Our zerothorder solution is characterized by three undetermined fluxsurface functions:
,
, and
.
In order to determine the forms of these functions, we need to expand our model to higher order. (See Section 8.8.)
Expanding Equation (11.68) to third order in , we obtain
we obtain

(11.124) 
where

(11.125) 
and use has been made of Equations (8.75), (11.95)–(11.99), (11.103), (11.104), (11.107), and (11.108).
The fluxsurface average of Equation (11.124) yields

(11.126) 
where use has been made of Equations (8.68), (8.70), and (11.114), and (11.116). Note that
, by symmetry.
Hence,
where use has been made of Equation (11.116).
Expanding Equation (11.69) to first order in ,
we obtain

(11.128) 
where use has been made of Equations (11.95)–(11.99), (11.101), (11.103), and (11.104). The fluxsurface average of the
previous equation yields

(11.129) 
We can solve the previous equation, subject to the boundary condition (11.105), to give

(11.130) 
Here, we have taken into account the previously mentioned fact that within the island separatrix.
Note that
is discontinuous across the island separatrix, which implies that the pressure gradient is also discontinuous across the separatrix. As discussed in Section 8.9, we expect this discontinuity to be resolved in a layer of characteristic thickness on the separatrix [see Equation (8.84) and Table 8.1].
Expanding Equation (11.71) to second order in , we obtain
we obtain
0 




(11.131) 
where use has been made of Equations (11.95)–(11.99), (11.101), (11.103), (11.104), (11.107), (11.108), (11.111), and (11.113). The
fluxsurface average of the previous equation yields

(11.132) 
According to Equation (11.121), recalling that
, we get

(11.133) 
inside the separatrix, which implies that . Hence, given that we have already concluded that , Equations (11.121) and
(11.122) yield

(11.134) 
The previous equation can be combined with Equation (11.132) to produce

(11.135) 
Now, it is apparent from the previous equation that there is no discontinuity in across the separatrix. Thus, given that
, it follows that
. It is also clear from Equations (11.105), (11.109), and (11.113) that
.
Thus, we can write

(11.136) 
where

(11.137) 
and
Here,
.