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  • 1
    Online Resource
    Online Resource
    San Diego :Elsevier,
    Keywords: Oceanography. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (586 pages)
    Edition: 1st ed.
    ISBN: 9780128236932
    DDC: 551.46
    Language: English
    Note: Front Cover -- Oceanography of the Mediterranean Sea -- Oceanography of the Mediterranean SeaAn Introductory GuideEdited byKatrin SchroederConsiglio Nazionale delle Ricerche-Istit ... -- Contents -- List of contributors -- About the editors -- 1 - Introduction -- 1.1 The Mediterranean Sea, a "miniature ocean" -- 1.2 Book structure and contents -- 1.3 Learning objectives at a glance -- References -- 2 - Mediterranean Sea evolution and present-day physiography -- 2.1 Origin of the Mediterranean Sea -- 2.1.1 Kinematic and geodynamical overview -- 2.1.2 Messinian salinity crisis: an extraordinary event -- 2.2 Dimensions and seafloor topography -- 2.3 Sedimentation on continental margins -- 2.3.1 Tectonic movements and sedimentation -- 2.3.2 Climate and sedimentation -- 2.4 Concluding remarks -- References -- 3 - Mediterranean climate: past, present and future -- 3.1 General climate and morphological characteristics of the Mediterranean basin -- 3.2 Instrumental observations, satellites, and reanalyses -- 3.3 Climate models and their evolution -- 3.3.1 Components of climate models and model hierarchy -- 3.3.2 Climate modeling international programs -- 3.4 Heat and moisture balance at Mediterranean regional scale and relation to surface climate -- 3.4.1 Heat budget -- 3.4.2 Moisture budget -- 3.5 The atmospheric circulation of the subtropics and mid-latitudes -- 3.5.1 The Mediterranean basin as a transitional region -- 3.5.2 The Mediterranean storm track -- 3.5.3 Remote factors affecting the Mediterranean climate -- 3.6 Evolution of Mediterranean climate -- 3.6.1 Astronomical forcing -- 3.6.2 The formation of the Mediterranean and geophysical forcing of Mediterranean climate -- 3.6.3 The last million years: the glacial cycles -- 3.6.4 The last millennia: the historical period -- 3.6.5 Anthropogenic climate change -- References. , 4 - The forcings of the Mediterranean Sea and the physical properties of its water masses -- 4.1 The forcings of the Mediterranean Sea -- 4.1.1 Exchanges through the strait of Gibraltar -- 4.1.2 Climatological mean surface flux fields -- 4.1.2.1 Wind stress -- 4.1.2.2 Heat flux -- 4.1.2.3 Freshwater flux -- 4.1.3 Temporal variability -- 4.2 The thermohaline properties of the Mediterranean water masses -- 4.2.1 Water masses, water types, and their representation -- 4.2.2 Water mass analysis and the interpretation of the TS diagram -- 4.2.3 Water mass properties and distribution in the Mediterranean Sea -- 4.2.3.1 Atlantic water -- 4.2.3.2 Intermediate water -- 4.2.3.3 Deep water -- 4.3 Other water mass tracers -- References -- 5 - Mediterranean Sea level -- 5.1 General concepts about sea level -- 5.2 Techniques for measuring sea level -- 5.2.1 Tide gauges -- 5.2.2 Satellite altimetry -- 5.2.3 Sea level proxies -- 5.2.4 Supplementary techniques for understanding sea level changes -- 5.3 Past evolution of Mediterranean Sea level -- 5.3.1 Holocene sea-level changes and the role of isostatic-related subsidence -- 5.3.2 Decadal to centennial sea level trends since the late 19th century -- 5.4 Future projections of Mediterranean Sea level -- References -- 6 - Surface wave and sea surface dynamics in the Mediterranean -- 6.1 General concepts about waves, definitions and phenomenology -- 6.2 Tides and seiches -- 6.2.1 Generalities and basic definitions -- 6.2.2 Tides in the Mediterranean Sea -- 6.3 Marine storms and coastal floods in the Mediterranean Sea -- 6.3.1 Storm surges -- 6.3.2 Planetary scale forcing of storm surges -- 6.3.3 Synoptic scale forcing of storm surges -- 6.3.4 Mesoscale forcing of storm surges -- 6.3.5 Prediction of storm surges -- 6.3.6 Coastal floods in future climates -- 6.4 Wind generated waves. , 6.4.1 Generalities and basic definitions -- 6.4.2 Wind and waves regimes in the Mediterranean Sea -- 6.4.3 Waves forecasts in the Mediterranean Sea -- 6.4.4 Past and future evolution of wind-generated waves -- 6.5 Tsunamis -- 6.5.1 Historical events in the Mediterranean Sea -- 6.5.2 Source, propagation and tsunami models -- 6.5.3 Meteotsunamis -- 6.5.4 Early warning systems -- References -- 7 - Dense and deep water formation processes and Mediterranean overturning circulation -- 7.1 General concepts -- 7.2 Dense/deep water characteristics and formation rates -- 7.3 Observations of deep/dense water formation in the Mediterranean Sea -- 7.3.1 Convection and deep water formation in the Gulf of Lion: five decades of observations -- 7.3.2 Deep water formation in the eastern Mediterranean -- 7.3.2.1 The Adriatic Sea as a main contributor to Eastern Mediterranean deep waters -- 7.3.2.2 The Aegean Sea as an intermittent deep water source to the eastern Mediterranean -- 7.3.3 Formation of intermediate water masses -- 7.3.3.1 Levantine intermediate water -- 7.3.3.2 Cretan intermediate water -- 7.3.3.3 Western intermediate water -- 7.3.3.4 Tyrrhenian intermediate water -- 7.3.4 Dense shelf water formation and cascading -- 7.3.4.1 Gulf of Lion -- 7.3.4.2 Adriatic Sea -- 7.4 Theory of dense/deep water formation processes: general concepts -- 7.4.1 Theory of dense/deep water formation in the open ocean -- 7.4.2 Dense water formation on the shelf and their cascading into the deep ocean -- 7.5 Numerical modeling of deep/dense water formation -- 7.5.1 Dense/deep water formation numerical modeling in the open ocean -- 7.5.2 Dense/deep water cascading numerical modeling -- 7.6 The Mediterranean overturning circulation: structure and dynamics -- 7.6.1 Zonal overturning -- 7.6.2 Western Mediterranean overturning -- 7.6.3 Eastern Mediterranean overturning. , 7.6.4 Comparison of the Mediterranean with the North Atlantic overturning -- 7.7 Concluding remarks -- References -- 8 - Fronts, eddies and mesoscale circulation in the Mediterranean Sea -- 8.1 General concepts -- 8.2 Mediterranean Sea mesoscale variability derived from satellite altimetry -- 8.2.1 Mediterranean sea field dependency on the satellite constellation -- 8.2.2 Quantifying spatial and temporal variability -- 8.3 Eddies, fronts and vertical velocity -- 8.3.1 Vertical velocity and fronts in the Mediterranean Sea -- 8.3.2 Eddy detection, tracking and characterisation -- 8.4 Future perspectives -- References -- 9 - Recent changes in the Mediterranean Sea -- 9.1 General concepts about Mediterranean water masses and their circulation -- 9.2 Changes observed in the Eastern Mediterranean water masses -- 9.2.1 Formation of dense waters and the Eastern Mediterranean Transient (EMT) -- 9.2.2 Decadal oscillations of the upper thermohaline circulation in the EMED -- 9.2.3 Post-EMT status in the EMED -- 9.3 Changes observed in the Western Mediterranean water masses -- 9.3.1 The twentieth century: gradual warming and salinification -- 9.3.2 Changes during the 21st century: the Western Mediterranean Transition (WMT) -- 9.4 Long-term trends and climate change -- 9.5 Impact on the Mediterranean-Atlantic system -- 9.5.1 Mediterranean outflow water (MOW) -- 9.5.2 Following the MOW signal: from the strait of Gibraltar to the North Atlantic -- 9.5.3 MOW trends and variability -- References -- 10 - Mediterranean observing and forecasting systems -- 10.1 The emergence of operational oceanography in the Mediterranean Sea -- 10.2 The framework for ocean observing and the essential ocean variables -- 10.3 Observing systems operating in the Mediterranean Sea -- 10.3.1 Satellites. , 10.3.2 In-situ and land-based remote sensing observations: systems and international coordination programs -- 10.3.2.1 Research vessels -- 10.3.2.2 Moorings -- 10.3.2.3 Tide gauges and coastal stations -- 10.3.2.4 Drifters -- 10.3.2.5 Profiling floats -- 10.3.2.6 Gliders -- 10.3.2.7 HF radars -- 10.3.2.8 FerryBox -- 10.3.2.9 Animal tagging -- 10.3.2.10 EuroGOOS and MONGOOS -- 10.3.3 Multi-platform regional and coastal observing systems -- 10.3.3.1 MOOSE -- 10.3.3.2 SOCIB -- 10.3.3.3 POSEIDON -- 10.3.3.4 Other sustained multi-platform observing systems and intensive surveys -- 10.4 Forecasting the Mediterranean Sea -- 10.4.1 General concepts -- 10.4.1.1 Hydrodynamics -- 10.4.1.2 Storm surges and meteotsunamis -- 10.4.1.3 Wind waves -- 10.4.1.4 Biogeochemistry -- 10.4.1.5 Data assimilation as a tool to integrate models and observations -- 10.4.1.6 Reaching coastal scales -- 10.4.1.7 Coupling hydrodynamics, wave, hydrology, and atmospheric components -- 10.4.2 Illustration of some of the Mediterranean regional ocean prediction systems -- 10.4.2.1 Copernicus marine environment monitoring service -- 10.4.2.2 SOCIB -- 10.4.2.3 Poseidon -- 10.4.2.4 Other prediction systems -- 10.5 Data management and distribution -- 10.6 Concluding remarks -- References -- 11 - Mediterranean Sea general biogeochemistry -- 11.1 Dissolved oxygen distribution and ventilation -- 11.1.1 Introduction -- 11.1.2 Measurements of oxygen and models contribution -- 11.1.3 Dissolved oxygen distribution in the Mediterranean Sea -- 11.1.4 Ventilation mechanisms -- 11.1.5 Long term trends: in situ observation and model contribution -- 11.2 Dissolved nutrients: forms, sources, distribution, and dynamics -- 11.2.1 Introduction -- 11.2.2 Nutrient forms and sources -- 11.2.3 Nutrients distribution -- 11.2.4 Impact of the circulation on nutrients and biological dynamics. , 11.2.5 Anomalous N:P ratio.
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  • 2
    Type of Medium: Book
    Pages: xxi, 561 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 9780128236925
    RVK:
    Language: English
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  • 3
    Publication Date: 2023-07-18
    Description: This data set contains station data of top-to-bottom oceanic current measurements performed with Lowered Acoustic Doppler Current Profilers (LADCP) during the Med-SHIP cruise TAlPro2022 (Chief Scientist: Katrin Schroeder; Toulone - La Spezia, RV Belgica, 17/05/2022 - 26/05/2016). The LADCP devices in use were a downward and an upward-looking ADCP of type Teledyne RDI Workhorse Monitor 300 kHz. Station data of zonal and meridional oceanic velocities are reported in [cm/s] on a 4 m vertical grid. The processing of the data has been done using the LDEO LADCP data processing software (Thurnherr et al., 2010).
