GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Online Resource
    Online Resource
    Singapore :Springer Singapore Pte. Limited,
    Keywords: Oceanography-Pacific Ocean. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (320 pages)
    Edition: 1st ed.
    ISBN: 9789811548864
    Series Statement: Atmosphere, Earth, Ocean and Space Series
    Language: English
    Note: Intro -- Contents -- 1 Introduction -- 2 Changes in Temperature, Chlorophyll Concentration, and Secchi Disk Depth in the Bering Sea from 1998 to 2016 -- 2.1 Introduction -- 2.2 Sea Surface Temperature -- 2.3 Chlorophyll Concentration -- 2.4 Secchi Disk Depth -- 2.5 Conclusions -- References -- 3 Long-Term Trend and Interannual to Decadal Variability in the Sea of Okhotsk -- 3.1 Background -- 3.2 Sea Ice and SST -- 3.3 Long-Term Trends and Variations in Dense Shelf Water and Intermediate-Layer Water -- 3.3.1 Sea Ice Production -- 3.3.2 Sea Surface Salinity -- 3.3.3 Numerical Modeling Results -- 3.4 Coherent Sea Level Variations in the Coastal Area -- 3.5 18.6-yr Lunar Nodal Tide and Its Influence on Water Mass Property Changes -- 3.6 Summary -- References -- 4 Changes in Temperature, Chlorophyll Concentration, and Secchi Disk Depth in the Okhotsk Sea from 1998 to 2016 -- 4.1 Introduction -- 4.2 Known Temporal Changes -- 4.3 Sea Surface Temperature -- 4.4 Chlorophyll Concentration -- 4.5 Secchi Disk Depth -- 4.6 Conclusions -- References -- 5 Long-Term Changes in the Abyssal Japan Sea (East Sea): A Physical View -- 5.1 Introduction -- 5.2 The Japan Sea Proper Water -- 5.3 Long-Term Trends in the JSPW -- 5.4 Decadal-Scale Variations in the JSPW -- 5.5 Changes in the Deep Flow Field -- 5.6 Concluding Remarks -- References -- 6 Anthropogenic Perturbations of the Carbon and Nitrogen Cycles in the East Sea (Sea of Japan) -- 6.1 Introduction -- 6.2 Physical Properties of the Interior of the East Sea -- 6.3 Anthropogenic CO2 in the East Sea -- 6.4 Anthropogenic Nitrogen -- 6.5 Conclusions -- References -- 7 The Changing Bohai and Yellow Seas: A Physical View -- 7.1 Introduction -- 7.2 Changes of Water Temperature -- 7.3 The Yellow Sea Cold Water Mass and Tidal Fronts -- 7.4 Changes of the Sea Levels: Rising Rate, Tides and Extremes -- 7.5 Summary. , References -- 8 Changing Nutrients, Dissolved Oxygen and Carbonate System in the Bohai and Yellow Seas, China -- 8.1 Changing Nutrients in the Bohai and Yellow Seas -- 8.2 Changing Dissolved Oxygen in the Bohai and Yellow Seas -- 8.3 Carbonate System in the Bohai and Yellow Seas and the Locally-Intensified Ocean Acidification in Subsurface Waters -- 8.4 Summary and Potential Ecological Effects -- References -- 9 The Changing East China Sea-A Physical View -- 9.1 Introduction -- 9.2 Sea Surface Temperature -- 9.3 Yellow Sea Cold Water -- 9.4 The Kuroshio -- 9.5 Changjiang Diluted Water -- 9.6 Sea Level -- 9.7 Discussion -- References -- 10 Changing Nutrients, Oxygen and Phytoplankton in the East China Sea -- 10.1 Introduction -- 10.2 Nutrients -- 10.2.1 East China Sea -- 10.2.2 Hangzhou Bay -- 10.2.3 N/P and N/Si Ratios -- 10.2.4 Changing Nutrient Inputs -- 10.3 Phytoplankton Communities -- 10.3.1 Phytoplankton Abundance -- 10.3.2 Phytoplankton Community Composition -- 10.3.3 Dominant Phytoplankton Species -- 10.4 Dissolved Oxygen and Hypoxia -- 10.4.1 Dissolved Oxygen -- 10.4.2 Seasonal Hypoxia -- 10.5 Conclusions -- References -- 11 The Changing Circulation of Asia-Pacific Marginal Seas in the South China