Oceanic finescale processes are loosely referred to as dynamical processes with horizontal scales of (0.01-100) km including mesoscale eddies, submesoscale processes, fronts, and internal waves, etc. These finescale processes play crucial roles in mediating oceanic energy cascade, biogeochemical and heat transport, and air-sea exchanges, and thus have significant impacts on the marine ecosystem and climate variations. For instance, the strong vertical motions induced by submesoscale processes can, on one hand, increase the primary productivity through upwelling and, one the other hand, facilitate the carbon export through downwelling, both of which having profound influences on biogeochemical cycles, ecosystems, and climate. However, the transient and small-size nature of finescale processes makes their observations and simulations challenging and critical gaps exist in understanding their mechanisms of energy cascade and tracer transport and their pathways in modulating the North Pacific ecosystems and climate. In particular, because the prevailing global models are still too coarse to resolve the finescale processes, their energy cascading and tracer transporting effects have to be parameterized in models. Improper parameterizations of finescale processes can lead to significant biases in projections of ocean warming, acidification, deoxygenation, and thus marine biodiversity and climate resilience.
The PICES Working Group 38 (
WG 38) on “Mesoscale and Sub-mesoscale Processes” has ended in 2019, and the
WG 50 on “Sub-mesoscale Processes and Marine Ecosystems” will be ended this year. While WG 38 and WG 50 have done a lot of work on meso- and submesoscale processes, additional finescale processes such as internal waves are not included. Furthermore, model parameterizations of finescale processes were not considered. It is timely and scientifically meaningful to transition from the tasks of the above two WGs to our proposed new WG: “Oceanic Finescale Processes: Impacts and Parameterizations”.
The new WG aims to (1) collecting and integrating high-resolution observational datasets and simulation outputs and data analysis methods to better study finescale processes, (2) better understanding the physics of finescale processes and their impacts on the North Pacific climate variations, (3) enhancing the knowledge finescale processes’ roles in biogeochemical processes (e.g., primary production and carbon export) and their impacts on the North Pacific ecosystems, (4) evaluating and developing parameterizations of finescale processes and (5) evaluating their influences on the models’ performance in the North Pacific”. The establishment of this WG helps to understand the status and changes of North Pacific ecosystems and climate and to improve the models’ simulation and projection capabilities on these issues. It will also develop tight collaborations with international colleagues to promote studies on the relevant topics.