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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Oceanography. ; Electronic books.
    Description / Table of Contents: This book addresses the important and apparently simple question: "How can continuous and reliable monitoring at the seafloor by means of seafloor observatories extend exploration and improve knowledge of our planet?".
    Type of Medium: Online Resource
    Pages: 1 online resource (688 pages)
    Edition: 1st ed.
    ISBN: 9783642113741
    Series Statement: Springer Praxis Bks.
    DDC: 551.46
    Language: English
    Note: Intro -- Contents -- List of figures -- List of tables -- 1 Introduction -- Part I Present scientific challenges to be addressed using seafloor observatories -- 2 Integrating continuous observatory data from the coast to the abyss: Assembling a multidisciplinary view of the ocean in four dimensions -- 2.1 Introduction -- 2.2 Spatial (environmental) scope -- 2.3 Temporal scope -- 2.4 Catastrophic episodicity -- 2.5 Complex interconnectedness -- 2.6 Challenges of multidisciplinarity -- 2.7 Integrated networks -- 2.8 Scientific initiatives -- 2.9 Scientific development -- 2.9.1 Builders -- 2.9.2 Future builders -- 2.9.3 Bridge-builders -- 2.9.4 Data analysts -- 2.9.5 Knowledge beneficiaries -- 2.10 Participants and data access -- 2.11 Summary -- References -- 3 Underwater neutrino telescopes: Detectors for astro-particle physics and a gateway for deep-sea laboratories -- 3.1 Introduction -- 3.2 High-energy neutrino astronomy -- 3.3 High-energy neutrino detection -- 3.3.1 The Cherenkov detection technique in transparent natural media -- 3.3.2 Underwater Cherenkov neutrino telescopes -- 3.4 Towards a deep-sea infrastructure for neutrino astronomy and Earth and sea science in the Mediterranean Sea -- 3.4.1 NESTOR: Neutrino Extended Submarine Telescope with Oceanographic Research -- 3.4.2 ANTARES: Astronomy with a Neutrino Telescope and Abyss environmental RESearch -- 3.4.3 NEMO: NEutrino Mediterranean Observatory -- 3.4.4 KM3NeT -- 3.4.4.1 Optical modules -- 3.4.4.2 Detection unit mechanical structure -- 3.4.4.3 Readout technology -- 3.4.4.4 Sea-floor network -- 3.5 Beyond the km3: New techniques for ultra-high-energy neutrino detection -- 3.6 Deep-sea science with neutrino telescopes -- 3.6.1 Bioluminescence -- 3.6.2 Seawater optical properties -- 3.6.3 Biofouling and sedimentation -- 3.6.4 Underwater currents -- 3.6.5 Bioacoustics -- 3.6.6 Geophysics. , 3.7 Conclusions -- References -- Web resources -- 4 Seafloor observations and observatory activities in the Sea of Marmara -- 4.1 Introduction -- 4.2 Geohazards in the Sea of Marmara -- 4.2.1 The Sea of Marmara seismic gap -- 4.2.2 Submarine landslides -- 4.2.3 Tsunamis -- 4.3 Fluids and seismicity in the Sea of Marmara -- 4.4 Oceanographic and environmental sensitivity of the Sea of Marmara -- 4.5 Sensors for seafloor observations in the Sea of Marmara -- 4.5.1 Seismic motion -- 4.5.2 Flowmeters -- 4.5.3 Piezometers (pore-pressure sensors) -- 4.5.4 Gas-bubble monitoring -- 4.5.5 Methane sensor -- 4.5.6 Oceanographic sensors -- 4.6 Recommended observatory sites -- 4.7 Present initiatives for seafloor observatories in the Sea of Marmara -- 4.7.1 Marmara Sea Bottom Observatory (MSBO) project -- 4.7.2 The ESONET Marmara-Demonstration