    Keywords: Acoustic Doppler Current Profiling (ADCP), TRDI Workhorse Monitor, 300 kHz; Belgica; current meter; Current velocity, east-west; Current velocity, north-south; DATE/TIME; DEPTH, water; Event label; LADCP; LATITUDE; LONGITUDE; Lowered Acoustic Doppler Current Profiler; Mediterranean; MedSHIP; Med-SHIP; physical oceanography; Station label; TAlPro2022; TAlPro2022_1; TAlPro2022_10; TAlPro2022_11; TAlPro2022_12; TAlPro2022_13; TAlPro2022_14; TAlPro2022_15; TAlPro2022_16; TAlPro2022_17; TAlPro2022_18; TAlPro2022_19; TAlPro2022_2; TAlPro2022_20; TAlPro2022_3; TAlPro2022_4; TAlPro2022_5; TAlPro2022_6; TAlPro2022_7; TAlPro2022_8; TAlPro2022_9
    Type: Dataset
    Format: text/tab-separated-values, 27879 data points
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  • 4
    Publication Date: 2023-12-05
    Description: This data set contains station data of top-to-bottom oceanic current measurements performed with Lowered Acoustic Doppler Current Profilers (LADCP) during the MedSHIP cruise TAlPro2016 (Palermo - Barcelona, RV Angeles Alvariño, 18/-8/2016 - 29/08/2-16). The LADCP devices in use were a downward and an upward-looking ADCP of type Teledyne RDI Workhorse Monitor 300 kHz. Station data of zonal and meridional oceanic velocities are reported in [cm/s] on a 10 m vertical grid. The processing of the data has been done using the LDEO LADCP data processing software (https://www.go-ship.org/Manual/Thurnherr_LADCP.pdf)
    Keywords: 1; 10; 11; 12; 13; 14; 15; 16; 17; 18; 19; 2; 20; 21; 22; 23; 24; 25; 26; 27; 28; 29; 3; 30; 31; 32; 33; 34; 35; 36; 37; 38; 39; 4; 40; 41; 42; 5; 6; 7; 8; 9; Angeles Alvarino; CTD/Rosette; CTD-RO; current meter; Current velocity, east-west; Current velocity, north-south; Current velocity, vertical; DATE/TIME; DEPTH, water; EUROFLEET2; Event label; LADCP; LATITUDE; LONGITUDE; Lowered Acoustic Doppler Current Profiler (LADCP), 300 kHz; Mediterranean Sea; MedSHIP; New operational steps towards an alliance of European research fleets; physical oceanography; Station label; TAlPro-2016; TAlPro-2016_001; TAlPro-2016_002; TAlPro-2016_003; TAlPro-2016_004; TAlPro-2016_005; TAlPro-2016_006; TAlPro-2016_007; TAlPro-2016_008; TAlPro-2016_009; TAlPro-2016_010; TAlPro-2016_011; TAlPro-2016_012; TAlPro-2016_013; TAlPro-2016_014; TAlPro-2016_015; TAlPro-2016_016; TAlPro-2016_017; TAlPro-2016_018; TAlPro-2016_019; TAlPro-2016_020; TAlPro-2016_021; TAlPro-2016_022; TAlPro-2016_023; TAlPro-2016_024; TAlPro-2016_025; TAlPro-2016_026; TAlPro-2016_027; TAlPro-2016_028; TAlPro-2016_029; TAlPro-2016_030; TAlPro-2016_031; TAlPro-2016_032; TAlPro-2016_033; TAlPro-2016_034; TAlPro-2016_035; TAlPro-2016_036; TAlPro-2016_037; TAlPro-2016_038; TAlPro-2016_039; TAlPro-2016_040; TAlPro-2016_041; TAlPro-2016_042; Time in seconds
    Type: Dataset
    Format: text/tab-separated-values, 39705 data points
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  • 5
    Publication Date: 2024-02-27
    Description: In Summer 2015 (4-31 August), CNR-ISMAR carried out an oceanographic field-study in the Western Mediterranean Sea, on board of R/V MINERVA UNO. Sampling stations consisted in 7 transects, that spanned from Sicily Channel to Ligurian sea, Catalan sea, and Balearic Basin, dividing the area in sub-basins. 92 stations were visited totally. The dataset includes 550 discrete data of carbonate chemistry (pH-total scale and Total Alkalinity), concentrations of dissolved oxygen, and basic hydrological data (temperature, salinity and density). Methods: At each station, pressure (dbar), temperature (°C), and conductivity(mS/cm) were measured with a CTD SBE 911 plus General Oceanics Rosette System, equipped with 24 12-litres Niskin Bottles. Salinity (S, psu) and depth (m) were calculated by Sea-Bird Scientific routines. Seawater samples (n = 550) for the determination of biogeochemical parameters were collected from the Niskin bottles. Samples