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Figure2 illustrates the resulting probe coverage for this From these tests it appears that the three-hole-per-step
technique in a vertical plane through the snow. method is significantly faster than the traditional coarse-
probing method. The reason must relate to the stepping
DISCUSSION part of the probe sequence. Multi-hole probing requires
Times within each test set were consistent and snow con- less walking per unit area. Less steps reduces the delays
ditions were ideal so it is possible to compare the various due to waiting for the slowest prober. It also reduces the
techniques. absolute amount of walking each rescuer must do. In the
Test sets #1 and #2 both employed the classic coarse- test site the walking conditions were ideal. In a normal
probe technique but varied the probe length. Using short- avalanchesite where walking is often difficult, the amount
ened probes and limiting the depth was marginally faster of energy saved, and the improvement of work productiv-
however, since the 'full depth' (test #1) was only to 2.1 m. ity should be even greater than in this test.
the results of this comparison are not strongly conclusive. The finger-tip to finger-tip spacing between the probers
The only difference in technique between test set #3 in the three-hole-per-step method results in a finer grid
and #4 was that the team members in #4 each proceededat pattern, 60 x 70 cmcompared to 75 x 70 cm for coarse prob-
their own pace.Wewereinterestedto observe thatthegroup ing. Even with this reduced area coverage factored in, the
with a designatedperson calling thepace(set #3) produced three holeper steptechniqueis still 30%faster thancoarse
a higher rate than the individually pacedgroup. probing. In Figure 3, the area of the respective rectangles
compares the productivity of a rescuer using each of the
techniques. Furthermore, the denser probe pattern actu-
ally improves the theoretical average probability of detec-

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