Short-period regional P/S amplitude ratios hold much promise for discrimina
ting low-magnitude explosions from earthquakes in a Comprehensive Test Ban
Treaty (CTBT) monitoring context. However, propagation path effects lead to
variability in regional-phase amplitudes that, if not accounted for, can r
educe or eliminate the ability of P/S ratios to identify the seismic source
. Here we compare four different methodologies that account for the effect
of heterogeneous structure on P/S amplitude variance: (1) distance correcti
ons, (2) path-specific crustal waveguide parameter regressions, (3) cap ave
raging (running mean smoothing), and (4) kriging, The predictability of eac
h method is established by cross-validation (leave-one-out) analysis. We ap
ply these techniques to Pn/Lg, Pg/Lg, and Pn/Sn observations in three frequ
ency bands from 0.75 to 6.0 Hz at station ABKT (Alibek, Turkmenistan), site
of a primary station of the International Monitoring System (IMS), Paths t
o ABKT sample diverse crustal structures (e.g, various topographic, sedimen
tary, and geologic structures), leading to great variability in the observe
d P/S amplitude ratios. For these data to be useful for isolating source ch
aracteristics, the scatter needs to be reduced by accounting for the path e
ffects, and the resulting distribution needs to be Gaussian for most existi
ng spatial interpolation and discrimination strategies to have valid applic
ation. Each method reduces the scatter of the P/S amplitude measurements wi
th varying degrees of success; however, kriging has the distinct advantages
of providing the greatest variance reduction and a continuous correction s
urface with an estimate of the model uncertainty. The largest reductions in
scatter are found for the lowest frequency P/S ratios (<3.0 Hz).