MOOSE T00_27 (EGO milou glider) deployment (Mediterranean Sea - Western basin)

Date 2017-09
Temporal extent 2013-09-20 -2013-11-02
Author(s) Testor PierreORCID1, 2, Mortier Laurent1, 3, Coppola LaurentORCID4, Claustre HervéORCID4, D'Ortenzio Fabrizio4, Bourrin FrançoisORCID2, 5, Durrieu De Madron XavierORCID5, Raimbault Patrick6
Contributor(s) Béguery Laurent, Benabdelmoumène Hassane, Duformentelle Pierrette
Affiliation(s) 1 : LOCEAN, France
2 : CNRS, France
3 : ENSTAParisTech, France
4 : LOV, France
5 : CEFREM, France
6 : MIO, France
DOI 10.17882/51423
Publisher SEANOE
Keyword(s) volume scattering function of radiative flux in sea water 532, volume absorption coefficient of radiative flux in sea water due to dissolved organic matter, volume scattering function of radiative flux in sea water 880, chlorophyll a signal from fluorescence sensor in sea water, volume scattering function of radiative flux in sea water 532, volume scattering function of radiative flux in sea water 470, sea water temperature, sea water electrical conductivity, sea water pressure, mole concentration of dissolved molecular oxygen in sea water, temperature of sensor for oxygen in sea water, uncalibrated phase shift reported by oxygen sensor, calibrated phase shift reported by oxygen sensor
Abstract

The proposed research is based on the monitoring of the long term evolution of the North Western Mediterranean Sea with glider repeat-sections carried out in the framework of the ALLENVI/INSU/ SOERE MOOSE (http://moose-network.fr), INSU/MISTRALS (http://www.mistrals-home.org), and EU FP7 PERSEUS (http://www.perseus-net.eu).  The objective is to monitor the oceanographic variability (physical and biogeochemical) of the north western Mediterranean Sea, over a continuum of spatial and temporal scales. Two cross-basin repeat-sections with a repeat rate of about 10-20 days allow to monitor the main circulation features (Northern Current, North Balearic Front, Western Corsica Current) on a regular basis, as well as major processes such as winter intermediate and deep water formations and vernal blooms. The gliders regularly visit MOOSE moorings for cross-calibration purposes and to explore the variability around these moorings.

i) T00 is a repeat-section between Nice and Calvi passing by the MOOSE mooring DYFAMED located in the central Ligurian Sea

ii) T02 is a repeat-section between Marseille and Menorca passing by the MOOSE mooring LION located in the center of the deep convection area

The following parameters are provided : 


  • Practical salinity

  • Sea temperature in-situ ITS-90 scale

  • Electrical conductivity

  • Sea water pressure, equals 0 at sea-level

Licence CC-BY-NC
Utilisation EGO data are published without any warranty, express or implied. The user assumes all risk arising from his/her use of EGO data. EGO data are intended to be research-quality and include estimates of data quality and accuracy, but it is possible that these estimates or the data themselves contain errors. It is the sole responsibility of the user to assess if the data are appropriate for his/her use, and to interpret the data, data quality, and data accuracy accordingly. EGO welcomes users to ask questions and report problems to the contact addresses listed in the data files or on the EGO internet page.
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Data
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51993.tar.gz 49 MB NC, NetCDF Quality controlled data Open access
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How to cite 

Testor Pierre, Mortier Laurent, Coppola Laurent, Claustre Hervé, D'Ortenzio Fabrizio, Bourrin François, Durrieu De Madron Xavier, Raimbault Patrick (2017). MOOSE T00_27 (EGO milou glider) deployment (Mediterranean Sea - Western basin). SEANOE. https://doi.org/10.17882/51423