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  • 1
    Publication Date: 2024-03-14
    Keywords: Adriatic Sea; Aegean Sea; Alboran Sea; CTD; CTD, Seabird; CTD/Rosette; CTD-R; CTD-RO; Date/Time of event; DEPTH, water; Eastern Basin; Elevation of event; Event label; Ionian Sea; Latitude of event; Longitude of event; M287; M288; M289; M290; M291; M292; M293; M294; M295; M296; M297; M298; M299; M300; M301; M302; M303; M304; M305; M306; M307; M308; M309; M310; M311; M312; M313; M314; M315; M316; M317; M318; M319; M320; M321; M322; M323; M324; M325; M326; M327; M328; M329; M330; M331; M332; M333; M334; M335; M336; M337; M338; M339; M340; M341; M342; M343; M344; M345; M346; M347; M348; M84/3; M84/3_287; M84/3_288; M84/3_289; M84/3_290; M84/3_291; M84/3_292; M84/3_293; M84/3_294; M84/3_295; M84/3_296; M84/3_297; M84/3_298; M84/3_299; M84/3_300; M84/3_301; M84/3_302; M84/3_303; M84/3_304; M84/3_305; M84/3_306; M84/3_307; M84/3_308; M84/3_309; M84/3_310; M84/3_311; M84/3_312; M84/3_313; M84/3_314; M84/3_315; M84/3_316; M84/3_317; M84/3_318; M84/3_319; M84/3_320; M84/3_321; M84/3_322; M84/3_323; M84/3_324; M84/3_325; M84/3_326; M84/3_327; M84/3_328; M84/3_329; M84/3_330; M84/3_331; M84/3_332; M84/3_333; M84/3_334; M84/3_335; M84/3_336; M84/3_337; M84/3_338; M84/3_339; M84/3_340; M84/3_341; M84/3_342; M84/3_343; M84/3_344; M84/3_345; M84/3_346; M84/3_347; M84/3_348; Meteor (1986); Oxygen; Pressure, water; Salinity; South Atlantic Ocean; Strait of Gibraltar; Temperature, water; Tirreno Sea; Western Basin
    Type: Dataset
    Format: text/tab-separated-values, 524455 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-03-14
    Keywords: Adriatic Sea; Aegean Sea; Alboran Sea; Alkalinity, total; Barium; Barium, standard deviation; Bottle number; Carbon, total; CTD; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Eastern Basin; Elevation of event; Event label; Freon-12 (dichlorodifluoromethane); Helium; Identification; Ionian Sea; Latitude of event; Longitude of event; M287; M288; M289; M290; M291; M292; M293; M294; M295; M296; M297; M298; M299; M300; M301; M302; M303; M304; M305; M306; M307; M308; M309; M310; M311; M312; M313; M314; M315; M316; M317; M318; M319; M320; M321; M322; M323; M324; M325; M326; M327; M328; M329; M330; M331; M332; M333; M334; M335; M336; M337; M338; M339; M340; M342; M344; M84/3; M84/3_287; M84/3_288; M84/3_289; M84/3_290; M84/3_291; M84/3_292; M84/3_293; M84/3_294; M84/3_295; M84/3_296; M84/3_297; M84/3_298; M84/3_299; M84/3_300; M84/3_301; M84/3_302; M84/3_303; M84/3_304; M84/3_305; M84/3_306; M84/3_307; M84/3_308; M84/3_309; M84/3_310; M84/3_311; M84/3_312; M84/3_313; M84/3_314; M84/3_315; M84/3_316; M84/3_317; M84/3_318; M84/3_319; M84/3_320; M84/3_321; M84/3_322; M84/3_323; M84/3_324; M84/3_325; M84/3_326; M84/3_327; M84/3_328; M84/3_329; M84/3_330; M84/3_331; M84/3_332; M84/3_333; M84/3_334; M84/3_335; M84/3_336; M84/3_337; M84/3_338; M84/3_339; M84/3_340; M84/3_342; M84/3_344; Meteor (1986); Neon; Nitrate; Nitrite; Oxygen; pH; Phosphate; Pressure, water; Quality flag; Salinity; Silicate; South Atlantic Ocean; Strait of Gibraltar; Sulfur hexafluoride, SF6; Temperature, technical; Temperature, water; Temperature, water, potential; Tirreno Sea; Tritium; Tritium, standard deviation; Western Basin; WOCE quality flag; δ13C; δ14C; δ14C, standard deviation; δ Helium-3; δ Helium-3, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 45912 data points
    Location Call Number Limitation Availability
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  • 3
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    PANGAEA
    In:  Supplement to: Tanhua, Toste; Hainbucher, Dagmar; Cardin, Vanessa; Álvarez, Marta; Civitarese, Giuseppe; McNichol, Ann P; Key, Robert M (2013): Repeat hydrography in the Mediterranean Sea, data from the Meteor cruise 84/3 in 2011. Earth System Science Data, 5(2), 289-294, https://doi.org/10.5194/essd-5-289-2013
    Publication Date: 2024-03-14
