GLORIA

GEOMAR Library Ocean Research Information Access

Language
Preferred search index
Number of Hits per Page
Default Sort Criterion
Default Sort Ordering
Size of Search History
Default Email Address
Default Export Format
Default Export Encoding
Facet list arrangement
Maximum number of values per filter
Auto Completion
Topics (search only within journals and journal articles that belong to one or more of the selected topics)
Feed Format
Maximum Number of Items per Feed
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
    Cham :Springer International Publishing AG,
    Keywords: Marine geophysics. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (290 pages)
    Edition: 1st ed.
    ISBN: 9783030406592
    Series Statement: Society of Earth Scientists Series
    DDC: 353.00823200000002
    Language: English
    Note: Intro -- Series Editor Foreword -- Foreword -- Preface -- Contents -- About the Editors -- Introduction-Scientific Drilling in the Indian Ocean: An Earth System Process Perspective -- 1 Himlayan-Tibetan Orogeny and Long Term Climate Evolution -- 1.1 Indian Monsoon Rainfall (IODP Expedition 353) -- 1.2 Bengal Fan -- 1.3 Indus Fan -- 2 The Indonesian Throughflow Expedtion -- 2.1 Indonesian Throughflow (ITF) and the Australian Monsoon -- 3 Maldives and Equatorial Indian Ocean -- 3.1 Maldives Monsoon and Sea Level -- 4 South African Climates -- 4.1 The South African Climates and Agulhas Current Density Profile -- 5 Plate Deformation Zones -- 5.1 "The Nature of the Lower Crust and Moho at Slower Spreading Ridges"-SloMo -- 5.2 To Understand the Role of Input Materials in the Northern Sumatra Subduction -- 6 Concluding Remarks -- References -- Morphological and Chemical Properties of Microtektite Grains from Bay of Bengal (IODP Expedition 354) -- 1 Introduction -- 2 Materials and Methods -- 3 Results and Discussion -- 4 Morphological Characteristics of the Microtektites -- 5 Shapes, Size and Color -- 6 Surface Sculpturing -- 7 Compositional Characteristics of Microtektites -- 8 Evidence of Extraterrestrial Materials Within the Microtektite Layer -- 9 Conclusions -- References -- Assessing Mid-pleistocene to Holocene Sea-Ice Extent and Carbonate Compensation Depth Fluctuations in the Japan Sea: A Multiproxy Approach -- 1 Introduction -- 2 Location, Lithology, and Hydrography of Japan Sea -- 2.1 Material and Methods -- 3 Results -- 3.1 Distribution of IRD and Detrital -- 3.2 Distribution of Foraminifera -- 3.3 Environmental Preferences of Dominant Planktic Species -- 4 Discussion -- 5 Conclusion -- References -- Modern Radiolarians Recovered from the Mudline Samples at IODP-341 Sites in the South Alaska Basin, North East Pacific Ocean -- 1 Introduction. , 2 Radiolarians from Mudline Samples -- 3 Results -- 3.1 Radiolarians in the Mudline, Hole U1417D -- 3.2 Radiolarians in the Mudline, Hole U1418C -- 3.3 Radiolarians in the Mudline Hole U1419A -- 3.4 Radiolarians in the Mudline, Hole U1421A -- 4 Conclusion -- References -- Carbon Stable Isotope Source Signature of Bulk Organic Matter in Middle Bengal Fan Sediment Collected During IODP Expedition 354 -- 1 Introduction -- 2 Site -- 3 Materials and Method -- 4 Results -- 4.1 TOC, N, C/N Ratio and δ13C of Sedimentary OM -- 5 Discussion -- 5.1 Preservation of OM -- 5.2 Source of OM -- 6 Conclusion -- References -- Geochemistry of Marine Carbonates from Hole 1394, off the Coast of Montserrat, IODP Expedition-340 -- Implications on Provenance, Paleoenvironment and Lesser Antilles Arc Migration -- 1 Introduction -- 2 Materials and Methods -- 3 Stratigraphy and Nature of Sediments -- 4 Results -- 4.1 Geochemistry -- 5 Discussion -- 5.1 Europium Anomalies (Eu/Eu*) -- 5.2 Cerium Anomalies (Ce/Ce*) -- 5.3 Er/Nd Ratios -- 5.4 Age of the Carbonates -- 5.5 Depth Wise Variation in Geochemical Parameters -- 5.6 Source Weathering and Alteration Characteristics -- 5.7 Contamination and Diagenetic Alterations -- 5.8 Temperate (Cool Water) Versus Tropical (Warm Water) Carbonates -- 5.9 Th/U Ratios -- 5.10 Paleo-redox Characteristics -- 5.11 Total Carbon and Carbonate Content -- 5.12 Shifting