Mission project -- 4.8 Conclusions -- References -- 5 The Hellenic deep sea observatory: Science objectives and implementation -- 5.1 Introduction -- 5.2 Hellenic observatory: Science objectives -- 5.2.1 Geodynamics and seismicity -- 5.2.2 Seafloor instabilities -- 5.2.3 Tsunamis -- 5.2.4 Fluid flow and mud volcanism -- 5.2.5 Thermohaline circulation and climate change -- 5.3 Existing stand-alone observatory (Poseidon system - Pylos site) -- 5.3.1 Surface buoy: Air-sea interaction monitoring -- 5.3.2 Water column monitoring -- 5.3.3 Seabed platform -- 5.4 Ongoing operation management -- 5.4.1 Data flow, management and quality control procedures -- 5.4.2 Data and information product dissemination -- 5.4.3 Operation of the POSEIDON-Pylos observatory, 2007-2010 -- 5.5 Concluding remarks -- Acknowledgments -- References -- 6 Marine seismogenic-tsunamigenic prone areas: The Gulf of Cadiz -- 6.1 Introduction -- 6.2 Large earthquakes and tsunamis in the Gulf of Cadiz -- 6.3 Main hazard source zones in SW Iberia. , 6.3.1 Gloria Fault -- 6.3.2 SW Iberian transpressive domain -- 6.3.2.1 Gorringe Bank zone -- 6.3.2.2 Horseshoe Marques-de-Pombal zone -- 6.3.2.3 The Algarve Margin -- 6.3.2.4 East dipping subduction slab -- 6.4 The strategy for seafloor continuous monitoring -- 6.4.1 First results -- 6.5 Conclusions -- Acknowledgments -- References -- Part II Technical solutions for seafloor observatory architecture -- 7 The role of Information Communication Technologies (ICT) for seafloor observatories: Acquisition, archival, analysis, interoperability -- 7.1 Introduction -- 7.2 Different types of ocean observatories -- 7.3 Benefits of ICT for an ocean observatory -- 7.4 Mandate of a software infrastructure for ocean observatories -- 7.5 Observatory system design -- 7.5.1 Design decisions imposed on the ICT -- 7.5.2 Network design considerations -- 7.5.3 National security issues -- 7.5.4 General network security threats mitigation -- 7.5.5 Design choices -- 7.5.6 Private network and IP address range -- 7.5.7 Access only through VPN or through software proxies -- 7.5.8 Isolation of VLANs to isolate instrument categories from one another -- 7.5.9 User authentication and authorization -- 7.5.10 Timing and time signals -- 7.6 Data acquisition -- 7.6.1 Data types in ocean sciences -- 7.6.1.1 Data flow as streams - Data flow as an event management problem -- 7.6.1.2 Interfaces to many different types of instruments -- 7.6.1.3 Interoperability -- 7.6.1.4 Science data vs. engineering data -- 7.6.2 Data archive and distribution management -- 7.6.2.1 The cost of a 25-year mandate -- 7.6.3 Data repository growth: Constant, linear or exponential? -- 7.6.3.1 Types of products -- 7.6.3.2 Evolution of raw data rate -- 7.6.3.3 Adapting the storage structure to expected use -- 7.6.3.4 Observatory assets management and operation support -- 7.6.3.5 Data access and analysis. , 7.6.3.6 Remote use of underwater assets -- 7.7 Summary -- 7.8 Non-exhaustive list of ocean observatories -- Reference -- Glossary of acronyms -- 8 Long-term subsea observatories: Comparison of architectures and solutions for infrastructure design, interfaces, materials, sensor protection and deployment operations -- 8.1 Introduction -- 8.2 Comparison between observatory architectures -- 8.2.1 Vertically cabled architecture -- 8.2.2 Non-cabled architecture -- 8.2.3 Cabled architecture -- 8.2.3.1 Architecture and mechanical design of a node and a junction box -- Mechanical design overview -- SJB design solutions -- 8.3 Recommendations for signals, protocols and connector pin-out between infrastructure and instrumentation -- 8.4 Long-term deployment: Materials for subsea observatories -- 8.5 Long-term deployment: Biofouling protection for marine environmental devices and sensors -- 8.5.1 Biofouling protection by "controlled" biocide generation: Localized seawater electro-chlorination system -- 8.6 ROV operations: Deployment and maintenance operations -- 8.7 Conclusion and next steps -- Acknowledgments -- References -- Web resources -- Glossary -- 9 Development and demonstration of a mobile response observatory prototype for subsea environmental monitoring: The case of ROSE -- 9.1 Introduction -- 9.2 System specifications -- 9.2.1 Functional specifications -- 9.2.2 Technical specifications -- 9.2.2.1 Acoustic network -- 9.2.2.2 Radio-electric link -- 9.2.2.3 Information flows -- 9.2.2.4 Sea bottom stations -- 9.2.2.5 The buoy -- 9.2.2.6 On-shore control station -- 9.2.2.7 Messengers -- 9.3 Study and construction of a prototype system -- 9.3.1 Seafloor stations -- 9.3.2 Buoy -- 9.3.3 Sensors -- 9.4 Prototype tests in Ifremer seawater tank -- 9.4.1 Station tests -- 9.4.2 Messenger tests -- 9.5 Demonstration at sea -- 9.5.1 Sea operations. , 9.5.1.1 System deployment -- 9.5.1.2 System operation from mid-June to early September -- 9.5.1.3 System recovery -- 9.5.2 Analyses of at-sea demonstration results -- 9.5.2.1 Communication system and station operation -- 9.5.2.2 Biofouling -- 9.5.2.3 Messenger -- 9.5.2.4 Sensors -- 9.6 Conclusions -- List of abbreviations -- Acknowledgment -- References -- 10 Construction of the DONET real-time seafloor observatory for earthquakes and tsunami monitoring -- 10.1 Introduction -- 10.2 System overview -- 10.3 Backbone cable system -- 10.4 Science node -- 10.5 Observatory -- 10.6 Scenario -- 10.7 ROV for observatory construction -- 10.8 DONET construction -- 10.9 Summary -- Acknowledgment -- References -- 11 GEOSTAR-class observatories 1995-2012: A technical overview -- 11.1 Introduction -- 11.2 The origins: ABEL and DESIBEL -- 11.3 GEOSTAR -- 11.3.1 GEOSTAR mission 1 (Adriatic Sea) -- 11.3.2 GEOSTAR mission 2 (Southern Tyrrhenian Sea) -- 11.3.3 GEOSTAR missions 3 and 4 (Southern Tyrrhenian Sea) -- 11.3.4 GEOSTAR mission 5 (Gulf of Cadiz) -- 11.3.5 GEOSTAR mission 6 (Gulf of Cadiz) -- 11.4 SN1 -- 11.4.1 SN1 mission 1 (Ionian Sea) -- 11.4.2 SN1 mission 2 (Ionian Sea) -- 11.4.3 SN1 mission 3 (Ionian Sea) -- 11.5 MABEL (SN2) -- 11.5.1 MABEL (SN2) mission 1 (Weddell Sea, Antarctica) -- 11.6 SN3 -- 11.6.1 SN3 missions 1 and 2 (Southern Tyrrhenian Sea) -- 11.7 SN4 -- 11.7.1 SN4 mission 1 (Corinth Gulf) -- 11.7.2 SN4 missions 2 and 3 (Marmara Sea) -- 11.8 GMM -- 11.8.1 GMM missions 1 and 2 (Gulf of Patras) -- 11.8.2 GMM mission 3 (Ionian Sea) -- 11.9 Conclusions -- Acknowledgments -- References -- Part III World-wide recent and ongoing projects and programmes -- 12 The two seafloor geomagnetic observatories operating in the western Pacific -- 12.1 Introduction -- 12.2 Instrumentation at sea -- 12.3 Seafloor experiments. , 12.3.1 Observed time-series on the seafloor.
