School of Oceanography
This website contains complete fields associated with a "hydrographic" inverse model to determine the absolute geostrophic flow consistent with conservation of potential vorticity and salinity on neutral surfaces.
If you use the data or fields in publications or presentations, please reference:
Hautala, S. L. (2018). The circulation of deep and abyssal water in the Northeast Pacific Basin. Progress in Oceanography 160: 68-82.
This project was funded by the National Science Foundation.
Thanks to undergraduate research assistant Una Miller for her work on website design and construction.