Sea: A Physical View -- 11.1 Introduction -- 11.2 Characteristics of Internal and External Forces in the SCS -- 11.2.1 The Monsoonal Wind -- 11.2.2 External Transport Through Straits -- 11.3 Circulation and Physical Characteristics in the SCS -- 11.3.1 SCS Layered Circulation -- 11.3.2 Characteristics of Thermohalines -- 11.3.3 Circulation Pathways and Residence Time -- 11.4 The Changing SCS Circulation -- 11.4.1 Changes in Horizontal Plane -- 11.4.2 SCS Layered Circulation Trends -- 11.5 Dynamics for the Changing SCS Circulation -- 11.5.1 Vorticity Dynamics -- 11.5.2 Dynamic Driver for the CAC Circulation. , 11.5.3 Mechanism for the Changing Layered Circulation -- 11.6 Summary -- References -- 12 Changing Biogeochemistry in the South China Sea -- 12.1 Introduction -- 12.2 Changing Sea Surface Temperature -- 12.3 Changing Chlorophyll Concentration -- 12.4 Changing Secchi Disk Depth -- 12.5 Conclusions -- References -- 13 Interdecadal Variations of the Oyashio and Extreme Cold Water Events Near the Japanese Coast from the 1960s to the 2010s -- 13.1 Introduction -- 13.2 Seasonality and Dynamics of the Oyashio -- 13.3 Basin-Scale Wind Stress and the Southernmost Latitude of the FOI -- 13.4 Long-Term Variations of the Oyashio -- 13.4.1 Mid-1960s to Mid-1980s -- 13.4.2 Mid-1990s to Mid-2010s -- 13.5 Impacts of the Oyashio on Coastal Waters -- 13.6 Future Perspectives -- References -- 14 Multidecadal Variations of Sea Surface CO2 Fugacity (fCO2) in the Oyashio Current-Influenced Ocean Margin -- 14.1 Introduction -- 14.2 Prior Results on Changes in fCO2 in the Japanese Margin -- 14.3 Analysis of the fCO2 Trends Using the SOCAT Version 5 Data -- 14.4 Time Scales for the Trend Calculations -- 14.5 Spatial Distribution of fCO2, SST, and SSS -- 14.6 Seawater fCO2 Trends -- 14.7 Temporal and Spatial Changes in SST and SSS and Their Effect on fCO2 -- 14.8 Effect of Changing Boundary Current Conditions on fCO2 Trend -- 14.9 CO2 Sink/Source Evolution -- 14.10 Conclusions -- References -- 15 Changing Kuroshio and Its Affected Shelf Sea: A Physical View -- 15.1 Introduction -- 15.2 Description of Regional Features of the Kuroshio -- 15.2.1 East of the Philippines -- 15.2.2 Luzon Strait -- 15.2.3 East of Taiwan -- 15.2.4 Subtropical Countercurrent Zone -- 15.2.5 Northeast of Taiwan -- 15.2.6 East China Sea -- 15.2.7 Around Kyushu Island -- 15.3 Comprehensive View of Mechanisms Driving Regional Kuroshio Variations -- 15.3.1 Integrated Features Connecting Each Region. , 15.3.2 The Mechanisms -- 15.4 Summary -- References -- 16 Transient Carbonate Chemistry in the Expanded Kuroshio Region -- 16.1 Introduction -- 16.2 Increasing Nutrients but Decreasing DO and pH of the KIW -- 16.3 Upper Layer Intrusion Reduces Productivity -- 16.4 Changing Carbonate Chemistry -- 16.5 Conclusions -- References.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Book
    Book
    [Arlington, VA] : Office of Naval Research
    Type of Medium: Book
    Pages: xi, 948 p , ill., 1 map , 28 cm
    DDC: 551.46
    Language: English
    Note: Final. 10-1-82 to 9-30-84 , Cover title , Oregon State University, School of Oceanography"--Rept. doc. p , Includes bibliographical references and indexes , N00014-79-C-0004, 61153N, RR03103, RR0310301, 083-102-39 , Item 407
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Online Resource
    Online Resource
    Singapore : Springer Singapore | Singapore : Imprint: Springer
    Keywords: Oceanography. ; Physical geography.
