In coastal regions the presence of the marine boundary layer can significan
tly affect RF propagation, The relatively high specific humidity of the und
erlying "marine layer" creates elevated trapping layers in the radio refrac
tivity structure. While direct sensing techniques provide good data, they a
re limited in their temporal and spatial scope. There is a need for assessi
ng the three-dimensional (3-D) time-varying refractivity structure. Recentl
y published results (Gingras et al, [1]) indicate that matched-field proces
sing methods hold promise for remotely sensing the refractive profile struc
ture between an emitter and receive array, This paper is aimed at precisely
quantifying the performance one can expect with matched-held processing me
thods for remote sensing of the refractivity structure using signal strengt
h measurements from a single emitter to an array of radio receivers. The pe
rformance is determined,ia simulation and is evaluated as a function of: 1)
the aperture of the receive array; 2) the refractivity profile model; and
3) the objective function used in the optimization. Refractivity profile es
timation results are provided for a surface-based duct example, an elevated
duct example, and a sequence of time-varying refractivity profiles. The re
fractivity profiles used were based on radiosonde measurements collected of
f the coast of southern California.