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  • 1
    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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  • 2
    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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  • 3
    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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  • 4
    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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  • 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: 2021-01-15
    Description: Laser reflectometry (BOTDR), commonly used for structural health monitoring (bridges, dams, etc.), for the first time is being tested to study movements of an active fault on the seafloor, 25 km offshore Catania Sicily (an urban area of 1 million people). Under ideal conditions, this technique can measure small strains (10E-6), across very large distances (10 - 200 km) and locate these strains with a spatial resolution of 10 - 50 m. As the first experiment of the European funded FOCUS project (ERC Advanced Grant), in late April 2020 we aimed to connect and deploy a dedicated 6-km long strain cable to the TSS (Test Site South) seafloor observatory in 2100 m water depth operated by INFN-LNS (Italian National Physics Institute). The work plan for the marine expedition FocusX1 onboard the research vessel PourquoiPas? is described here. First, microbathymetric mapping and a video camera survey are performed by the ROV Victor6000. Then, several intermediate junction frames and short connector cables (umbilicals) are connected. A cable-end module and 6-km long fiber-optic strain cable (manufactured by Nexans Norway) is then connected to the new junction box. Next, we use a deep-water cable-laying system with an integrated plow (updated Deep Sea Net design Ifremer, Toulon) to bury the cable 20 cm in the soft sediments in order to increase coupling between the cable and the seafloor. The targeted track for the cable crosses the North Alfeo Fault at three locations. Laser reflectometry measurements began April 2020 and will be calibrated by a three-year deployment of seafloor geodetic instruments (Canopus acoustic beacons manufactured by iXblue) also started April 2020, to quantify relative displacement across the fault. During a future marine expedition, tentatively scheduled for 2021 (FocusX2) a passive seismological experiment is planned to record regional seismicity. This will involve deployment of a temporary network of OBS (Ocean Bottom Seismometers) on the seafloor and seismic stations on land, supplemented by INGV permanent land stations. The simultaneous use of laser reflectometry, seafloor geodetic stations as well as seismological land and sea stations will provide an integrated system for monitoring a wide range of types of slipping events along the North Alfeo Fault (e.g. - creep, slow-slip, rupture). A long-term goal is the development of dual-use telecom cables with industry partners.
    Type: Conference or Workshop Item , NonPeerReviewed
    Format: text
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  • 7
    Publication Date: 2019-09-23
    Description: Laser reflectometry (BOTDR), commonly used for structural health monitoring (bridges, dams, etc.), will for the first time be applied to study movements of an active fault on the seafloor 25 km offshore Catania Sicily. The goal of the European funded FOCUS project (ERC Advanced Grant) is to connect a 6-km long strain cable to the EMSO seafloor observatory in 2100 m water depth. Laser observations will be calibrated by seafloor geodetic instruments and seismological stations. A long-term goal is the development of dual-use telecom cables with industry partners.
    Type: Article , NonPeerReviewed
    Format: text
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  • 8
    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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  • 9
    Publication Date: 2023-02-24
    Keywords: DATE/TIME; DEPTH, water; EGIM; EGIM_1:OBSEA:2016-12-01; EMSODEV; EMSO Generic Instrument Module; EMSO implementation and operation: DEVelopment of instrument module; OBSEA; OBSEA_EGIM_2017; OBSEA cabled observatory; OBSEA underwater observatory site; Turbidity (Nephelometric turbidity unit); Turbidity meter, WET Labs ECO NTURTD, SN 689
    Type: Dataset
    Format: text/tab-separated-values, 2425292 data points
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  • 10
    Publication Date: 2023-02-24
    Keywords: Conductivity; CTD, SEA-BIRD SBE 37-SIP, P7000-RS232; DATE/TIME; DEPTH, water; EGIM; EGIM_1:OBSEA:2016-12-01; EMSODEV; EMSO Generic Instrument Module; EMSO implementation and operation: DEVelopment of instrument module; OBSEA; OBSEA_EGIM_2017; OBSEA cabled observatory; OBSEA underwater observatory site; Salinity; Sound velocity in water; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 803364 data points
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