One difference though is that the ARGO floats are unfortunately not recycled, and just wash up on various beaches. (I'm curious whether you think you can realistically collect many of these mini balloons?)
If you do want to control the lateral position of fleets of sensors, oceanographers also now have "gliders", which are basically small powered drone submarines. These are used by a few groups, but most of the gliders in the world are operated by the US Navy, who launch them out of torpedo tubes to survey local ocean conditions (which is badass).
https://oceanservice.noaa.gov/facts/ocean-gliders.html
The recorded measurements present an interesting data assimilation challenge - they record data along 3D trajectories (4D including time), sampling jagged and twisting lines through the 4D space. But we normally prefer to think of weather/ocean data as gridded, so you need to interpolate the trajectory data onto the grid, whilst keeping the result physically-consistent. Oceanographers use systems like ECCO for ocean state estimation, which effectively find the "ocean of best fit" to various data sources.
Interestingly ECCO uses an auto-differentiable form of the governing equations for the ocean flow to ensure that updates stay physically consistent. This works by using a differentiable ocean fluid model called [MITgcm](https://github.com/MITgcm/MITgcm) to perform runs which match experimental data as closely as possible, and minimizing a loss function through gradient descent. The gradient is of a loss function (error) with respect to model input parameters + forcings, which is calculated by running MITgcm in adjoint mode - i.e. automatic differentation. Therefore this approach is sort of ML before it was cool (they were doing all this well before the new batch of AI weather models). See slides 9-18 of this deck for a nice explanation
https://firebasestorage.googleapis.com/v0/b/firescript-577a2...
The trajectory data is also interesting because it's sort of tabular, but also you often want to query it in an array-like 4D space. You could also call it a "ragged" array. We have nice open-source tools for gridded (non-ragged) arrays (e.g. xarray and zarr, and the pangeo.io project) but I think we could provide scientists with better tools for trajectory-like data in general. If that seems relevant to you I would love to chat.
P.S: Sorceror seems awesome, and I applaud you for working on something hard-tech & climate-tech!