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  • 2
    Keywords: Oceanographic research stations Congresses ; Ocean bottom Research ; Congresses ; Seismology Research ; Congresses ; Konferenzschrift 1999 ; Konferenzschrift ; Tiefsee ; Erforschung ; Gerät ; Messgerät ; Tiefsee ; Forschungsstation ; Technologie ; Ustica ; Tiefsee ; Erforschung ; Gerät ; Messgerät ; Tiefsee ; Forschungsstation ; Technologie ; Forschungsstation ; Tiefsee
    Type of Medium: Book
    Pages: XVIII, 268 S. , Ill.
    ISBN: 0444505911
    Series Statement: Developments in marine technology 12
    DDC: 551.46/0072
    Language: English
    Note: Includes bibliographical references. - Papers from the 16th Course of the International School of Geophysics, held Ustica and Erice, September 1999
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  • 3
    Book
    Book
    Berlin : Springer | Chichester : Praxis Publishing
    Keywords: Meeresboden ; Technische Überwachung ; Wissenschaftliche Beobachtung
    Type of Medium: Book
    Pages: XXX, 676 S. , Ill., Kt. , 260 mm x 193 mm
    ISBN: 9783642113734
    Series Statement: Springer-Praxis books in geophysical sciences
    DDC: 550
    Language: English
    Note: Literaturangaben
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  • 4
    Keywords: Geography ; Physical geography ; Oceanography ; Aquatic biology ; Meeresboden ; Technische Überwachung ; Wissenschaftliche Beobachtung
    Description / Table of Contents: The oceans cover 70% of the terrestrial surface, and exert a pervasive influence on the Earth's environment but their nature is poorly recognized. Knowing the ocean's role deeply and understanding the complex, physical, biological, chemical and geological systems operating within it represent a major challenge to scientists today. Seafloor observatories offer scientists new opportunites to study multiple, interrelated natural phenomena over time scales ranging from seconds to decades, from episodic to global and long-term processes. Seafloor Observatories addresses the important and apparently simple question, "How can continuous and reliable monitoring at the seafloor by means of Seafloor Observatories extend exploration and improve knowledge of our planet?" The book leads the reader through the present scientific challenges to be addressed with seafloor observatories; the technical solutions for their architecture; an excursus on worldwide ongoing projects and programmes. some relevant scientific multidisciplinary results; and a presentation of new and interesting long-term perspectives for the coming years. Scientific results from seafloor observatories will yield significant improvements and exert a strong impact not only on current knowledge of our Planet but also on human life evolution
    Type of Medium: Online Resource
    Pages: Online-Ressource (688 p)
    Edition: Springer eBook Collection. Earth and Environmental Science
    ISBN: 9783642113741
    Series Statement: Springer praxis books in geophysical sciences
    DDC: 551.46
    Language: English
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  • 5
    Publication Date: 2019-09-23
    Description: Society’s needs for a network of in situ ocean observing systems cross many areas of earth and marine science. Here we review the science themes that benefit from data supplied from ocean observatories. Understanding from existing studies is fragmented to the extent that it lacks the coherent long-term monitoring needed to address questions at the scales essential to understand climate change and improve geo-hazard early warning. Data sets from the deep sea are particularly rare with long-term data available from only a few locations worldwide. These science areas have impacts on societal health and well-being and our awareness of ocean function in a shifting climate. Substantial efforts are underway to realise a network of open-ocean observatories around European Seas that will operate over multiple decades. Some systems are already collecting high-resolution data from surface, water column, seafloor, and sub-seafloor sensors linked to shore by satellite or cable connection in real or near-real time, along with samples and other data collected in a delayed mode. We expect that such observatories will contribute to answering major ocean science questions including: How can monitoring of factors such as seismic activity, pore fluid chemistry and pressure, and gas hydrate stability improve seismic, slope failure, and tsunami warning? What aspects of physical oceanography, biogeochemical cycling, and ecosystems will be most sensitive to climatic and anthropogenic change? What are