    Description / Table of Contents: Sea of Okhotsk -- Japan Sea -- East China Sea -- Yellow and Bohai Seas -- South China Sea -- Kuroshio and its affected Shelf Sea -- Oyashio and its affected Shelf Sea.
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(VI, 320 p. 128 illus., 109 illus. in color.)
    Edition: 1st ed. 2020.
    ISBN: 9789811548864
    Series Statement: Atmosphere, Earth, Ocean & Space
    Language: English
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2023-01-30
    Description: The Fukushima accident released short-lived Cs-134 and longer-lived Cs-137 to the ocean. The amount, although substantial, is much less than that produced during the atomic bomb tests 60 yrs ago. Cs-134 and Cs-137 are anthropogenic radionuclides and soluble in seawater, hence, the radioactivity can be used as a tracer for special event or currents. Here we collected Cs-134 and Cs-137 samples in seawaters surrounding Taiwan including the Kuroshio, the northern South China Sea, the Taiwan Strait, and the southern East China Sea from 2018 to 2021. Most surface seawater samples were collected from boats using 20-L tanks, and a few samples were gathered from the shore. Non-surface seawater samples were taken from R/Vs Ocean Researcher I, II, and III with Niskin bottles mounted on a CTD rosette. All samples were determined in the Radian Monitor Center, Atomic Energy Council of Taiwan. Ammonium molybdophosphate (AMP) was used to pre-concentrated Radiocesium. Each 40-L (60-L) sample was counted for 200,000 s (120,000 s) using a high-purity germanium (HPGe) detector with lead shielding. The detection limits of 137Cs was 0.5 Bq m−3. The averaged surface Cs-137 activities was 1.18±0.25 Bq m-3, however, the activities of Cs-134 samples were all under detection limit. Complete data are archived, including sampling date, location, water depth, temperature, salinity, and Cs-137 activity; total sample amount is 577.
    Keywords: Caesium-137; Cs-137; DATE/TIME; DEPTH, water; East China Sea; Fukushima accident; High-purity Germanium (HPGe) detector; Kuroshio; LATITUDE; LONGITUDE; MULT; Multiple investigations; Salinity; South China Sea; Taiwan_Seawater; Taiwan Strait; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 1731 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2024-04-20
    Description: These data were compiled from original and published datasets of coastal groundwater / subterranean estuary research efforts along global coastline (sites within 1km of shoreline). The dataset includes sampling site names, locations, original sample information, sample depth, temperature, salinity, dissolved nitrogen concentrations, and dissolved phosphorus concentrations. The data source or curator is also included in the dataset.
