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  • 1
    Publication Date: 2024-07-04
    Description: To gain information on the physical parameters of deep water in the Northwest Atlantic, CTD measurements were taken during seven dives to the RMS Titanic wreck (front of bow approx. 41.7330181, -49.9460561; 3816 m water depth) and one dive to the Nargeolet-Fanning Ridge (approx. 41.5980514, -49.4386889; 2896 m water depth) during the OceanGate expedition aboard the AHTS Horizon Arctic, 15 June - 25 July 2022. The CTD measurements of the water column down to a maximum water depth of 3853 m were conducted using a Valeport MIDAS SVX2 6000 unit attached to the submersible Titan for the duration of each dive and provided standard data for conductivity, temperature, and pressure. Conductivity and temperature data were used to compute salinity.
    Keywords: Conductivity; CTD; CTD, Valeport, MIDAS SVX2 6000, mounted on submersible; CTD-MIDAS_SVX2-SUB; CTD profile; DATE/TIME; Deep sea; Density, sigma-theta (0); Depth; DEPTH, water; Doppler velocity log (DVL), Sonardyne, mounted on submersible; DVL_Sonardyne_SUB; Event label; Horizon Arctic (AHTS); iAtlantic; Integrated Assessment of Atlantic Marine Ecosystems in Space and Time; LATITUDE; LONGITUDE; Newfoundland; Northwest Atlantic; Number of observations; NW Atlantic; OceanGate; Pressure, water; Salinity; Sigma theta (calculated, using CTD salinity); Temperature; Temperature, water; Titan-2022-C2_0073; Titan-2022-C2_0075; Titan-2022-C2_0076; Titan-2022-C2_0079; Titan-2022-C2_0080; Titan-2022-C2_0081; Titan-2022-C2_0082; Titan-2022-C2_0083
    Type: Dataset
    Format: text/tab-separated-values, 1242327 data points
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  • 2
    Call number: 6/M 24.95762
    In: International Association of Geodesy Symposia, 155
    Description / Table of Contents: Intro -- Preface -- Contents -- Part I Gravity Field Modelling and Height Systems -- Remarks on the Terrain Correction and the Geoid Bias -- 1 Introduction -- 2 The Terrain Correction for Masses Located in the Remote Zone of the Bouguer Shell -- 3 The Terrain Correction for Masses Located Outside the Bouguer Plate -- 4 The Terrain Correction Due to Masses in the Near-Zone Inside the Bouguer Plate -- 5 Conclusions -- References -- Why a Height Theory Must Be Rigorous and Physically Correct -- 1 Review -- 2 Problems with Molodensky's Approach -- 3 Arrival of Satellites and the Problem of Height Congruency -- 4 Conclusions -- References -- Geodetic Heights and Holonomity -- 1 Introduction -- 2 What Is a Geodetic Heigh? -- 2.1 A New Definition of a General Geodetic Height HG -- 3 The Four Height Systems Are Geodetic Heights -- 4 Holonomity of the Geodetic Heights -- 5 Comparisons and Conclusions -- References -- Physical Heights of Inland Lakes -- 1 Introduction -- 2 Orthometric Height -- 3 Orthometric Height Variation at Lake Surface -- 4 Quantification: Case Studies -- 4.1 Lake Vänern, Sweden -- 4.2 Lake Michigan, USA -- 4.3 Issyk Kul, Kyrgyzstan -- 4.4 Salar de Uyuni, Bolivia -- 5 Conclusions and Outlook -- Appendix 1: Approximation -- Appendix 2: Normal Height Variation -- References -- The Uncertainties of the Topographical Density Variations in View of a Sub-Centimetre Geoid -- 1 Introduction -- 2 Theory -- 3 Numerical Results -- 4 Conclusion and Remarks -- References -- Estimation of Height Anomalies from Gradients of the Gravitational Potential Using a Spectral Combination Method -- 1 Introduction -- 2 Spectral Combination -- 3 Numerical Experiments -- 4 Conclusion -- References -- Evaluation of the Recent African Gravity Databases V2.x -- 1 Introduction -- 2 Data Used for Establishing the AFRGDB_V2.x Gravity Databases.
    Type of Medium: Monograph available for loan
    Pages: 189 Seiten , Illustrationen
    Edition: 1st ed.
