@Mengyang Zhou, @SBachman, does OceanParcels support computing back-trajectories? The forward problem is interesting, because we can tag a parcel of water and see where it goes. Back trajectories are interesting because, for example, if we have an observation at a point, we can see where the water came from.
Yes, OceanParcels supports running in backward time. I can do some experiments on that.
cool, stay focused on the forward runs
at least for now
Yeah, I see.
This paper is focused on atmospheric dynamics, but seems relevant to the questions at hand:
https://journals.ametsoc.org/view/journals/atsc/51/4/1520-0469_1994_051_0530_cawsat_2_0_co_2.xml?tab_body=pdf
and perhaps this:
https://acp.copernicus.org/articles/9/2577/2009/acp-9-2577-2009.pdf
Here's an application of particle advection to the "RunningTide" approach to CDR (launching free-drifting algae platforms)
https://www.nature.com/articles/s41559-022-01722-1
There's some relationship between our questions and "finite-time Lyapunov exponents," which provide a scalar representation of spreading rate. I am not sure how useful FTLE's are in the context of the problem at hand...but they might be and there's substantial literature exploring their applications.
cc @SBachman
FSLE: https://www.sciencedirect.com/science/article/pii/S1463500310001824
FTLE: https://sites.krieger.jhu.edu/waugh/files/2015/07/Waugh_etal_2012_jpo.pdf
https://core.ac.uk/download/pdf/36055385.pdf
Last updated: May 16 2025 at 17:14 UTC