for dissolved oxygen (DO) were drawn in 60-mL BOD bottles and treated with Winkler reagents immediately after collection. For the determination of pH on the total hydrogen ion scale at 25 °C (pHT25), the samples were drawn after DO samples into 10 cm long cylindrical glass cells and analyzed spectrophotometrically. For the determination of total alkalinity (TA; μmol kg-1), the samples were collected in 300 ml borosilicate bottles, poisoned with mercuric chloride, tightly closed and stored in the dark at a temperature similar to the in situ one (4-25 °C). DO samples were analyzed by the Winkler method (Grasshoff et al., 1999) using an automated Metrohm 798 MPT Titrino potentiometric titration system (CV = 0.17 % at 210 µmol L-1). pHT25 was measured on board, within 24 h after the sampling, using the spectrophotometric method with m-cresol purple as indicator (Clayton and Byrne, 1993). The precision was ±0.002 units (n = 3), accuracy and stability of the method were checked daily with reference seawater certified for TA and TCO2 (n = 34, CRM batch 146 provided by Prof A. G. Dickson, Scripps, 210 California). TA was determined by potentiometric titration in an open cell with a difference derivative readout (Hernandez-Ayon et al., 1999). The average precision was ±2.0 μmol kg-1 (n = 86 duplicate samples) and the accuracy was checked daily by the titration of certified reference seawater (n = 59, CRM batch 146)
    Keywords: 108; 109; 110; 111; 213; 215; 217; 218; 219; 225; 227; 231; 261; 291; 405; 406; 433; 434; 438; 451; 460; 462; 51; 900; 901; 903; 906; 907; 908; 910; 911; 912; 913; Alkalinity, total; B1; B2; B3; B4; B5; B6; B7; B8; Balearic Basin; CORS-MOOR; CTD, Sea-Bird SBE 911plus; CTD/Rosette; CTD-RO; D1; D2; D3; D5; D7; DATE/TIME; DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; M9; MINERVA UNO; OC2015; OC2015_108; OC2015_109; OC2015_110; OC2015_111; OC2015_213; OC2015_215; OC2015_217; OC2015_218; OC2015_219; OC2015_225; OC2015_227; OC2015_231; OC2015_261; OC2015_291; OC2015_405; OC2015_406; OC2015_433; OC2015_434; OC2015_438; OC2015_451; OC2015_460; OC2015_462; OC2015_51; OC2015_900; OC2015_901; OC2015_903; OC2015_906; OC2015_907; OC2015_908; OC2015_910; OC2015_911; OC2015_912; OC2015_913; OC2015_B1; OC2015_B2; OC2015_B3; OC2015_B4; OC2015_B5; OC2015_B6; OC2015_B7; OC2015_B8; OC2015_CORS-MOOR; OC2015_D1; OC2015_D2; OC2015_D3; OC2015_D5; OC2015_D7; OC2015_M9; OC2015_S10; OC2015_S12; OC2015_S14; OC2015_S16; OC2015_S18; OC2015_S19; OC2015_S2; OC2015_S20; OC2015_S4; OC2015_S6; OC2015_S8; Ocean acidification; OCEAN-CERTAIN; Ocean Food-web Patrol – Climate Effects: Reducing Targeted Uncertainties with an Interactive Network; Oxygen; pH; Pressure, water; S10; S12; S14; S16; S18; S19; S2; S20; S4; S6; S8; Salinity; Sicily Channel; Spectrophotometry; Temperature, water; Titration, Winkler; Titration potentiometric; Total alkalinity; Western Mediterranean; Winkler oxygen
    Type: Dataset
    Format: text/tab-separated-values, 2921 data points
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  • 6
    Publication Date: 2024-04-20
    Description: This data set contains underway Temperature, Salinity and Fluorescence data collected by a Thermosalinograph (TSG) during the MedSHIP cruise TAlPro2016 (Palermo - Barcelona, RV Angeles Alvariño, 18/08/2016 - 29/08/2016). Underway data was collected along the cruise track with an autonomous TSG system, consisting of a SBE21 together with a SBE38 Thermometer. Both systems worked independent from each other throughout the cruise. While temperature is taken at the water inlet in about 5 m depth (SBE38, S/N 0437, last calibration on 11/07/2008), salinity is estimated within the interior TSG from conductivity and interior temperature (SBE21, S/N 3329, last calibration on 15/01/2016). A Turner fluorometer 10-Au-005 (S/N 7019 RTX, last calibration on 21/01/2016) is connected to the system.