    Description: Here we report on data from an oceanographic cruise on the German research vessel Meteor covering large parts of the Mediterranean Sea during spring of 2011. The main objective of this cruise was to conduct measurements of physical, chemical and biological variables on a section across the Mediterranean Sea with the goal of producing a synoptic picture of the distribution of relevant physical and biogeochemical properties, in order to compare those to historic data sets. During the cruise, a comprehensive data set of relevant variables following the guide lines for repeat hydrography outlined by the GO-SHIP group (http://www.go-ship.org/) was collected. The measurements include salinity and temperature (CTD), an over-determined carbonate system, inorganic nutrients, oxygen, transient tracers (CFC-12, SF6), helium isotopes and tritium, and carbon isotopes. The cruise sampled all major basins of the Mediterranean Sea following roughly an east-to-west section from the coast of Lebanon through to the Strait of Gibraltar, and to the coast of Portugal. Also a south-to-north section from the Ionian Sea to the Adriatic Sea was carried out. Additionally, sampling in the Aegean, Adriatic and Tyrrhenian Seas were carried out. The sections roughly followed lines and positions that have been sampled previously during other programs, thus providing the opportunity for comparative investigations of the temporal development of various parameters.
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2024-04-19
    Keywords: CTD; CTD, underway; CTD/Rosette; CTD-RO; CTD-UW; DATE/TIME; DEPTH, water; Event label; LATITUDE; LONGITUDE; Maria S. Merian; MSM72; MSM72_100-1; MSM72_10-1; MSM72_101-1; MSM72_102-1; MSM72_103-1; MSM72_104-1; MSM72_105-1; MSM72_106-1; MSM72_107-1; MSM72_108-1; MSM72_109-1; MSM72_1-1; MSM72_110-1; MSM72_11-1; MSM72_111-1; MSM72_11-2; MSM72_112-1; MSM72_113-2; MSM72_114-1; MSM72_115-1; MSM72_116-1; MSM72_117-1; MSM72_118-1; MSM72_119-1; MSM72_120-1; MSM72_12-1; MSM72_121-1; MSM72_122-1; MSM72_123-1; MSM72_124-1; MSM72_125-1; MSM72_126-1; MSM72_127-1; MSM72_128-1; MSM72_129-1; MSM72_130-2; MSM72_13-1; MSM72_131-1; MSM72_132-1; MSM72_133-1; MSM72_134-1; MSM72_135-1; MSM72_136-1; MSM72_14-1; MSM72_15-1; MSM72_16-1; MSM72_17-1; MSM72_18-1; MSM72_19-1; MSM72_20-1; MSM72_2-1; MSM72_21-1; MSM72_22-1; MSM72_23-1; MSM72_24-1; MSM72_25-1; MSM72_26-1; MSM72_27-1; MSM72_28-1; MSM72_30-1; MSM72_3-1; MSM72_31-1; MSM72_32-1; MSM72_33-1; MSM72_34-1; MSM72_35-1; MSM72_36-1; MSM72_37-1; MSM72_38-1; MSM72_39-1; MSM72_40-1; MSM72_4-1; MSM72_41-1; MSM72_42-1; MSM72_43-1; MSM72_44-1; MSM72_45-1; MSM72_46-1; MSM72_47-2; MSM72_48-1; MSM72_49-1; MSM72_50-1; MSM72_5-1; MSM72_51-1; MSM72_52-1; MSM72_53-1; MSM72_54-1; MSM72_55-1; MSM72_56-1; MSM72_57-1; MSM72_58-1; MSM72_59-1; MSM72_60-1; MSM72_6-1; MSM72_61-1; MSM72_62-1; MSM72_63-1; MSM72_64-1; MSM72_65-1; MSM72_66-1; MSM72_67-1; MSM72_68-1; MSM72_69-1; MSM72_70-1; MSM72_7-1; MSM72_71-1; MSM72_72-1; MSM72_73-1; MSM72_74-1; MSM72_75-1; MSM72_75-2; MSM72_76-1; MSM72_77-2; MSM72_79-1; MSM72_80-1; MSM72_8-1; MSM72_81-1; MSM72_82-1; MSM72_83-1; MSM72_83-2; MSM72_84-1; MSM72_85-1; MSM72_86-1; MSM72_87-1; MSM72_88-1; MSM72_89-1; MSM72_90-1; MSM72_9-1; MSM72_91-2; MSM72_92-1; MSM72_93-1; MSM72_94-1; MSM72_95-1; MSM72_96-1; MSM72_97-2; MSM72_98-1; MSM72_99-1; Oxygen; Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 1168516 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2020-07-23
    Description: This study presents aspects of the spatial and temporal variability of abyssal water masses in the Ionian Sea, as derived from recent temperature, salinity, dissolved oxygen and velocity observations and from comparisons between these and former observations. Previous studies showed how in the Southern Adriatic Sea the Adriatic Deep Water (AdDW) became fresher (ΔS ≈ −0.08) and colder (ΔT ≈ −0.1°C) after experiencing warming and salinification between 2003 and 2007. Our data, collected from October 2009 to July 2010 from two bottom moorings, one within the Strait of Otranto and the other in the northern Ionian, confirm this tendency: a bottom vein of southward-flowing AdDW, whose temperature and salinity continuously decreased during the observation time, was detected there. Typically, the vein travel time between the two stations ranged between 45 and 50 days. This gave us a temporal estimate for AdDW anomaly propagation towards the Ionian abyss from their Adriatic generation region. The density excess of the observed vein was always enough to enable its existence as a bottom-arrested current. This evidence confirms that, at that time (2009 and 2010), the Adriatic Sea was greatly contributing to the formation of Eastern Mediterranean Deep Water (EMDW), the bottom water of the Eastern Mediterranean. Hence, based on these results and on the evidence that, from 2003 to 2009, abyssal Ionian waters became saltier and warmer under the time-lagged influence of AdDW, possible future changes in the EMDW characteristics, as a response to Adriatic variability, are discussed.
