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Description of the model

(MM, A)limepy: (Multi-Mass, Anisotropic) Lowered Isothermal Model Explorer in Python

Isotropic models

The isotropic distribution functions are defined as (Gomez-Leyton & Velazquez 2014)

f_g(E) = \displaystyle \begin{cases}
A\exp(E), &g=0 \\
\displaystyle A\exp(E)P(g, E), &g>1
\end{cases}

where \displaystyle E = \frac{\phi - \phi(r_{\rm
t}) - v^2/2}{\sigma^2}, \sigma is a velocity scale, 0 <
\phi-\phi(r_{\rm t}) <W_0/\sigma^2 is the (positive) potential and P(s,x) is the regularised lower incomplete gamma function P(s,x) =
\gamma(s,x)/\Gamma(x). For some integer values of g several well known models are found

Anisotropic models

Radial anisotropy a la Michie (1963) can be included as follows

f_g(E, J^2) = \exp(-J^2)f_g(E),

where J^2 = (rv_t)^2/(2r_{\rm a}^2\sigma^2), here r_{\rm a} is the user-defined anisotropy radius.

Multi-mass model

Multi-mass models are found by summing the DFs of individual mass components and adopting for each component (following Gunn & Griffin (1979))

\sigma_j       &\propto  \mu_j^{-\delta}\\
r_{{\rm a},j}  &\propto  \mu_j^{\eta}

where \mu_j = m_j/\bar{m} and \bar{m} is the central density weighted mean mass.