@book{Newman1977,
author = {J. N. Newman},
title = {Marine Hydrodynamics},
- journal = {},
+ url = {https://mitpress.mit.edu/9780262534826/marine-hydrodynamics/},
+ publisher = {The MIT Press},
year = 1977
}
@article{HeltaiBangerthKronbichler-2021,
author = {Luca Heltai and Wolfgang Bangerth and Martin Kronbichler and Andrea Mola},
journal = {Transactions on Mathematical Software},
- month = {December},
+ month = dec,
+ url = {https://dl.acm.org/doi/10.1145/3468428},
+ doi = {10.1145/3468428},
number = {4},
pages = {1--30},
title = {Propagating geometry information to finite element computations},
the flow is unitary in each coordinate direction, i.e., $(1,1)$ in dimension two and $(1,1,1)$ in dimension #3#, so the appropriate exact solution on the
surface of the sphere is the superposition of the above solution with
the analogous solutions along the other axes, or $\phi =
-(x + y)$ in dimension two and $\phi = \frac{1}{2}(x + y + z)$ in dimension three.
\ No newline at end of file
+(x + y)$ in dimension two and $\phi = \frac{1}{2}(x + y + z)$ in dimension three.