    Type: Article , PeerReviewed
    Format: text
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  • 6
    Publication Date: 2023-02-08
    Description: The last few decades have seen dramatic changes in the hydrography and biogeochemistry of the Mediterranean Sea. The complex bathymetry and highly variable spatial and temporal scales of atmospheric forcing, convective and ventilation processes contribute to generate complex and unsteady circulation patterns and significant variability in biogeochemical systems. Part of the variability of this system can be influenced by anthropogenic contributions. Consequently, it is necessary to document details and to understand trends in place to better relate the observed processes and to possibly predict the consequences of these changes. In this context we report data from an oceanographic cruise in the Mediterranean Sea on the German research vessel Maria S. Merian (MSM72) in March 2018. The main objective of the cruise was to contribute to the understanding of long-term changes and trends in physical and biogeochemical parameters, such as the anthropogenic carbon uptake and to further assess the hydrographical situation after the major climatological shifts in the eastern and western part of the basin, known as the Eastern and Western Mediterranean Transients. During the cruise, multidisciplinary measurements were conducted on a predominantly zonal section throughout the Mediterranean Sea, contributing to the Med-SHIP and GO-SHIP long-term repeat cruise section that is conducted at regular intervals in the Mediterranean Sea to observe changes and impacts on physical and biogeochemical variables.
    Type: Article , PeerReviewed
    Format: text
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  • 7
    Publication Date: 2022-01-31
    Description: The Mediterranean community represented in this paper is the result of more than 30 years of EU and nationally funded coordination, which has led to key contributions in science concepts and operational initiatives. Together with the establishment of operational services, the community has coordinated with universities, research centers, research infrastructures and private companies to implement advanced multi-platform and integrated observing and forecasting systems that facilitate the advancement of operational services, scientific achievements and mission-oriented innovation. Thus, the community can respond to societal challenges and stakeholders needs, developing a variety of fit-for-purpose services such as the Copernicus Marine Service. The combination of state-of-the-art observations and forecasting provides new opportunities for downstream services in response to the needs of the heavily populated Mediterranean coastal areas and to climate change. The challenge over the next decade is to sustain ocean observations within the research community, to monitor the variability at small scales, e.g., the mesoscale/submesoscale, to resolve the sub-basin/seasonal and inter-annual variability in the circulation, and thus establish the decadal variability, understand and correct the model-associated biases and to enhance model-data integration and ensemble forecasting for uncertainty estimation. Better knowledge and understanding of the level of Mediterranean variability will enable a subsequent evaluation of the impacts and mitigation of the effect of human activities and climate change on the biodiversity and the ecosystem, which will support environmental assessments and decisions. Further challenges include extending the science-based added-value products into societal relevant downstream services and engaging with communities to build initiatives that will contribute to the 2030 Agenda and more specifically to SDG14 and the UN's Decade of Ocean Science for sustainable development, by this contributing to bridge the science-policy gap. The Mediterranean observing and forecasting capacity was built on the basis of community best practices in monitoring and modeling, and can serve as a basis for the development of an integrated global ocean observing system.
