MSEAS forecast of 3D Lagrangian subduction of water volumes for 8 Apr 1200Z to 12 Apr 1200Z 2019, Issued 8 Apr 2019

The following figures show the water volumes that are forecast to subduct in 3D (computed based on our MSEAS forward flowmap forecast) from the surface layers to deeper layers. They illustrate in 3D+time where these waters start, how they move, and where they end up.

The waters that are plotted in this subduction analysis are only the volumes of water that start within the upper ocean layers (0-to-10 m depths) anywhere in our modeling domain and reach 50m after 4 days. This is all that is plotted, at 3 times (blue is day 0, green is day 2 and red is day 4).

Below, the blue water volumes are the initial positions of these waters that start within 0-to-10 m depths and reach 50m after 4 days. These water volumes are advected using a flowmap-based and composition-based advection scheme, using our MSEAS forecast of the 3D ocean currents (u, v and w). The green water volumes represent the location of the parcels after two days while the red water volumes represent the final location after 4 days. The combined figures in the last row show the 3D water volumes, overlaid, at the 3 different times.

As also shown in the forecast below, the ridges of the forward Finite-Time Lyapunov Exponents (FTLEs) are the repelling FTLE structures: they tend to 'repel' water parcels. Two parcels that are close to each other at t=0 but on different sides of the forward FTLE ridge will advect further away from each other than other parcels. The ridges of the backward FTLEs are the attracting FTLE structures: they tend to 'attract' water parcels.

The figures below illustrate the MSEAS forecast of the dominant 3D subduction pathways (from above 10m depth to deeper than 50m depth) over the period 8 Apr 1200Z to 12 Apr 1200Z 2019. The winds are forecast to remain to the east on average and of medium strength up to Apr 10. They are forecast to become weaker for Apr 11 and beyond. The 3D subduction is forecast to continue but weaken along the African coastline and in eddies in that region. However, 3D subduction also occurs along (sub)-mesoscale eddies and frontal structures in the middle of the Alboran sea, especially on the edges of a weak WAG and of the Atlantic jet (e.g. sinking in thin sheets along convergent/attracting fronts and edges of interacting eddies.). Note there is a direct relation between this 3D subduction (from above 10m depth to deeper than 50m depth) and the 3D attracting Lagrangian Coherent Structures that we forecast (see the maps of the forecast 3D backward FTLE fields).

3D Lagrangian subduction in the Calypso Domain (MSEAS 1/200deg tidally-forced forecasts downscaled from WMOP)

Time & Depths	Top View	3D View	Side View
t0 and upper 10m
t0 + 48 hours
t0 + 96 hours and water reaching 60m
Overlaid

96-hr Forecast Backward 3D FTLE field at various depths for April 8 1200Z - April 12 1200Z - The ridges in this 3D field are the flow structures that most attract fluid parcels in 3D over the 4 days.

Depth	2 m	4 m	20 m	40 m	60 m
April 8 - April 12

96-hr Forecast Forward 3D FTLE field at various depths for April 8 1200Z - April 12 1200Z - The ridges in this 3D field are the flow structures that most repel fluid parcels in 3D over the 4 days.

Depth	2 m	4 m	20 m	40 m	60 m
April 8 - April 12