natural versus anthropogenic changes? Most fundamentally, how are marine processes that occur at differing scales related? The development of ocean observatories provides a substantial opportunity for ocean science to evolve in Europe. Here we also describe some basic attributes of network design. Observatory networks provide the means to coordinate and integrate the collection of standardised data capable of bridging measurement scales across a dispersed area in European Seas adding needed certainty to estimates of future oceanic conditions. Observatory data can be analysed along with other data such as those from satellites, drifting floats, autonomous underwater vehicles, model analysis, and the known distribution and abundances of marine fauna in order to address some of the questions posed above. Standardised methods for information management are also becoming established to ensure better accessibility and traceability of these data sets and ultimately to increase their use for societal benefit. The connection of ocean observatory effort into larger frameworks including the Global Earth Observation System of Systems (GEOSS) and the Global Monitoring of Environment and Security (GMES) is integral to its success. It is in a greater integrated framework that the full potential of the component systems will be realised. Highlights ► Societies increasingly depend on timely information on ecosystems and natural hazards. ► Data is needed to improve climate-related uncertainty and geo-hazard early warning. ► Observatory networks coordinate and integrate the collection of standardised data. ► Ocean observatories provide opportunity for ocean science to evolve.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 6
    Publication Date: 2022-01-31
    Description: Increasing interest in the acquisition of biotic and abiotic resources from within the deep sea (e.g., fisheries, oil–gas extraction, and mining) urgently imposes the development of novel monitoring technologies, beyond the traditional vessel-assisted, time-consuming, high-cost sampling surveys. The implementation of permanent networks of seabed and water-column-cabled (fixed) and docked mobile platforms is presently enforced, to cooperatively measure biological features and environmental (physicochemical) parameters. Video and acoustic (i.e., optoacoustic) imaging are becoming central approaches for studying benthic fauna (e.g., quantifying species presence, behavior, and trophic interactions) in a remote, continuous, and prolonged fashion. Imaging is also being complemented by in situ environmental-DNA sequencing technologies, allowing the traceability of a wide range of organisms (including prokaryotes) beyond the reach of optoacoustic tools. Here, we describe the different fixed and mobile platforms of those benthic and pelagic monitoring networks, proposing at the same time an innovative roadmap for the automated computing of hierarchical ecological information on deep-sea ecosystems (i.e., from single species’ abundance and life traits to community composition, and overall biodiversity).
    Type: Article , PeerReviewed
    Format: text
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  • 7
    Publication Date: 2011-06-01
    Description: A cumulative frequency-magnitude relation, the Gutenberg-Richter law, dominates the statistics of the occurrence of earthquakes. Although it is an empirical law, some authors have tried to give some physical meaning to its a and b parameters. Here, we recall some theoretical expressions for the probability of occurrence of an earthquake with magnitude M in terms of a and b values. A direct consequence of the maximum likelihood estimation (MLE) and the maximum entropy principle (MEP) is that a and b values can be expressed as a function of the mean magnitude of a seismic sequence over a certain area. We then introduce the definition of the Shannon entropy of earthquakes and show how it is related to the b value. In this way, we also give a physical interpretation to the b value: the negative logarithm of b is the entropy of the magnitude frequency of earthquake occurrence. An application of these concepts to two case studies, in particular to the recent seismic sequence in Abruzzi (central Italy; mainshock Mw 6.3, 6 April 2009 in L'Aquila) and to an older 1997 sequence (Umbria-Marche, central Italy; mainshock Mw 6.0, 26 September 1997 in Colfiorito), confirms their potential to help in understanding the physics of earthquakes. In particular, from the comparison of the two cases, a simple scheme of different regimes in succession is proposed in order to describe the dynamics of both sequences.
