New software enables global ocean biogeochemical modeling in Python

Have you ever wondered what life would be like if you could write and run complex biogeochemical models easily and conveniently in Python? Wonder no more. In a paper published in J. Adv. Model. Earth Syst., Samar Khatiwala (2025; see reference below) describes tmm4py, a new software to enable efficient, global scale biogeochemical modelling in Python.

tmm4py is based on the Transport Matrix Method (TMM), an efficient numerical scheme for “offline” simulation of tracers driven by circulations from state-of-the-art physical models and state estimates. tmm4py exposes this functionality in Python, providing the tools needed to implement complex models in pure Python using standard modules such as NumPy, and run them interactively on hardware ranging from laptops to supercomputers. No knowledge of parallel computing required! tmm4py even extends the interactivity to models written in Fortran, allowing the many existing models coupled to the TMM, e.g., MITgcm, to be used from the familiar comfort of Python. Whether you’re a seasoned modeler, just want to try out an idea, or illustrate a concept in your teaching, tmm4py is designed to make biogeochemical modeling more widely accessible.

Download the code from: https://github.com/samarkhatiwala/tmm

Click here to open the image in a new window for a larger view.
Figure: Schematic illustrating the structure of tmm4py and its relationship with the various libraries and components it is built on or interacts with. Outlined boxes represent user‐supplied code (such as the “Hello World” example of the ideal age tracer shown on the left). Other low-level libraries on which tmm4py depends, for example, BLAS and LAPACK for linear algebra, MPI for parallel communication, and CUDA for GPUs, are not shown.

Reference:

Khatiwala, S. (2025). tmm4py: Global Ocean Biogeochemical Modeling in Python With the Transport Matrix Method. Journal of Advances in Modeling Earth Systems, 17. doi: 10.1029/2025ms005028

Joint Science Highlight with US Ocean Carbon and Biogeochemistry Programme (OCB).

Latest highlights

Another step towards replacing NOBIAS Chelate PA-1

Kanna and his colleagues successfully carried out the quantitative pre-concentration of seven trace metals…

Neodymium budget in the Arabian Sea is governed by a combination of water mass advection and dominant boundary exchange processes

Karri and Singh established the neodymium concentrations and isotopic compositions along a North-South section in the eastern Arabian Sea…

Cerium isotopes confirm that hydrogenetic iron-manganese crusts are precipitating from the oxygen minimum zone to abyssal depths

Li and co-authors provide new insights on the formation mechanism of ferromanganese crusts.

Continuous record of the Antarctic Circumpolar Current latitude over the last glacial-interglacial cycles

The meridional positions of the oceanic fronts separating subtropical and Antarctic waters are key to constraining the mechanisms that drive the degassing of deeply-stored CO2 at the end of the glacial periods…

Rechercher