    Keywords: biogeochemistry; groundwater; nutrients; subterranean estuary
    Type: Dataset
    Format: application/vnd.ms-excel.sheet.macroenabled.12, 1.4 MBytes
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Journal of oceanography 46 (1990), S. 201-210 
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Recent carbonate data collected in the North Pacific were combined with the data in the literature in order to understand more clearly the carbonate chemistry in the North Pacific. Our analyses show that inorganic CaCO3 dissolution contributes about 26% of the total inorganic CO2 increase of deep water, after leaving the Southern Ocean. The calcium and alkalinity data indicate a CaCO3 dissolution rate of 0.060±0.010 and 0.053±0.005 µ mol kg−1 yr−1 respectively, for waters deeper than 2,000 m in reference to the Weddell Sea Deep Water. The organic carbon decomposition rate is 0.107±0.012 µ mol kg−1 yr−1 while the oxygen consumption rate is 0.13±0.002 µ mol kg−1 yr−1. These results which are based on the direct comparison of two water masses agree well with other estimates which are based on methods such as the one-dimensional-diffusion-advection model. Comparison of data along the two sections at 165°E and 150°W shows no significant difference in the ratio of the CaCO3 dissolution rate and the organic carbon decomposition rate. The eastern section, however, has a higher TCO2 input than the western section because of the older age of the deep water along the eastern section.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Journal of oceanography 52 (1996), S. 17-25 
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract In order to understand the influence of the South China Sea (SCS) water on the Kuroshio, and to study the dissolved carbonate system, we participated in six WOCE cruises aboard R/V Ocean Researcher 1. The areas studied were the northeast South China Sea and the West Philippine Sea near the Luzon Strait. Temperature, salinity, pH, alkalinity and total CO2 were measured. Our data indicate that, although the Kuroshio and the SCS waters flow in and out of the Luzon Strait near surface, the SCS water seems mainly to flow out of the SCS at mid-depth. There exists a “mid-depth front” near 122°E between 350 and 1350 m in all seasons and years that we studied. The water mass between 350 and 1350 m east of the front belongs to the West Philippine Sea proper water, while on the west is the mixed water of the South China Sea and the West Philippine Sea.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2023-02-08
    Description: Highlights • The vent fluids discharged from the Lutao hydrothermal field experienced low-degree subcritical phase separation. • The temperature and chemical compositions of the vent fluids were modulated by tides. • The time delay between tides and the response of hydrothermal system was about 3 h. • The typhoon “Fung-wong” cooled the reaction zone and decreased the degree of phase separation. • The hydrothermal system began to recover after the typhoon passed by. Abstract The Lutao hydrothermal field is an intertidal arc-volcanic system located offshore southeast Taiwan, hosting a Zhudanqu (ZDQ) vent and a Huwaichi (HWC) spring with strongly contrasting fluid chemistry. Low Mg, moderately enriched Cl, and H+ with respect to seawater indicate that the ZDQ endmember was derived from the brine phase that was formed during low-degree subcritical phase separation. In contrast, the endmember for the HWC vent fluids is related to the vapor phase. Temperature and pressure of the phase separation were estimated as ~150 °C and ~7 bar, respectively. The water/rock ratio was roughly calculated as about 2. The Lutao hydrothermal system was slightly affected by semi-diurnal tides, by some combination of tidal loading and tidal currents. The time delay between tides and the response of the hydrothermal system was about 3 h. While freshwater was almost absent in the HWC vent fluids at normal conditions, the typhoon “Fung-wong” on Sep 21st, 2014, led to intrusions of freshwater into the vent fluids with a percentage of ~16%. Both the ZDQ and the HWC endmember compositions showed some changes after the typhoon event, suggesting a cooling of the reaction zone. After the typhoon passed by, the hydrothermal system began to recover, evidenced by increasing percentages of the HWC endmember and decreasing freshwater contributions. The flux of the HWC endmember was estimated as 460–560 L h−1 based on these observations. This study, for the first time, reports a shallow-depth tidal-influenced hydrothermal system that was temporarily cooled by a tropical storm.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2024-02-07
    Description: Highlights • Aerobic oxidation of alkanes was observed in hydrothermal fluids during storage. • The residual CH4 shows the highest ever reported δ13C of up to +243‰. • The εC for C1, C2, and C3 oxidation were −37.1‰, −14.8‰ and −4.7‰, respectively. • The εH for methane was −281 ± 187‰, while the Λ value was 8.4 ± 4.6. • Aerobic oxidation could produce carbon isotope reversal of the residual alkanes. Aerobic oxidation of short-chain alkanes was observed in gas samples from the Lutao intertidal hydrothermal vents in Taiwan, during storage at 20 °C for up to 29 months without adding bacterial strains and replenishing substrates. The carbon isotope fractionation factors (εC) of methane (C1), ethane (C2), and propane (C3), were calculated using the Rayleigh fractionation equation to be −37.1 ± 7.5‰, −14.8 ± 4.8‰, and −4.7 ± 5.2‰, respectively. The hydrogen isotope fractionation factor (εH) of methane was determined to be −281 ± 187‰. DNA sequencing of the 16S rRNA gene in the vent fluids suggests that aerobic oxidation is dominated by methanotrophs of the genera Methylomicrobium and Methylophaga, which use the ribulose monophosphate pathway (RuMP). The degrees of isotope fractionation (εC and εH values) herein are larger than previously reported values, possibly due to the limited O2 supply and low abundance of aerobic methane-oxidizing bacteria in the experiments. Since the fractionation factor of methane is higher than those of ethane and propane, the aerobic oxidation of thermogenic or microbial alkanes could produce a carbon isotope reversal, which is frequently noted as a trait of abiotic hydrocarbons. This work demonstrates that in addition to anaerobic microbial oxidation, aerobic oxidation with a low cell density can also produce significant isotope fractionation of alkanes in geological closed/semi-closed environments and open flow reaction systems that are characterized by moderate temperatures and a limited supply of substrates and O2; these environments include cold seeps, mud volcanoes, and low-temperature hydrothermal plumes/aquifers/reservoirs.