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
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  • 8
    Publication Date: 2021-06-25
    Description: Understanding micro-seismicity is a critical question for earthquake hazard assessment. Since the devastating earthquakes of Izmit and Duzce in 1999, the seismicity along the submerged section of North Anatolian Fault within the Sea of Marmara (comprising the “Istanbul seismic gap”) has been extensively studied in order to infer its mechanical behaviour (creeping vs locked). So far, the seismicity has been interpreted only in terms of being tectonic-driven, although the Main Marmara Fault (MMF) is known to strike across multiple hydrocarbon gas sources. Here, we show that a large number of the aftershocks that followed the M 5.1 earthquake of July, 25th 2011 in the western Sea of Marmara, occurred within a zone of gas overpressuring in the 1.5–5 km depth range, from where pressurized gas is expected to migrate along the MMF, up to the surface sediment layers. Hence, gas-related processes should also be considered for a complete interpretation of the micro-seismicity (~M 〈 3) within the Istanbul offshore domain.
    Description: Published
    Description: id 6819
    Description: 3A. Geofisica marina e osservazioni multiparametriche a fondo mare
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
    Publication Date: 2020-10-29
    Description: Acoustic noise levels were measured in the Gulf of Catania (Ionian Sea) from July 2012 to May 2013 by a low frequency (〈1000Hz) hydrophone, installed on board the NEMO-SN1 multidisciplinary observatory. NEMO-SN1 is a cabled node of EMSO-ERIC, which was deployed at a water depth of 2100m, 25km off Catania. The study area is characterized by the proximity of mid-size harbors and shipping lanes. Measured noise levels were correlated with the passage of ships tracked with a dedicated AIS antenna. Noise power was measured in the frequency range between 10Hz and 1000Hz. Experimental data were compared with the results of a fast numerical model based on AIS data to evaluate the contribution of shipping noise in six consecutive 1/3 octave frequency bands, including the 1/3 octave frequency bands centered at 63Hz and 125Hz, indicated by the Marine Strategy Framework Directive (2008/56/EC).
    Description: Published
    Description: 97-103
    Description: 3A. Geofisica marina
    Description: JCR Journal
    Keywords: Shipping noise ; Ionian Sea ; AIS ; EU marine strategy ; EMSO-ERIC ; Deep-sea cabled observatory
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 10
    Publication Date: 2021-05-12
    Description: Research Infrastructures (RIs) are large-scale facilities encompassing instruments, resources, data and services used by the scientific community to conduct high-level research in their respective fields. The development and integration of marine environmental RIs as European Research Vessel Operators [ERVO] (2020) is the response of the European Commission (EC) to global marine challenges through research, technological development and innovation. These infrastructures (EMSO ERIC, Euro-Argo ERIC, ICOS-ERIC Marine, LifeWatch ERIC, and EMBRC-ERIC) include specialized vessels, fixed-point monitoring systems, Lagrangian floats, test facilities, genomics observatories, bio-sensing, and Virtual Research Environments (VREs), among others. Marine ecosystems are vital for life on Earth. Global climate change is progressing rapidly, and geo-hazards, such as earthquakes, volcanic eruptions, and tsunamis, cause large losses of human life and have massive worldwide socio-economic impacts. Enhancing our marine environmental monitoring and prediction capabilities will increase our ability to respond adequately to major challenges and efficiently. Collaboration among European marine RIs aligns with and has contributed to the OceanObs’19 Conference statement and the objectives of the UN Decade of Ocean Science for Sustainable Development (2021–2030). This collaboration actively participates and supports concrete actions to increase the quality and quantity of more integrated and sustained observations in the ocean worldwide. From an innovation perspective, the next decade will increasingly count on marine RIs to support the development of new technologies and their validation in the field, increasing market uptake and produce a shift in observing capabilities and strategies.
    Description: Published
    Description: 180
    Description: 3A. Geofisica marina e osservazioni multiparametriche a fondo mare
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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