    Type: Article , PeerReviewed
    Format: text
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  • 8
    Publication Date: 2022-01-31
    Description: The oceans play a key role in global issues such as climate change, food security, and human health. Given their vast dimensions and internal complexity, efficient monitoring and predicting of the planet’s ocean must be a collaborative effort of both regional and global scale. A first and foremost requirement for such collaborative ocean observing is the need to follow well-defined and reproducible methods across activities: from strategies for structuring observing systems, sensor deployment and usage, and the generation of data and information products, to ethical and governance aspects when executing ocean observing. To meet the urgent, planet-wide challenges we face, methods across all aspects of ocean observing should be broadly adopted by the ocean community and, where appropriate, should evolve into “Ocean Best Practices.” While many groups have created best practices, they are scattered across the Web or buried in local repositories and many have yet to be digitized. To reduce this fragmentation, we introduce a new open access, permanent, digital repository of best practices documentation (oceanbestpractices.org) that is part of the Ocean Best Practices System (OBPS). The new OBPS provides an opportunity space for the centralized and coordinated improvement of ocean observing methods. The OBPS repository employs user-friendly software to significantly improve discovery and access to methods. The software includes advanced semantic technologies for search capabilities to enhance repository operations. In addition to the repository, the OBPS also includes a peer reviewed journal research topic, a forum for community discussion and a training activity for use of best practices. Together, these components serve to realize a core objective of the OBPS, which is to enable the ocean community to create superior methods for every activity in ocean observing from research to operations to applications that are agreed upon and broadly adopted across communities. Using selected ocean observing examples, we show how the OBPS supports this objective. This paper lays out a future vision of ocean best practices and how OBPS will contribute to improving ocean observing in the decade to come.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
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  • 9
    Publication Date: 2022-01-31
    Description: The European Research Infrastructure Consortium “Integrated Carbon Observation System” (ICOS) aims at delivering high quality greenhouse gas (GHG) observations and derived data products (e.g., regional GHG-flux maps) for constraining the GHG balance on a European level, on a sustained long-term basis. The marine domain (ICOS-Oceans) currently consists of 11 Ship of Opportunity lines (SOOP – Ship of Opportunity Program) and 10 Fixed Ocean Stations (FOSs) spread across European waters, including the North Atlantic and Arctic Oceans and the Barents, North, Baltic, and Mediterranean Seas. The stations operate in a harmonized and standardized way based on community-proven protocols and methods for ocean GHG observations, improving operational conformity as well as quality control and assurance of the data. This enables the network to focus on long term research into the marine carbon cycle and the anthropogenic carbon sink, while preparing the network to include other GHG fluxes. ICOS data are processed on a near real-time basis and will be published on the ICOS Carbon Portal (CP), allowing monthly estimates of CO2 air-sea exchange to be quantified for European waters. ICOS establishes transparent operational data management routines following the FAIR (Findable, Accessible, Interoperable, and Reusable) guiding principles allowing amongst others reproducibility, interoperability, and traceability. The ICOS-Oceans network is actively integrating with the atmospheric (e.g., improved atmospheric measurements onboard SOOP lines) and ecosystem (e.g., oceanic direct gas flux measurements) domains of ICOS, and utilizes techniques developed by the ICOS Central Facilities and the CP. There is a strong interaction with the international ocean carbon cycle community to enhance interoperability and harmonize data flow. The future vision of ICOS-Oceans includes ship-based ocean survey sections to obtain a three-dimensional understanding of marine carbon cycle processes and optimize the existing network design.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
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  • 10
    Publication Date: 2024-01-30
    Description: The Mediterranean Sea has been sampled irregularly by research vessels in the past, mostly by national expeditions in regional waters. To monitor the hydrographic, biogeochemical and circulation changes in the Mediterranean Sea, a systematic repeat oceanographic survey programme called Med-SHIP was recommended by the Mediterranean Science Commission (CIESM) in 2011, as part of the Global Ocean Ship-based Hydrographic Investigations Program (GO-SHIP). Med-SHIP consists of zonal and meridional surveys with different frequencies, where comprehensive physical and biogeochemical properties are measured with the highest international standards. The first zonal survey was done in 2011 and repeated in 2018. In addition, a network of meridional (and other key) hydrographic sections were designed: the first cycle of these sections was completed in 2016, with three cruises funded by the EU project EUROFLEETS2. This paper presents the physical and chemical data of the meridional and key transects in the Western and Eastern Mediterranean Sea collected during those cruises.
    Type: Article , PeerReviewed
    Format: text
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