## 5. An approximation for a general atmosphereModel atmospheres are usually not so perfect as to be considered in the cases treated in the last section. In the absence of a general analytical solution for the evolution operator, we must manage those general models numerically. Our strategy is to integrate everything we can and to linearize the rest. For this purpose we borrow a technique from other successful numerical integrators as the well-known DELO (Rees et al., 1989). In what follows we develop this idea. We want to integrate the transfer equation The integration is to be made in the interval and the atmosphere in the two extreme points and is specified, that is, we know and and also and . The incoming light is also given. We want to obtain the polarized light at : . After the last section we already know how to integrate the transfer equation if the atmosphere is characterized by the prescriptions given there. Note that, given the atmosphere at the two points and , one can always calculate the angles and and the matrix at those two levels, and look for a suitable integrable atmosphere in agreement with expression (27) which satisfy the data at and as far as possible. So let us approximate our atmosphere between these two levels by this integrable atmosphere, represented by a matrix and an emission vector . We can obtain a solution for the equation taking as initial condition . Substraction of Eq. (65) from Eq. (64) results in where and given as solution to Eq. (65). This equation reflects the error made under the previous approximation. Following our strategy, once we have solved for the integrable part we linearize the rest. So that we now assume that the right hand side of equation (66) is small and can be linearized in the interval . We define and upon linearization we write where At , we have , and we obtain To solve Eq. (67) we write And by means of the linearization the last integral becomes so that, substituting In this expression everything is already known except for that is precisely what we want to calculate. A convenient choice of the overlined parameters may render equation (73) simpler. For illustration, let us choose and , . We then obtain a solution for . This solution is not exact, its precision depends on how good the linear approximation is. In the limit, we can made the integration interval as small as we want but at the cost of increasing the number of layers. A compromise will be necessary between speed and required precision. © European Southern Observatory (ESO) 1999 Online publication: December 22, 1998 |