    ISBN: 9783031553592
    Series Statement: International Association of Geodesy Symposia Series 155
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
    Call number: https://doi.org/10.1007/978-3-031-55360-8
    In: International Association of Geodesy Symposia, 155
    Description / Table of Contents: Part I: Gravity Field Modelling and Height Systems -- Remarks on the Terrain Correction and the Geoid Bias -- Why a Height Theory Must Be Rigorous and Physically Correct -- Geodetic Heights and Holonomity -- Physical Heights of Inland Lakes -- The Uncertainties of the Topographical Density Variations in View of a Sub-Centimetre Geoid -- Estimation of Height Anomalies from Gradients of the Gravitational Potential Using a Spectral Combination Method -- Evaluation of the Recent African Gravity Databases V2.x -- Part II : Estimation Theory -- PDF Evaluation of Elliptically Contoured GNSS Integer Ambiguity Residuals -- Spatio-Spectral Assessment of Some Isotropic Polynomial Covariance Functions on the Sphere -- MDBs Versus MIBs in Case of Multiple Hypotheses: A Study in Context of Deformation Analysis -- A Simple TLS-Treatment of the Partial EIV-Model as One with Singular Cofactor Matrices I: The Case of a Kronecker Product for QA = Q0 ⊗ Qx -- Bayesian Robust Multivariate Time Series Analysis in Nonlinear Regression Models with Vector Autoregressive and t-Distributed Errors -- Part III: Geodetic Data Analysis -- An Estimate of the Effect of 3D Heterogeneous Density Distribution on Coseismic Deformation Using a Spectral Finite-Element Approach -- On the Estimation of Time Varying AR Processes -- Refinement of Spatio-Temporal Finite Element Spaces for Mean Sea Surface and Sea Level Anomaly Estimation -- On the Coestimation of Long-Term Spatio-Temporal Signals to Reduce the Aliasing Effect in Parametric Geodetic Mean Dynamic Topography Estimation -- A Flexible Family of Compactly Supported Covariance Functions Based on Cutoff Polynomials -- Modeling of Inhomogeneous Spatio-Temporal Signals by Least Squares Collocation -- A Multi-Epoch Processing Strategy for PPP-RTK Users -- Part IV: Geoid and Quasi-Geoid -- Geoid or Quasi-Geoid? A Short Comparison -- The Quasigeoid: Why Molodensky Heights Fail -- Molodensky’s and Helmert’s Theories: Two Equivalent Geodetic Approaches to the Determination of the Gravity Potential and the Earth Surface. .
    Description / Table of Contents: This open access volume contains the proceedings of the X Hotine-Marussi Symposium on Mathematical Geodesy which was held from 13 to 17 June 2022 at the Politecnico di Milano, Milan, Italy. Since 2006 the series of the Hotine-Marussi Symposia has been under the responsibility of the Inter-Commission Committee on Theory (ICCT) within the International Association of Geodesy (IAG). The ICCT organized the last five Hotine-Marussi Symposia held in Wuhan (2006), Rome (2009, 2013 and 2018), and Milan (2022). The overall goal of the ICCT and Hotine-Marussi Symposia has always been to advance geodetic theory which is indeed documented by the 22 research articles published in these proceedings. The jubilee X Hotine-Marussi Symposium was organized in 10 topical sessions covering all parts of geodetic theory including reference frames, gravity field modelling, adjustment theory, height systems, time series analysis, or advanced numerical methods. In total, 60 participants attended the Symposium who delivered 62 oral and 18 poster presentations. During a special session, five invited speakers discussed two basic concepts of physical geodesy – geoid and quasigeoid.
    Type of Medium: 12
    Pages: 1 Online-Ressource(X, 165 p. 76 illus., 64 illus. in color.)
    Edition: 1st ed. 2024.
    ISBN: 9783031553608
    Series Statement: International Association of Geodesy Symposia 155
    Language: English
    Branch Library: GFZ Library
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  • 4
    Publication Date: 2024-07-03
    Description: Highlights • All investigated sites are in quiescent stage. Multi layers of clam shell debris were the ancient sediment surfaces during high methane flux. • Current fluxes contribute to less than 2 wt % of authigenic carbonates and 2 wt % iron sulfide minerals being precipitated in 600-800 cm sediment. • The sequestration of carbon could be 〉 50 mmol C cm-2 yr-1 under current in situ condition. Abstract Methane seepage records information of the local carbon cycle with respect to the generation, consumption and sequestration of carbon. Here presents the investigation of 7 gravity cores retrieved in 2004 during cruise SO-177 in the Haiyang 4 Area at the northern slope of the South China Sea. Porewater solutes, sulfate, methane, total alkalinity, sulfide and calcium demonstrate currently the weak seep activity. Local carbon cycling and sequestration is also revealed, that dominates by anaerobic oxidation of biogenic methane to dissolved bicarbonate inducing calcium carbonate and iron sulfide minerals (mainly pyrite) precipitation. A reactive transport model was employed to quantify the carbon cycle and budget. Model results show that current methane fluxes contribute to less than 2 wt % of authigenic carbonates and 2 wt % iron sulfide minerals being precipitated in 600–800 cm sediment depth. The sequestration of carbon could be 〉 50 mmol C cm−2 yr−1 under in situ condition. The observed increase of carbonate and iron sulfide minerals at ∼100 cm, however, require higher methane fluxes to shift the zone of anaerobic oxidation of methane upwards to around 1 m below the seafloor, which have occurred during sea level low stands in the geological past. The oscillation of seepage flux contributed to the formation of multiple layers of authigenic carbonates and pyrite, which indicates the high capability of carbon sink and is speculated to be induced by the dissociation of the underlying hydrates triggered by sea level drop and or temperature increase.
