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  • PAGEPress Publications  (3)
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  • PAGEPress Publications  (3)
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  • 1
    Online Resource
    Online Resource
    PAGEPress Publications ; 2012
    In:  Advances in Oceanography and Limnology Vol. 3, No. 1 ( 2012-06-01), p. 41-
    In: Advances in Oceanography and Limnology, PAGEPress Publications, Vol. 3, No. 1 ( 2012-06-01), p. 41-
    Abstract: In order to monitor, describe and understand the marine environment, many research institutions are involved in the acquisition and distribution of ocean data, both from observations and models. Scientists from these institutions are spending too much time looking for, accessing, and reformatting data: they need better tools and procedures to make the science they do more efficient. The U.S. Integrated Ocean Observing System (US-IOOS) is working on making large amounts of distributed data usable in an easy and efficient way. It is essentially a network of scientists, technicians and technologies designed to acquire, collect and disseminate observational and modelled data resulting from coastal and oceanic marine regions investigations to researchers, stakeholders and policy makers. In order to be successful, this effort requires standard data protocols, web services and standards-based tools. Starting from the US-IOOS approach, which is being adopted throughout much of the oceanographic and meteorological sectors, we describe here the CNR-ISMAR Venice experience in the direction of setting up a national Italian IOOS framework using the THREDDS (THematic Real-time Environmental Distributed Data Services) Data Server (TDS), a middleware designed to fill the gap between data providers and data users. The TDS provides services that allow data users to find the data sets pertaining to their scientific needs, to access, to visualize and to use them in an easy way, without downloading files to the local workspace. In order to achieve this, it is necessary that the data providers make their data available in a standard form that the TDS understands, and with sufficient metadata to allow the data to be read and searched in a standard way. The core idea is then to utilize a Common Data Model (CDM), a unified conceptual model that describes different datatypes within each dataset. More specifically, Unidata ( 〈 a href="http://www.unidata.ucar.edu" target="_blank" 〉 www.unidata.ucar.edu 〈 /a 〉 ) has developed CDM specifications for many of the different kinds of data used by the scientific community, such as grids, profiles, time series, swath data. These datatypes are aligned the NetCDF Climate and Forecast (CF) Metadata Conventions and with Climate Science Modelling Language (CSML); CF-compliant NetCDF files and GRIB files can be read directly with no modification, while non compliant files can be modified to meet appropriate metadata requirements. Once standardized in the CDM, the TDS makes datasets available through a series of web services such as OPeNDAP or Open Geospatial Consortium Web Coverage Service (WCS), allowing the data users to easily obtain small subsets from large datasets, and to quickly visualize their content by using tools such as GODIVA2 or Integrated Data Viewer (IDV). In addition, an ISO metadata service is available through the TDS that can be harvested by catalogue broker services (e.g. GI-cat) to enable distributed search across federated data servers. Example of TDS datasets can be accessed at the CNR-ISMAR Venice site 〈 a href="http://tds.ve.ismar.cnr.it:8080/thredds/catalog.html" target="_blank" 〉 http://tds.ve.ismar.cnr.it:8080/thredds/catalog.html 〈 /a 〉 .
    Type of Medium: Online Resource
    ISSN: 1947-573X , 1947-5721
    Language: Unknown
    Publisher: PAGEPress Publications
    Publication Date: 2012
    detail.hit.zdb_id: 2556332-4
    Library Location Call Number Volume/Issue/Year Availability
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  • 2
    Online Resource
    Online Resource
    PAGEPress Publications ; 2011
    In:  Advances in Oceanography and Limnology Vol. 2, No. 1 ( 2011-06-17), p. 55-
    In: Advances in Oceanography and Limnology, PAGEPress Publications, Vol. 2, No. 1 ( 2011-06-17), p. 55-
    Abstract: The World Ocean Database 2001 data located in the Ross Sea (named WOD01 and containing data in this region since 1928) are merged with recent data collected by the Italian expeditions (CLIMA dataset) in the period November 1994-February 2004 in the same area. From this extended dataset, austral summer climatologies of the main Ross Sea subsurface, intermediate and bottom water masses: High Salinity Shelf Water (HSSW), Low Salinity Shelf Water (LSSW), Ice Shelf Water (ISW) and Modified Circumpolar Deep Water (MCDW) have been drawn. The comparison between the WOD01_1994 climatologies (a subset of the WOD01 dataset until April 1994) and the CLIMA ones for the period 1994/95-2003/04 showed significant changes occurred during the decade. The freshening of the Ross Sea shelf waters which occurred during the period 1960-2000, was confirmed by our analysis in all the main water masses, even though with a spatially varying intensity. Relevant variations were found for the MCDW masses, which appeared to reduce their presence and to deepen; this can be ascribed to the very limited freshening of the MCDW core, which allowed an increased density with respect to the surrounding waters. Variations in the MCDW properties and extension could have relevant consequences, e.g. a decreased Ross Ice Shelf basal melting or a reduced supply of nutrients, and may also be indicative of a reduced thermohaline circulation within the Ross Sea. Shelf Waters (SW) having neutral density γn & gt; 28.7 Kg m-3, which contribute to form the densest Antarctic Bottom Waters (AABW), showed a large volumetric decrease in the 1994/95-2003/04 decade, most likely as a consequence of the SW freshening.
    Type of Medium: Online Resource
    ISSN: 1947-573X , 1947-5721
    Language: Unknown
    Publisher: PAGEPress Publications
    Publication Date: 2011
    detail.hit.zdb_id: 2556332-4
    Library Location Call Number Volume/Issue/Year Availability
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  • 3
    Online Resource
    Online Resource
    PAGEPress Publications ; 2010
    In:  Advances in Oceanography and Limnology Vol. 1, No. 1 ( 2010-06-01), p. 11-
    In: Advances in Oceanography and Limnology, PAGEPress Publications, Vol. 1, No. 1 ( 2010-06-01), p. 11-
    Abstract: The Mediterranean Sea is an enclosed basin composed of two similar basins and different sub-basins. It is a concentration basin, where evaporation exceeds precipitation. In the surface layer there is an inflow of Atlantic water which is modified along its path to the Eastern basin. This transformation occurs through surface heat loss and evaporation specifically in the Levantine basin. The Mediterranean is furthermore the site of water mass formation processes, which can be studied experimentally because of their easy accessibility. There are two main reasons why the Mediterranean is important. The first one is the impact of the Mediterranean on the global thermohaline circulation, the second reason is that the Mediterranean basin can be considered as Laborartory for investigating processes occurring on the global scale of the world ocean. In this paper we want to provide a short historical review of the evolving knowledge of the Mediterranean circulation that has emerged from experimental investigations over the last decades. We start by describing the old picture of the basin circulation which had stationary, smooth large scale patterns. Then we show the major experiments that led to the discovery of the sub-basin scale circulation and its mesoscale features. We conclude with the dynamical discovery of EMT in the 1990s and the most exciting ongoing new research programmes.
    Type of Medium: Online Resource
    ISSN: 1947-573X , 1947-5721
    Language: Unknown
    Publisher: PAGEPress Publications
    Publication Date: 2010
    detail.hit.zdb_id: 2556332-4
    Library Location Call Number Volume/Issue/Year Availability
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