2 Capture Fishery in Japanese Waters -- 13.3.3.3 Aquaculture -- 13.3.3.4 Invasive Species -- 13.3.4 Ecosystem-Based Fisheries Assessment and Management Issues -- 13.4 Suggestions -- References -- 14 Benthic Animals -- Abstract -- 14.1 Introduction -- 14.2 Local Scale Macrofauna Distributions -- 14.2.1 Southwestern Coasts -- 14.2.2 Northwestern Coasts -- 14.2.3 Dokdo (Dok Island) -- 14.3 Large Scale Macrobenthic Fauna Communities -- 14.3.1 Southwestern Shelf Area -- 14.3.2 Southwestern Shelf and Slope Area -- 14.3.3 Western Slope Area -- 14.3.4 North Bathyal and Abyssal Area -- 14.4 Ocean Dumping Areas -- 14.5 Summary and Further Study -- References -- 15 Marine Mammals -- Abstract -- 15.1 Introduction -- 15.2 The Historic Records of Whales in Korean Waters -- 15.3 Marine Mammals -- 15.3.1 Cetacean -- 15.3.1.1 Baleen Whales -- Northern Right Whale (Eubalaena japonica) -- Blue Whale (Balaenoptera musculus) -- Fin Whale (Balaenoptera physalus) -- Minke Whale (Balaenoptera acutorostrata) -- Humpback Whale (Megaptera novaeangliae) -- Gray Whale (Eschrichtius robustus) -- 15.3.1.2 Toothed Whales -- Sperm Whale (Physeter macrocephalus) -- Baird's Beaked Whale (Berardius bairdii) -- Stejneger's Beaked Whale (Mesoplodon stejnegeri). , Killer Whale (Orcinus orca).
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  • 2
    Keywords: Earth sciences ; Earth Sciences ; Climate change ; Sedimentology ; Oceanography ; Marine sciences ; Freshwater ; Earth sciences ; Climate change ; Sedimentology ; Oceanography ; Marine sciences ; Freshwater
    Description / Table of Contents: From the Contents: Introduction -- History -- Geography -- Physical Oceanography -- Introduction -- Circulation -- Water masses -- Inflow-outflow system -- Air-Sea Interaction -- High frequency variation -- Remote Sensing -- Chemical Oceanography -- Introduction -- Nutrients and dissolved oxygen -- Carbon cycle.
    Type of Medium: Online Resource
    Pages: Online-Ressource (XVI, 460 p. 150 illus., 68 illus. in color, online resource)
    Edition: 1st ed. 2016
    ISBN: 9783319227207
    Series Statement: SpringerLink
    Language: English
    Note: From the Contents: IntroductionHistory -- Geography -- Physical Oceanography -- Introduction -- Circulation -- Water masses -- Inflow-outflow system -- Air-Sea Interaction -- High frequency variation -- Remote Sensing -- Chemical Oceanography -- Introduction -- Nutrients and dissolved oxygen -- Carbon cycle.
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  • 3
    Publication Date: 2023-05-12
    Keywords: Conductivity, average; Depth, bottom/max; ELEVATION; Heat flow; LATITUDE; LONGITUDE; Method comment; Number; Sample, optional label/labor no; Temperature gradient
    Type: Dataset
    Format: text/tab-separated-values, 35 data points
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 227 (1970), S. 1041-1043 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Critical Rayleigh number and Reynolds number considerations indicate that heat and momentum are transferred by molecular processes in a layer of thickness h = 1 to 4 cm just above the (smooth) sea floor5. Above this conductive layer there is convection. Townsend6 describes three regimes which he ...
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Journal of oceanography 51 (1995), S. 553-569 
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Using climatological atlas data and historical hydrographic data, the relationship between dynamic height anomaly ΔD and acoustic round-trip travel time τ in the Pacific Ocean is investigated. A tight, linear relation is found in a region centered on the Kuroshio and Kuroshio Extension. In this region, the slopem of the relation is approximately −50 dyn m s−1, about equal to the value expected for first-baroclinicmode response and twice as large as the value form in the Gulf Stream region of the Atlantic Ocean. The value ofm in the Pacific generally increases in magnitude towards the south and with increasing depth to which the integrals for ΔD and τ are carried. It is changed only slightly by correcting for the temperature and salinity march of the seasons in the surface layer. The Kuroshio region is established as one in which the record of τ from an inverted echo sounder can be interpreted reliably in terms of ΔD. An inverted echo sounder can also be used in this way in a number of other regions of the Pacific, although the available hydrographic data sets are too sparse to establish their boundaries clearly.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Journal of oceanography 52 (1996), S. 771-784 
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The Kuroshio flows north along the east coasts of the Philippines and Taiwan. Between these two land masses lies the Luzon Strait which connects the Pacific Ocean to the South China Sea. The Kuroshio usually flows north past this strait, but at times part or all of it flows west through the strait into the South China Sea forming a loop current. It has been suggested that the loop current forms when the northeast monsoon deflects the Kuroshio through the Luzon Strait. In this study, satellite-derived sea-surface temperature images are used to observe the Kuroshio in the Luzon Strait region. Together with wind data from the region, these observations indicate a loop-current development process which is largely determined by an integrated supercritical wind stress parameter. The loop current grows when a four-day average of the local wind-stress component directed to the south exceeds 0.08 Nm−2. When this average wind-stress component drops below the critical value, the Kuroshio returns to its northward path.
    Type of Medium: Electronic Resource
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  • 7
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2009. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 36 (2009): L16602, doi:10.1029/2009GL039216.
    Description: Pacific Decadal Oscillation (PDO) index is strongly correlated with vertically integrated transport carried by the Kuroshio through the East China Sea (ECS). Transport was determined from satellite altimetry calibrated with in situ data and its correlation with PDO index (0.76) is highest at zero lag. Total PDO-correlated transport variation carried by the ECS-Kuroshio and Ryukyu Current is about 4 Sv. In addition, PDO index is strongly negatively correlated, at zero lag, with NCEP wind-stress-curl over the central North Pacific at ECS latitudes. Sverdrup transport, calculated from wind-stress-curl anomalies, is consistent with the observed transport variations. Finally, PDO index and ECS-Kuroshio transport are each negatively correlated with Kuroshio Position Index in the Tokara Strait; this can be explained by a model in which Kuroshio path is steered by topography when transport is low and is inertially controlled when transport is high.
    Description: MA, MW and JP were supported by ONR grant N000140210271. XZ was supported by the National Natural Science Foundation of China under grant 40776021 and the National Basic Research Programs of China under grant 2006CB400603. KK and KC were supported by the Korea EAST-I Program.
    Keywords: Kuroshio ; PDO ; Transport
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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