    Type: Article , PeerReviewed
    Format: text
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  • 5
    Publication Date: 2024-07-03
    Description: Offshore explosive ordnance disposal (EOD) in the marine environment is a high-risk activity. Structured risk assessment (RA) can be a helpful tool to provide EOD experts with decision-making support. This paper hypothesizes that existing RA approaches that address unexploded ordnance (UXO) in the sea do not meet the requirements of EOD RA. To test this hypothesis, the paper proposes a novel categorization tool. It uses five review criteria: study type (qualitative vs. quantitative), level of decision-making (strategic vs. applied), risk component (probability vs. consequence), spatial scale (global vs. local), and temporal scale (long-term vs. short-term). The categorization tool is used to identify the requirements of EOD RA and to test whether nine existing RA methods fulfill these requirements. The study finds that none of the investigated RAs meets the requirements and, hence, concludes that a new method should be developed. However, some aspects of the existing studies should be considered when designing a new method. This includes using risk factors (type and mass of explosive material, type and state of the fuze, and water depth) that are relevant for EOD RA. It also involves setting up a directed graph to assess the complex interdependencies between these risk factors.
    Type: Article , PeerReviewed
    Format: text
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  • 6
    Publication Date: 2024-07-03
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 7
  • 8
    Publication Date: 2024-07-03
    Description: Abstract
    Description: This data publication includes the half-hourly Hp30 and ap30 indices as well as the hourly Hp60 and ap60 indices, collectively denoted as Hpo. This dataset is based on near real-time geomagnetic observatory data provided by 13 contributing observatories. It is derived and distributed by GFZ German Research Centre for Geosciences. When using the Hpo index, please cite this data publication as well as the accompanying publications Yamazaki et al. (2024) and Yamazaki et al. (2022), which serve as documentation of the Hpo. The dataset is organised in yearly files, which, for the current year, are updated on a monthly basis. Typically, during the second week of a month, the data for the previous month is appended to the current year's file. The files are in ASCII files and start with header lines marked with # (hash). The Hpo index was initially developed within the H2020 project SWAMI (grant agreement No 776287) and is produced by Geomagnetic Observatory Niemegk, GFZ German Research Centre for Geosciences. It derives from the same 13 geomagnetic observatories that also contribute to the Kp index (Matzka et al., 2021, https://doi.org/10.5880/Kp.0001). They are listed as contributors to this data publication. With the introduction of the DOI for the Hpo index (Matzka et al, 2021, https://doi.org/10.5880/Hpo.0001), this DOI landing page and the associated HTTPS server linked to the DOI become the primary archive of Hpo (while the other established index distribution mechanisms at GFZ will be maintained in parallel). With the DOI, the dataset can grow with time, but a change of the data, once published, is not possible. If necessity arises in the future to correct already published values, then the corrected dataset will be published with a new DOI. Older DOIs and data sets will then still be available. For each DOI, an additional versioning mechanism will be available to document changes to the files such as header or format changes, which do not affect the integrity of the data. The DOI https://doi.org/10.5880/Hpo.0003 identifies the current version. A format description and a version history are provided in the data download folder.
