“…The parameters not directly available (
, τ 2 , σ , and
) can be mapped by fitting our functions to in situ observations, then relating these parameters to some property of the surface ocean (e.g., trophic levels), or physical observations (e.g., the larger Argo array), or to time and space (e.g., biogeochemical provinces, seasons), such that they can be mapped over large scales, and used with the other inputs and parameters to extrapolate the surface fields seen from a satellite down through the epipelagic zone. As we move into an era of ocean robotic platforms, with an expanding number of in situ observations, model parameters can be mapped with a higher degree of confidence, and we can continue to improve our capability to monitor ocean biogeochemical cycles (Brewin et al.,
2021; Claustre et al.,
2021).…”