    Keywords: Angeles Alvarino; Calculated from temperature and conductivity; Conductivity; DATE/TIME; DEPTH, water; Digital oceanographic thermometer, Sea-Bird, SBE 38; EUROFLEET2; FLU; Fluorescence; Fluorometer; LATITUDE; LONGITUDE; New operational steps towards an alliance of European research fleets; Salinity; Surface; TAlPro-2016; TAlPro-2016_TSG; Temperature; Temperature, water; Thermosalinograph (TSG), Sea-Bird, SBE 21 SEACAT; Time in seconds; TSG
    Type: Dataset
    Format: text/tab-separated-values, 460620 data points
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  • 7
    Publication Date: 2024-04-20
    Description: The western Mediterranean Sea climatology (BGC-WMED) presented here is a product derived from in situ observations, that included various data sources: in total, 2253 in-situ inorganic nutrient profiles over the period 1981-2017 have been used (Medar/MEDATLAS, Fichaut et al., 2003; the CNR-WMED biogeochemical dataset, Belgacem et al., 2019,2020; SeaDataNet data product, https://www.seadatanet.org; Mediterranean Ocean Observing System for the Environment, MOOSE, http://www.moose-network.fr/). This climatology provides an annual mean gridded nutrient fields for the period 1981-2017, and sub-periods 1981-2004 and 2005-2017, on a horizontal 1/4° × 1/4° grid. The biogeochemical climatology is built on 19 depth levels and for the dissolved inorganic nutrients nitrate, phosphate and orthosilicate. To generate smooth and homogeneous interpolated fields, an advanced N-dimensional version of DIVA, DIVAnd v2.5.1 (Barth et al., 2014), has been used.
    Keywords: Binary Object; Binary Object (File Size); Binary Object (Media Type); climatology; Dissolved Inorganic Nutrient; File content; marine biogeochemistry; Mediterranean Region; MULT; Multiple investigations; Western_Mediterranean_Sea; Western Mediterranean Sea
    Type: Dataset
    Format: text/tab-separated-values, 18 data points
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  • 8
    Publication Date: 2024-04-20
    Description: This data set contains the post-processed current profiles collected by means of a vessel-mounted ADCP (on the Belgia vessel RV BELGICA) in the Western Mediterranean Sea during May 2022. The TAlPro2022 cruise was part of the Med-SHIP programme. During the whole campaign a VM-ADCP (RDI Ocean Surveyor, 75 KHz) worked along the ship route. The depth range of the current profiler is about 725 m. Data acquisition is carried out using the RDI VMDAS software vers. 1.50.19. The number of bins has been set to 80, with a bin size of 10 m . The instrument ran in narrowband mode and was controlled by computers using the conventional RDI VMDAS software under a MS Windows system with a pinging set to be as fast as possible. No interferences with other used acoustical instruments were observed. The ADCP data have been post-processed with the CODAS3 Software System, which allows extracting data, assigning coordinates, editing and correcting velocity data. Moreover, the data were corrected for errors in the value of sound velocity in water, and misalignment of the instrument with respect to the axis of the ship (about 0.42 degrees). After additional editing, to eliminate suspect values, and those where certain thresholds were surpassed, one netCDF file was created by CODAS3.
