Modern atmospheric and ocean science require sophisticated geophysical fluid dynamics models. Among them, stochastic partial
differential equations (SPDEs) have become increasingly relevant. The stochasticity in such models can account for the effect
of the unresolved scales (stochastic parametrizations), model uncertainty, unspecified boundary condition, etc. Whilst there is an
extensive SPDE literature, most of it covers models with unrealistic noise terms, making them un-applicable to
geophysical fluid dynamics modelling. There are nevertheless notable exceptions: a number of individual SPDEs with specific forms
and noise structure have been introduced and analysed, each of which with bespoke methodology and painstakingly hard arguments.
In this talk I will present a criterion for the existence of a unique maximal strong solution for nonlinear SPDEs. The work
is inspired by the abstract criterion of Kato and Lai [1984] valid for nonlinear PDEs. The criterion is designed to fit viscous fluid
dynamics models with Stochastic Advection by Lie Transport (SALT) as introduced in Holm [2015]. As an immediate application, I show that
the incompressible SALT 3D Navier-Stokes equation on a bounded domain has a unique maximal solution.
This is joint work with Oana Lang, Daniel Goodair and Romeo Mensah and it is partially supported by European Research Council (ERC)
Synergy project Stochastic Transport in the Upper Ocean Dynamics (https://www.imperial.ac.uk/ocean-dynamics-synergy/