of Platformal Carbonates to Deep Ocean: Evidence from Ce and La (Pr/Pr*) Anomalies -- 5.13 Tectonic Setting -- 6 Conclusions -- References -- Morpho-taxonomy of Corycaeid Cyclopoids from Lakshadweep Sea, South Eastern Arabian Sea-A Part of the Indian Ocean -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion and Conclusion -- References. , Sedimentological Attributes and Quartz Microtexture in the Levee Sediments of a Submarine Channel in Context of the East Antarctic Ice Sheet Fluctuations: A Study from Site U-1359 of IODP-318 Expedition -- 1 Introduction -- 2 Site U1359 -- 3 Materials and Methods -- 4 Results -- 4.1 Grain Size Analysis -- 4.2 Quartz Grain Microtextures -- 5 Discussion -- 5.1 Sedimentary Processes -- 5.2 Depositional Environment -- 6 Conclusions -- References -- Late Quaternary Sedimentation and Slope Failure Events on the Costa Rican Margin -- 1 Introduction -- 2 Materials and Methods -- 2.1 Samples and Data -- 2.2 Sample Processing for XRD Analysis -- 2.3 Quantification of Clay Minerals -- 2.4 Sample Processing for XRF Analysis -- 2.5 Sample Processing for IRMS Analysis -- 2.6 Age Model -- 3 Results and Discussion -- 3.1 Clay Minerals -- 3.2 Quantification of Major Elements -- 3.3 Carbon and Nitrogen Isotopes -- 4 Summary and Conclusions -- References -- mtCOI Sequence-Based Barcoding of Calanoid Copepods from Lagoon Waters of Lakshadweep, South-west Coast of India -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 3.1 Molecular Records and Systematics of the Calanoid Copepods -- 3.2 Barcode Library Developed for the Calanoid Copepods -- 4 Discussion -- References -- A Summary of the South China Sea Evolution -- 1 Introduction -- 2 Regional Geological Setting -- 3 Evolution History -- 4 Dynamics of the South China Sea -- 4.1 The Tectonic Extrusion Model -- 4.2 Backarc Extension Model -- 4.3 Two-Stage Rifting Model -- 4.4 Proto-SCS Dragging Model -- 4.5 Models that Involve Extension Induced by Mantle Plume -- 4.6 Combined Model -- References -- Microbial Community Profile of Deep-Sea Sediment from Eastern Arabian Sea (IODP 355) -- 1 Introduction -- 2 Materials and Methods -- 2.1 Deep Sea Sediment Cores IODP -- 2.2 DNA Extraction. , 2.3 16S rRNA Gene Sequencing -- 3 Quality Control, Taxonomic Assignment, Diversity Estimation and Total Cell Counts -- 4 Result and Discussion -- 4.1 Total Cell Counts -- 4.2 Taxonomic Assignment and Microbial Diversity -- References.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Keywords: Geochemistry. ; Paleontology . ; Sedimentology. ; Aufsatzsammlung ; Integrated Ocean Drilling Program ; Indien ; Geowissenschaftler ; Meeresgeologie
    Description / Table of Contents: Scientific drilling in the Indian Ocean: An Earth system process perspective -- Morphological and chemical properties of microtektite grains from Bay of Bengal (IODP Expedition 354) -- Assessing Mid-Pleistocene to Holocene Sea-ice Extent and Carbonate Compensation Depth fluctuations in the Japan Sea: a multiproxy approach -- Modern Radiolarians Recovered from the mudline samples at IODP-341 sites in the South Alaska Basin, North East Pacific Ocean -- Carbon Stable Isotope Source Signature of Bulk Organic Matter in Middle Bengal Fan Sediment Collected During IODP Expedition 354 -- Geochemistry of Marine Carbonates from Hole 1394, off the coast of Montserrat, IODP Expedition-340; Implications on provenance, paleoenvironment and Lesser Antilles arc migration -- Morpho-taxonomy of Corycaeid cyclopoids from Lakshadweep Sea, South Eastern Arabian Sea- a part of the Indian Ocean -- Sedimentological attributes and quartz microtexture in the levee sediments of a submarine channel in context of the East Antarctic ice sheet fluctuations: A study from site U-1359 of IODP-318 expedition -- Late Quaternary sedimentation and slope failure events on the Costa Rican margin -- Mt COI sequence-based barcoding of calanoid copepods from lagoon waters of Lakshadweep, South-West coast of India -- A Summary of the South China Sea Evolution -- Microbial Community Profile and Deep-sea sediment of Eastern Arabian Sea (IODP 355).
