55
Such considerations point to the need for a three-dimensional hydrodynamic model to compute
the vertical fluxes in the domain of interest.
Figure 6. Limits of the computational domain, with bathymetry (depth in meters).
176' W
175' W
174' W
4 n lldy,. S
'''11;1
r1
I. Lawrence Is.
66'
cold water plume
17)' W L - -...... ---'"---~ 64~ ' ":": N--------":': 65~ . -::-.........
170' W
169' W
Figure 7. Schematic representation of the plume of cold water downstream of the Anadyr Strait.