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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
    Type of Medium: Book
    Pages: III S,, S. 195 - 315 , graph. Darst
    Series Statement: Journal of marine systems 78.2009,2
    Language: English
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  • 4
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2010. 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 37 (2010): L01606, doi:10.1029/2009GL041601.
    Description: Moored current observations in the southwestern East/Japan Sea of 16.5 months duration clearly captured two episodes of downward phase propagation (upward energy propagation) of near-inertial waves (NIWs). Time series of temperature and velocity from the mooring and ancillary information indicate that the mooring was located near the center of an anticyclonic eddy during these events. Considering the typical vertical structure of quasi-permanent eddy features in the region, the observed downward phase propagation appeared to occur within the seasonal thermocline and upper thermostad of the anticyclonic mesoscale eddy. Ray tracing simulation of NIW using the observed subinertial currents suggests that the upward energy propagation is caused by the reflection of the NIWs within the thermostad of the anticyclonic eddy, where the effect of the vertical shear of subinertial horizontal currents is larger than the buoyancy effect in controlling the propagation of NIWs.
    Description: This work was supported by grants from the Ministry of Land, Transport, and Maritime Affairs (Ocean Climate Variability Program), and the US NSF, grant OCE-0647949 to RWS.
    Keywords: Near-inertial waves ; Mesoscale eddy ; Wave reflection
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 5
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2012. 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 117 (2012): C02017, doi:10.1029/2011JC007369.
    Description: The upper ocean heat content variability in the East/Japan Sea was investigated using a 40 year temperature and salinity data set from 1968 to 2007. Decadal variability was identified as the dominant mode of variability in the upper ocean (0–300 m) aside from the seasonal cycle. The decadal variability is strong to the west of northern Honshu, west of the Tsugaru Strait, and west of southern Hokkaido. Temperature anomalies at 50–125 m exhibit a large contribution to the decadal variability, particularly in the eastern part of the East/Japan Sea. The vertical structure of regressed temperature anomalies and the spatial patterns of regressed 10°C isotherms in the East/Japan Sea suggest that the decadal variability is related to upper ocean circulation in the East/Japan Sea. The decadal variability also exhibits an increasing trend, which indicates that the regions showing large decadal variations experienced warming on decadal time scales. Further analysis shows that the decadal variability in the East/Japan Sea is not locally isolated but is related to variability in the northwestern Pacific.
    Description: This work was supported by grants from the Ministry of Land, Transport, and Maritime Affairs, Korea (Ocean Climate Variability Program and EAST-I Project).
    Description: 2012-08-09
    Keywords: East/Japan Sea ; Decadal variability ; Heat content ; Northwestern Pacific
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 6
    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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  • 7
    Publication Date: 2022-05-25
    Description: Author Posting. © Elsevier B.V., 2009. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Journal of Marine Systems 78 (2009): 249-264, doi:10.1016/j.jmarsys.2009.02.017.
    Description: Reanalyzed products from a MOM3-based East Sea Regional Ocean Model with a 3- dimentional variational data assimilation module (DA-ESROM), have been compared with the observed hydrographic and current datasets in the Ulleung Basin (UB) of the East/Japan Sea (EJS). Satellite-borne sea surface temperature and sea surface height data, and in-situ temperature profiles have been assimilated into the DA-ESROM. The performance of the DA-ESROM appears to be efficient enough to be used in an operational ocean forecast system. Comparing with the results from Mitchell et al. (2005a), the DA-ESROM fairly well simulates the high variability of the Ulleung Warm Eddy and Dok Cold Eddy as well as the branching of the Tsushima Warm Current in the UB. The overall root-mean-square error between 100m temperature field reproduced by the DA-ESROM and the observed 100-dbar temperature field is 2.1°C, and the spatially averaged grid-to-grid correlation between the two temperature fields is high with a mean value of 0.79 for the intercomparison period. The DA-ESROM reproduces the development of strong southward North Korean Cold Current (NKCC) in summer consistent with the observational results, which is thought to be an improvement of the previous numerical models in the EJS. The reanalyzed products show that the NKCC is about 35 km wide, and flows southward along the Korean coast from spring to summer with maximum monthly mean volume transport of about 0.8 Sv in August-September.
    Description: The major part of this works was conducted with financial support by Agency for Defense Development under the contract UD031003AD. The first and seventh authors were supported at the final stage of this work by KORDI’s research projects (PE9830Q and PG47100). The second author was supported by EAST-I Program of the Ministry of Maritime Affairs and Fisheries.
    Keywords: Modeling ; Oceanic currents ; Oceanic eddies ; 3-dimensional variational technique ; East Sea Regional Ocean Model ; North Korean Cold Current ; East/Japan Sea ; Ulleung Basin
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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  • 8
    Publication Date: 2022-05-25
    Description: Author Posting. © American Meteorological Society, 2014. 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 27 (2014): 8185–8204, doi:10.1175/JCLI-D-13-00500.1.
    Description: The East Asian winter monsoon (EAWM) and the North Pacific Oscillation (NPO) constitute two outstanding surface atmospheric circulation patterns affecting the winter sea surface temperature (SST) variability in the western North Pacific. The present analyses show the relationship between the EAWM and NPO and their impact on the SST are nonstationary and regime-dependent with a sudden change around 1988. These surface circulation patterns are tightly linked to the upper-level Ural and Kamchatka blockings, respectively. During the 1973–87 strong winter monsoon epoch, the EAWM and NPO were significantly correlated to each other, but their correlation practically vanishes during the 1988–2002 weak winter monsoon epoch. This nonstationary relationship is related to the pronounced decadal weakening of the Siberian high system over the Eurasian continent after the 1988 regime shift as well as the concomitant positive NPO-like dipole change and its eastward migration in tropospheric circulation over the North Pacific. There is a tight tropical–extratropical teleconnection in the western North Pacific in the strong monsoon epoch, which disappears in the weak monsoon epoch when there is a significant eastward shift of tropical influence and enhanced storm tracks into the eastern North Pacific. A tentative mechanism of the nonstationary relationship between the EAWM and NPO is proposed, stressing the pivotal role played in the above teleconnection by a decadal shift of the East Asian trough resulting from the abrupt decline of the EAWM since the late 1980s.
    Description: G. Pak has been supported from the Brain Korea 21 Project of SNU, for which we are very grateful to K.-R. Kim, and also from the Ministry of Oceans and Fisheries, South Korea (OCCAPA and EAST-I projects). Y.-O. Kwon is supported by the U.S. National Science Foundation Climate and Large-Scale Dynamics program (AGS-1035423) and Department of Energy (DOE) Climate and Environmental Science Division (DESC0007052).
    Description: 2015-05-01
    Keywords: Climate variability ; Interannual variability ; Interdecadal variability ; North Pacific Oscillation
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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