SpECTRE
v2024.06.18

Redistributes gridpoints on the sphere. More...
#include <EquatorialCompression.hpp>
Public Member Functions  
EquatorialCompression (double aspect_ratio, size_t index_pole_axis=2)  
EquatorialCompression (EquatorialCompression &&)=default  
EquatorialCompression (const EquatorialCompression &)=default  
EquatorialCompression &  operator= (const EquatorialCompression &)=default 
EquatorialCompression &  operator= (EquatorialCompression &&)=default 
template<typename T >  
std::array< tt::remove_cvref_wrap_t< T >, 3 >  operator() (const std::array< T, 3 > &source_coords) const 
std::optional< std::array< double, 3 > >  inverse (const std::array< double, 3 > &target_coords) const 
The inverse function is only callable with doubles because the inverse might fail if called for a point out of range, and it is unclear what should happen if the inverse were to succeed for some points in a DataVector but fail for other points.  
template<typename T >  
tnsr::Ij< tt::remove_cvref_wrap_t< T >, 3, Frame::NoFrame >  jacobian (const std::array< T, 3 > &source_coords) const 
template<typename T >  
tnsr::Ij< tt::remove_cvref_wrap_t< T >, 3, Frame::NoFrame >  inv_jacobian (const std::array< T, 3 > &source_coords) const 
void  pup (PUP::er &p) 
bool  is_identity () const 
Static Public Attributes  
static constexpr size_t  dim = 3 
Friends  
bool  operator== (const EquatorialCompression &lhs, const EquatorialCompression &rhs) 
Redistributes gridpoints on the sphere.
A mapping from the sphere to itself which redistributes points towards (or away from) a userspecifed axis, indicated by index_pole_axis_
. Once the axis is selected, the map is determined by a single parameter, the aspect_ratio
\(\alpha\), which is the ratio of the distance perpendicular to the polar axis to the distance along the polar axis for a given point. This parameter name was chosen because points with \(\tan \theta = 1\) get mapped to points with \(\tan \theta' = \alpha\). In general, gridpoints located at an angle \(\theta\) from the pole are mapped to a new angle \(\theta'\) satisfying \(\tan \theta' = \alpha \tan \theta\).
For an aspect_ratio
greater than one, the gridpoints are mapped towards the equator, leading to an equatorially compressed grid. For an aspect_ratio
less than one, the gridpoints are mapped towards the poles. Note that the aspect ratio must be positive.
Suppose the polar axis were the zaxis, given by index_pole_axis_ == 2
. We can then define the auxiliary variables \( r := \sqrt{x^2 + y^2 +z^2}\) and \( \rho := \sqrt{x^2 + y^2 + \alpha^{2} z^2}\).
The map corresponding to this transformation in cartesian coordinates is then given by:
\[\vec{x}'(x,y,z) = \frac{r}{\rho}\begin{bmatrix} x\\ y\\ \alpha^{1} z\\ \end{bmatrix}.\]
The mappings for polar axes along the x and y axes are similarly obtained.