    Keywords: ADCP data; Belgica; current meter; Current velocity, east-west; Current velocity, north-south; DATE/TIME; DEPTH, water; EUROFLEET2; LATITUDE; LONGITUDE; Mean angle of ships heading; Mediterranean Sea; Med-SHIP; New operational steps towards an alliance of European research fleets; Number of pings; Percent good pings; Quality flag, profile; Ship velocity, East; Ship velocity, North; Signal strength; TAIPro2022_ADCP; TAlPro2022; Temperature, technical; Time in days; Vessel mounted Acoustic Doppler Current Profiler, RDI Ocean Surveyor, 75 kHz
    Type: Dataset
    Format: text/tab-separated-values, 1197081 data points
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  • 9
    Publication Date: 2024-04-20
    Description: This data set contains the post-processed current profiles collected by means of a vessel-mounted ADCP (on the Spanish vessel RV Ángeles Alvariño) in the Western Mediterranean Sea during August 2016. The TAlPro2016 cruise was part of the MedSHIP programme. During the whole campaign a VM-ADCP (RDI Ocean Surveyor, 150 KHz) works along the whole ship track. The depth range of the current profiler is about 300m. Data acquisition is carried out using the RDI VMDAS software vers. 1.44. The number of bins has been set to 60 m, with a bin size of 8 m. The instrument ran in narrowband mode and was controlled by computers using the conventional RDI VMDAS software under a MS Windows system with a pinging set to be as fast as possible. No interferences with other used acoustical instruments were observed. The ADCP data have been post-processed with the CODAS3 Software System,, which allows extracting data, assigning coordinates, editing and correcting velocity data. Moreover, the data were corrected for errors in the value of sound velocity in water, and misalignment of the instrument with respect to the axis of the ship (about 0.3 degrees). After additional editing, to eliminate suspect values, and those where certain thresholds were surpassed, a netCDF file was created by CODAS3.
    Keywords: ADCP data; Angeles Alvarino; CT; current meter; EUROFLEET2; Mediterranean Sea; New operational steps towards an alliance of European research fleets; TAlPro-2016; TAlPro2016-track; Underway cruise track measurements
    Type: Dataset
    Format: application/x-netcdf, 12.2 MBytes
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  • 10
    Publication Date: 2024-04-20
    Description: The Sicily Channel (SC) site has been monitored for thermohaline properties and water mass exchanges since 1993 by two moorings located within parallel trenches in the 150 km-long transect between Tunisia and Sicily. They form two of the longest Mediterranean time series of thermohaline properties. Due to the Coriolis effect, the IW core at the sill that funnel its westward flow is squeezed to the right, in both trenches, with the 400 m deep record in the north-eastern mooring (called C01) showing slightly warmer (by about 0.04 °C) and saltier (by about 0.01) values than the south-western one (called C02). As the temperature (T) and salinity (S) time series at both sites are very similar only the C02 (WMO code: 6101022, position: 37.2843° N, 11.4995° E) time series is presented here. The nominal depth of the instruments is 400 m, which is however subject to slight variations between servicing of the mooring, of the order of few tens of meters. From 1993 to November 2002 temperature and conductivity have been recorded by means of Aanderaa RCM7 current meters, with an accuracy of 0.05 °C and 0.05 for T and S, respectively. Since November 2002, SBE37 probes have been used, which further improved the quality of the measurements, yielding 0.002 °C and 0.001 for T and S, respectively. Both types of instruments (RCM and SBE) have been regularly calibrated (at least on an annual basis).
    Keywords: C02; CIESM Hydrochanges Program; COMMON_SENSE; Cost-effective sensors, interoperable with international existing ocean obsering systems, to meet EU policies requirements; DATE/TIME; DEPTH, water; Hydrochanges; JERICO; Latitude of event; Longitude of event; Mediterranean Sea; Mooring; Mooring (long time); MOORY; OCEAN-CERTAIN; Ocean Food-web Patrol – Climate Effects: Reducing Targeted Uncertainties with an Interactive Network; PERSEUS; Policy-oriented marine Environmental Research in the Southern EUropean Seas; RITMARE; RITMARE Flagship Project; Salinity; Salinity; Temperature; see abstract; SESAME; Sicily Channel; Southern European Seas: Assessing and Modelling Ecosystem Changes; Temperature, water; Time in days; Towards a joint European research infrastructure network for coastal observatories; warming; WMO_6101022
    Type: Dataset
    Format: text/tab-separated-values, 23804 data points
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