School of Oceanography
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.
Neutral surface pressure, absolute salinity and potential vorticity (PV) are on a 1° grid (coordinates indicated by lat, lon). Absolute geostrophic streamfunction (Aabs) is on a 2° grid (coordinates indicated by lat_A, lon_A). Absolute geostrophic velocity components (Uabs = eastward; Vabs = northward) are on a 2° grid with coordinates in between lat_A and lonA.
Neutral surface pressure, absolute salinity and potential vorticity (PV) are on a 1° grid (coordinates indicated by lat, lon).
Absolute geostrophic streamfunction (Aabs) is on a 2° grid (coordinates indicated by lat_A, lon_A).
Absolute geostrophic velocity components (Uabs = eastward; Vabs = northward) are on a 2° grid with coordinates in between lat_A and lonA.