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(XIV, 283 p. 121 illus., 80 illus. in color.)
    Edition: 1st ed. 2020.
    ISBN: 9783030406592
    Series Statement: Society of Earth Scientists Series
    Language: English
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Review of Scientific Instruments 70 (1999), S. 2140-2149 
    ISSN: 1089-7623
    Source: AIP Digital Archive
    Topics: Physics , Electrical Engineering, Measurement and Control Technology
    Notes: A spherical field meter has been developed to measure the atmospheric electric field vector above the ground surface. Its calibrations in the radial and linear electric fields and the method to find out the distortion coefficients are described. Extensive measurements of the components of the atmospheric electric field and the resulting electric field vector in fair weather and during the passage of a small dust devil over the spherical field meter are reported. Observations made at Pune (18°32′ N, 73°51′ E, 559 m above msl), show that in fair weather the horizontal component of the electric field may be upto 5% of the vertical component. Variations in the horizontal components of the electric field when averaged over an interval of more than 4 s are small and are generally but not always identical to its vertical components. However, at a frequency of few Hertz, variations in the horizontal components may be comparatively larger and generally independent of the vertical components. Observations made during the passage of a small dust devil over the spherical field meter show the development of appreciable horizontal component of electric field above the ground surface. These observations demonstrate the capability and reliability of the spherical field meter to measure the magnitude and direction of the electric field vector. They also demonstrate that the movement of small space charge pockets close to the surface may cause the development of horizontal component of the electric field. © 1999 American Institute of Physics.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Electronic Resource
    Electronic Resource
    Woodbury, NY : American Institute of Physics (AIP)
    Applied Physics Letters 57 (1990), S. 1870-1872 
    ISSN: 1077-3118
    Source: AIP Digital Archive
    Topics: Physics
    Notes: The ability of scanning electron acoustic microscopy (SEAM) to characterize ceramic materials is assessed. SEAM images of Vickers indentations in SiC whisker-reinforced alumina clearly reveal not only the radial cracks, the length of which can be used to estimate the fracture toughness of the material, but also reveal strong contrast, interpreted as arising from the combined effects of lateral cracks and the residual stress field left in the SiC whisker-reinforced alumina by the indenter. The strong contrast is removed after the material is heat treated at 1000 °C to relieve the residual stresses around the indentations. A comparison of these observations with SEAM and reflected polarized light observations of Vickers indentations in soda-lime glass both before and after heat treatment confirms our interpretation of the strong contrast.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2020-01-07
    Description: We present an analysis of annual and seasonal mean characteristics of the Indian Ocean circulation and water masses from 16 global ocean–sea-ice model simulations that follow the Coordinated Ocean-ice Reference Experiments (CORE) interannual protocol (CORE-II). All simulations show a similar large-scale tropical current system, but with differences in the Equatorial Undercurrent. Most CORE-II models simulate the structure of the Cross Equatorial Cell (CEC) in the Indian Ocean. We uncover a previously unidentified secondary pathway of northward cross-equatorial transport along 75 °E, thus complementing the pathway near the Somali Coast. This secondary pathway is most prominent in the models which represent topography realistically, thus suggesting a need for realistic bathymetry in climate models. When probing the water mass structure in the upper ocean, we find that the salinity profiles are closer to observations in geopotential (level) models than in isopycnal models. More generally, we find that biases are model dependent, thus suggesting a grouping into model lineage, formulation of the surface boundary, vertical coordinate and surface salinity restoring. Refinement in model horizontal resolution (one degree versus degree) does not significantly improve simulations, though there are some marginal improvements in the salinity and barrier layer results. The results in turn suggest that a focus on improving physical parameterizations (e.g. boundary layer processes) may offer more near-term advances in Indian Ocean simulations than refined grid resolution.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2021-09-21
    Description: We present an analysis of annual and seasonal mean characteristics of the Indian Ocean circulation and water masses from 16 global ocean-sea-ice model simulations that follow the Coordinated Ocean-ice Reference Experiments (CORE) interannual protocol (CORE-II). All simulations show a similar large-scale tropical current system, but with differences in the Equatorial Undercurrent. Most CORE-II models simulate the structure of the Cross Equatorial Cell (CEC) in the Indian Ocean. We uncover a previously unidentified secondary pathway of northward cross-equatorial transport along 75 °E, thus complementing the pathway near the Somali Coast. This secondary pathway is most prominent in the models which represent topography realistically, thus suggesting a need for realistic bathymetry in climate models. When probing the water mass structure in the upper ocean, we find that the salinity profiles are closer to observations in geopotential (level) models than in isopycnal models. More generally, we find that biases are model dependent, thus suggesting a grouping into model lineage, formulation of the surface boundary, vertical coordinate and surface salinity restoring. Refinement in model horizontal resolution (one degree versus ¼ degree) does not significantly improve simulations, though there are some marginal improvements in the salinity and barrier layer results. The results in turn suggest that a focus on improving physical parameterizations (e.g. boundary layer processes) may offer more near-term advances in Indian Ocean simulations than refined grid resolution.