    Type: Article , PeerReviewed
    Format: text
    Format: archive
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2024-02-07
    Description: The chemical and isotopic characteristics of calcium (Ca) in subduction zones are closely related to the budget of Ca and carbon cycles. Here we investigate the ultra-high Ca concentrations that characterize the hydrothermal fluids discharged from two types of vents, named the Zhudanqu brine vent (ZDQ) and the Huwaichi vapor spring (HWC), in the Lutao hydrothermal system at the north Luzon arc. The Ca concentrations of up to 159 mM and Ca/Cl ratio of up to 0.26 in the ZDQ vent fluids are possibly the highest ever reported for Ca enrichment in global seawater-circulated hydrothermal/geothermal systems. The differences in chemical compositions between the ZDQ and the HWC vent fluids are primary controlled by subcritical phase separation. The brine phase constitutes the ZDQ vent fluids, while the HWC vent fluids represent mixtures of the vapor phase and seawater. Both the vapor and the brine phases exhibit similar δ44/40Ca values (0.72 ± 0.05‰), suggesting no significant Ca isotope fractionation has occurred during phase separation. The hydrothermal endmember before phase separation (the “Lutao endmember”) presents depletions of 213 ± 15 mM of Na, 24.4 ± 0.4 mM of SO42−, and 10.2 mM of K, and enrichment of 130.2 ± 5.5 mM of Ca with respect to the percolated seawater. The total gained Ca is 154.6 ± 5.9 mM with a δ44/40Ca value of 0.67‰ – 0.77‰ (0.72 ± 0.05‰), considering anhydrite precipitation during hydrothermal circulation. The Holocene raised coral reef is unlikely to contribute substantial Ca into the Lutao system. Much of the gained Ca (111.6 ± 7.5 mM) is produced by high-degree albitization of the Lutao host rock, which is promoted by the low water/rock ratio (~ 2), slightly alkaline conditions, and relatively lower temperature of the Lutao system with respect to most mid-ocean ridge hydrothermal systems. Ca derived from this process inherits the Ca isotopes of plagioclase in the Lutao host rocks (δ44/40Ca = 0.82 ± 0.06‰). According to mass and isotopic balances, the recycled marine carbonate is proposed to contribute 43 ± 13.4 mM Ca with a δ44/40Ca value of 0.46−0.63+0.35‰ into the Lutao system. Such isotopically lighter Ca is derived from either pore fluids expulsed from underlying Philippine Sea sediments, or more probably, carbonate-bearing subduction fluids from the subducting South China Sea sediments and slab. The carbonate solubility in the subduction fluids could maintain at 600 mM near the reaction zone. The carbonate-rich fluids were subsequently migrated into the Lutao reaction zone and released an additional 43 ± 13.4 mM Ca via dolomitization. A small amount (~ 9%) addition of carbonate-rich fluids would not significantly change the budgets of Na, Mg, and Cl but could generate substantial Ca enrichment and Ca isotopic variations.
    Type: Article , PeerReviewed
    Format: text
    Format: text
    Format: other
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...