The helicity of a vector field is a metric independent density. Functi
onals with first order elliptic systems for Euler-Lagrange equations h
ave been constructed from the helicity. The metric invariance is prese
rved for finite element discretizations involving ''Whitney elements.'
' This paper relates differential geometric aspects of inverse problem
s to helicity based functionals in two contexts. First, the inverse pr
oblem of electrical impedance tomography in isotropic media is known t
o be equivalent to determining a metric within a given conformal class
from a given ''Dirichlet to Neumann'' map. This fact is related to th
e helicity functional and Wexler's algorithm for recovering an isotrop
ic conductivity. Second, Maxwell's equations in ''spinor form'' are sh
own to be the Euler-Lagrange equations of some complexified time depen
dent generalization of the helicity functional. In this case metric de
pendent aspects yield insight into the ''inverse kinematic problem in
seismology.'' These two examples illustrate the underlying geometric s
tructure in classes of inverse problems and algorithms for their solut
ion.