    Description: Published
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2022-05-26
    Description: Author Posting. © American Meteorological Society, 2009. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Bulletin of the American Meteorological Society 90 (2009):459-480, doi:10.1175/2008BAMS2608.1.
    Description: The Indian Ocean is unique among the three tropical ocean basins in that it is blocked at 25°N by the Asian landmass. Seasonal heating and cooling of the land sets the stage for dramatic monsoon wind reversals, strong ocean–atmosphere interactions, and intense seasonal rains over the Indian subcontinent, Southeast Asia, East Africa, and Australia. Recurrence of these monsoon rains is critical to agricultural production that supports a third of the world's population. The Indian Ocean also remotely influences the evolution of El Niño–Southern Oscillation (ENSO), the North Atlantic Oscillation (NAO), North American weather, and hurricane activity. Despite its importance in the regional and global climate system though, the Indian Ocean is the most poorly observed and least well understood of the three tropical oceans. This article describes the Research Moored Array for African–Asian–Australian Monsoon Analysis and Prediction (RAMA), a new observational network designed to address outstanding scientific questions related to Indian Ocean variability and the monsoons. RAMA is a multinationally supported element of the Indian Ocean Observing System (IndOOS), a combination of complementary satellite and in situ measurement platforms for climate research and forecasting. The article discusses the scientific rationale, design criteria, and implementation of the array. Initial RAMA data are presented to illustrate how they contribute to improved documentation and understanding of phenomena in the region. Applications of the data for societal benefit are also described.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2022-05-26
    Description: Author Posting. © The Oceanography Society, 2016. This article is posted here by permission of The Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 29, no. 2 (2016): 14–17, doi:10.5670/oceanog.2016.34.
    Description: The Bay of Bengal has a surprisingly large influence on the world. It nurtures the South Asian summer monsoon, a tremendous ocean-atmosphere-land phenomenon that delivers freshwater to more than a third of the human population on this planet. During summer, southwesterly winds gather moisture from the ocean and carry it deep inland over the Indian subcontinent, bringing welcome rains to a parched land. During winter, the winds reverse to northeasterly, and the ocean circulation responds by dispersing the terrestrial freshwater runoff concentrated in the northern part of the bay. This freshwater impacts the ocean’s structure, circulation, and biogeochemistry in numerous ways and, through modification of sea surface temperature, feeds back to influence air-sea fluxes. Because the atmosphere obtains its moisture and heat for convection from the ocean, the interplay between ocean and atmosphere is crucial for the development and sustenance of the monsoon.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2022-05-26
    Description: Author Posting. © The Oceanography Society, 2016. This article is posted here by permission of The Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 29, no. 2 (2016): 50–61, doi:10.5670/oceanog.2016.38.
    Description: Upper-ocean turbulent heat fluxes in the Bay of Bengal and the Arctic Ocean drive regional monsoons and sea ice melt, respectively, important issues of societal interest. In both cases, accurate prediction of these heat transports depends on proper representation of the small-scale structure of vertical stratification, which in turn is created by a host of complex submesoscale processes. Though half a world apart and having dramatically different temperatures, there are surprising similarities between the two: both have (1) very fresh surface layers that are largely decoupled from the ocean below by a sharp halocline barrier, (2) evidence of interleaving lateral and vertical gradients that set upper-ocean stratification, and (3) vertical turbulent heat fluxes within the upper ocean that respond sensitively to these structures. However, there are clear differences in each ocean’s horizontal scales of variability, suggesting that despite similar background states, the sharpening and evolution of mesoscale gradients at convergence zones plays out quite differently. Here, we conduct a qualitative and statistical comparison of these two seas, with the goal of bringing to light fundamental underlying dynamics that will hopefully improve the accuracy of forecast models in both parts of the world.
    Description: We gratefully acknowledge support from the Office of Naval Research, the National Science Foundation, and the Ocean Mixing and Monsoon (OMM) program of the Monsoon Mission of India.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2022-05-26
    Description: © The Author(s), 2020. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Wong, A. P. S., Wijffels, S. E., Riser, S. C., Pouliquen, S., Hosoda, S., Roemmich, D., Gilson, J., Johnson, G. C., Martini, K., Murphy, D. J., Scanderbeg, M., Bhaskar, T. V. S. U., Buck, J. J. H., Merceur, F., Carval, T., Maze, G., Cabanes, C., Andre, X., Poffa, N., Yashayaev, I., Barker, P. M., Guinehut, S., Belbeoch, M., Ignaszewski, M., Baringer, M. O., Schmid, C., Lyman, J. M., McTaggart, K. E., Purkey, S. G., Zilberman, N., Alkire, M. B., Swift, D., Owens, W. B., Jayne, S. R., Hersh, C., Robbins, P., West-Mack, D., Bahr, F., Yoshida, S., Sutton, P. J. H., Cancouet, R., Coatanoan, C., Dobbler, D., Juan, A. G., Gourrion, J., Kolodziejczyk, N., Bernard, V., Bourles, B., Claustre, H., D'Ortenzio, F., Le Reste, S., Le Traon, P., Rannou, J., Saout-Grit, C., Speich, S., Thierry, V., Verbrugge, N., Angel-Benavides, I. M., Klein, B., Notarstefano, G., Poulain, P., Velez-Belchi, P., Suga, T., Ando, K., Iwasaska, N., Kobayashi, T., Masuda, S., Oka, E., Sato, K., Nakamura, T., Sato, K., Takatsuki, Y., Yoshida, T., Cowley, R., Lovell, J. L., Oke, P. R., van Wijk, E. M., Carse, F., Donnelly, M., Gould, W. J., Gowers, K., King, B. A., Loch, S. G., Mowat, M., Turton, J., Rama Rao, E. P., Ravichandran, M., Freeland, H. J., Gaboury, I., Gilbert, D., Greenan, B. J. W., Ouellet, M., Ross, T., Tran, A., Dong, M., Liu, Z., Xu, J., Kang, K., Jo, H., Kim, S., & Park, H. Argo data 1999-2019: two million temperature-salinity profiles and subsurface velocity observations from a global array of profiling floats. Frontiers in Marine Science, 7, (2020): 700, doi:10.3389/fmars.2020.00700.
    Description: In the past two decades, the Argo Program has collected, processed, and distributed over two million vertical profiles of temperature and salinity from the upper two kilometers of the global ocean. A similar number of subsurface velocity observations near 1,000 dbar have also been collected. This paper recounts the history of the global Argo Program, from its aspiration arising out of the World Ocean Circulation Experiment, to the development and implementation of its instrumentation and telecommunication systems, and the various technical problems encountered. We describe the Argo data system and its quality control procedures, and the gradual changes in the vertical resolution and spatial coverage of Argo data from 1999 to 2019. The accuracies of the float data have been assessed by comparison with high-quality shipboard measurements, and are concluded to be 0.002°C for temperature, 2.4 dbar for pressure, and 0.01 PSS-78 for salinity, after delayed-mode adjustments. Finally, the challenges faced by the vision of an expanding Argo Program beyond 2020 are discussed.
    Description: AW, SR, and other scientists at the University of Washington (UW) were supported by the US Argo Program through the NOAA Grant NA15OAR4320063 to the Joint Institute for the Study of the Atmosphere and Ocean (JISAO) at the UW. SW and other scientists at the Woods Hole Oceanographic Institution (WHOI) were supported by the US Argo Program through the NOAA Grant NA19OAR4320074 (CINAR/WHOI Argo). The Scripps Institution of Oceanography's role in Argo was supported by the US Argo Program through the NOAA Grant NA15OAR4320071 (CIMEC). Euro-Argo scientists were supported by the Monitoring the Oceans and Climate Change with Argo (MOCCA) project, under the Grant Agreement EASME/EMFF/2015/1.2.1.1/SI2.709624 for the European Commission.
    Keywords: global ; ocean ; pressure ; temperature ; salinity ; Argo ; profiling ; floats
    Repository Name: Woods Hole Open Access Server
    Type: Article
    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...