Ashik and Novakow: Numerical Modelling of Storm Surges in the Laptev Sea
19
Figure I: The grid of the finite elements.
(10)
n is the number of the elements joined in i-th point.
Let us define Fj = 0 for the points of the solid boundary in equations (7) and (8) and Fj= 0 for
the points of the open sea boundary in (9) to satisfy the boundary conditions (2), (3).
Now we can obtain gradients of the variables in the domain, as:
19
Figure I: The grid of the finite elements.
(10)
n is the number of the elements joined in i-th point.
Let us define Fj = 0 for the points of the solid boundary in equations (7) and (8) and Fj= 0 for
the points of the open sea boundary in (9) to satisfy the boundary conditions (2), (3).
Now we can obtain gradients of the variables in the domain, as: