Overview animation of glider movements during MASSMO 4 (Marine Autonomous Systems in Support of Marine Observations) in the Faroe-Shetland Channel in May-June 2017. MASSMO is a pioneering multi-partner series of trials and demonstrator missions that aim to explore the UK seas using a fleet of innovative marine robots. This animation shows some qualitative comparisons between the glider data (DSTL, NOC) with satellite altimetry (Copernicus), satellite-derived front position (PML) and FOAM AMM7 model data (Copernicus). Bathymetry is GEBCO, animation created using Paraview.

SSH1
Particle tracks released into Sea Surface Height vector field

This animation combined numerous different datasets, and varied in scale from entire ocean basins to internal front structure measuring a few kilometres.  As in other recent Paraview projects, I created the whole animation in spherical coordinates.  This entailed using trigonometry to convert (lat,lon,depth) to positions on a global sphere of radius 1.  The ocean was exaggerated by 75 times so the internal structure could easily be seen.

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The full MASSMO 4 glider mission north of the UK, viewed from the north-east.  Observed water temperatures are shown.
model1
A cutaway of bathymetry to show a cross-section of the FOAM model as it bisects the glider observations

During the mission, three of the gliders investigated a frontal region visible on satellite imagery.  Satellites can’t ‘see’ below the sea surface, so the fleet of gliders was able to responsively move to the location of the front and map the 3D internal structure.

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Satellite-derived front positions (PML) on 24th May 2017 overlaid on glider data and local bathymetry
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Close-up of frontal region on the shallow continental shelf.  Glider salinity observations are shown, along with satellite-derived front positions and modelled flow speeds

The mission was supported by the Met Office FOAM (Forecast Ocean Assimilation Model) which provided context for the glider observations.

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Modelled slope current – vectors and surface showing core of flow
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