Figures & data
Figure 1. The spherical coordinate system: θ is the polar angle, φ is the azimuthal angle (the angle of longitude) and r represents the distance to the origin.
Research Article
Exact solutions for geophysical flows with discontinuous variable density and forcing terms in spherical coordinates
Jifeng Chua Department of Mathematics, Shanghai Normal University, Shanghai, People's Republic of China;b Erwin Schrödinger International Institute for Mathematics and Physics, University of Vienna, Vienna, Austria
https://orcid.org/0000-0002-8380-8878View further author information
https://orcid.org/0000-0002-8380-8878View further author information, Calin Iulian Martinb Erwin Schrödinger International Institute for Mathematics and Physics, University of Vienna, Vienna, Austria;c Faculty of Mathematics, University of Vienna, Wien, AustriaCorrespondence[email protected]
https://orcid.org/0000-0002-5800-9265View further author information
https://orcid.org/0000-0002-5800-9265View further author information & Kateryna Marynetsb Erwin Schrödinger International Institute for Mathematics and Physics, University of Vienna, Vienna, Austria;d Faculty of Electrical Engineering, Mathematics and Computer Science, Delft Institute of Applied Mathematics, Delft University of Technology, Delft, The Netherlandshttps://orcid.org/0000-0002-0043-6336View further author information
https://orcid.org/0000-0002-0043-6336View further author information