    Description: Other
    Description: Version history: 2024-07-10: publication of version 3.0 (https://doi.org/10.5880/Hpo.0003). This version replaces version Hpo.0001 and Hpo.0002. The algorithm to calculate Hpo was changed to give a better occurrence frequency of index values for Hpo 〉= 9. Additionally, index values for 1984 to 1995 were added. The change is described in the accompanying publication. ------------------------------------------------------------ 2022-05-13: Addition of key reference (Yamazaki et al. 2022, https://doi.org/10.1029/2022GL098860) to the landing page, the data files and the format description (metadata update, no new version released) ------------------------------------------------------------ 2022-03-26: Publication of Version 2.0 (https://doi.org/10.5880/Hpo.0001). This version replaces version Hpo.0001. The Hpo, like the Kp nowcast, is based on the FMI algorithm (see Matzka et al., 2021, https://doi.org/10.1029/2020SW002641) and goes through a rescaling procedure to be more similar to the definitive Kp values. The data in version Hpo.0001 from 2018 onwards suffered from a slight error in this rescaling algorithm, causing for example somewhat too few Hpo 0 values and somewhat too many Hpo 0.333 values. This error was corrected for version Hpo.0002. The values from 1995 to 2017 are identical for both versions. ------------------------------------------------------------ 2021-04-26: Publication of Version 1.0 (https://doi.org/10.5880/Hpo.0001)
    Keywords: Hpo ; Hpo index ; Hp30 ; ap30 ; Hp60 ; ap60 ; Kp ; Kp index ; ap index ; geomagnetism ; space weather ; space physics ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMAGNETISM ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMAGNETISM 〉 GEOMAGNETIC INDICES 〉 KP INDEX ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 IONOSPHERE/MAGNETOSPHERE DYNAMICS 〉 AURORAE ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 IONOSPHERE/MAGNETOSPHERE DYNAMICS 〉 GEOMAGNETIC INDICES ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 IONOSPHERE/MAGNETOSPHERE DYNAMICS 〉 MAGNETIC FIELDS/MAGNETIC CURRENTS ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 IONOSPHERE/MAGNETOSPHERE DYNAMICS 〉 MAGNETIC STORMS ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 IONOSPHERE/MAGNETOSPHERE DYNAMICS 〉 SOLAR WIND
    Type: Dataset , Dataset
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  • 9
    Publication Date: 2024-07-03
    Description: Le présent travail tente de mettre au point une technique reproductrice de production post-larvaire de crevette Penaeus Kerathurus, au Centre National d’Aquaculture de Monastir (C.N.A.) et de définir les normes et rendements de chaque étape de l'écloserie (élevages des larves et des post-larves). Au niveau des élevages larvaires le bilan, montre que les petits volumes (350 l),donnent de meilleurs résultats zootechniques que les grands volumes (2 et 4m3) avec un meilleur contrôle des paramètres du milieu et de l'état des larves. Les meilleurs rendements sont obtenus à la densité initiale de 160 N/l et avec le rationnement des Artemia, par une distribution en continue (goutte à goutte). Pendant l'élevage post-larvaire, l'utilisation d'un aliment composé sec s'avère nécessaire. Cet aliment abouti en effet à de meilleurs résultats zootechniques que le zooplancton ou les clovisses congelés. L'acquisition de l'activité benthique des post-larves, à partir de P15-P20, nécessite par ailleurs l'utilisation de bac à fond plat. A la température moyenne de 25,5°C, les post-larves atteignent les tailles de 5 mm à P10, 6mm à P16, 10mm à P35 et 12mm à P40, quand elles sont sevrées sur Artemia congelées puis nourries avec un aliment composé sec à 55. de protéines et 14. de lipides
    Description: Published
    Description: Refereed
    Keywords: PRODUCTION HALIEUTIQUE ; COQUILLAGES ET CRUSTACES ; AQUACULTURE
    Repository Name: AquaDocs
    Type: Journal Contribution
    Format: 29-47 pp
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  • 10
    Publication Date: 2024-07-03
    Description: Le présent travail montre qu'il est possible d'obtenir des pontes de la crevette royale Penaeus Kerathurus en écloserie à partir de pondeuses pêchées matures, au large de Monastir pendant le mois de juin. Il propose une technique reproductible de conditionnement des femelles capturées non encores matures, en vue de programmer les pontes en fonction de la disponibilité des structures des élevages larvaires et post-larvaires. L'épédonculation permet la maturation et l'échelonnement des pontes. Maintenues à la charge de 8 individus/m², au sex-ratio de 1/2 dans des conditions physico-chimiques stables et sur une alimentation fraîche, les femelles pondent dans les 16 à 32 jours qui suivent l'épédondulation. Les taux de fertilisation et d'éclosion sont respectivement de 75 plus ou moins 5. et 63 plus ou moins 9. et la fécondité d'une femelle de 57 plus ou moins 6g est en moyenne de 115000 oeufs/ponte
    Description: Published
    Description: Refereed
    Keywords: FERTILITE ; COQUILLAGES ET CRUSTACES ; ECLOSION ; MAITRISE DE LA REPRODUCTION
    Repository Name: AquaDocs
    Type: Journal Contribution
    Format: 175-182pp
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