Experimental efforts to measure neutrinos by radio-frequency (RF) signals resulting from neutrino interactions in-ice have intensified over the last decade. Recent calculations indicate that one may dramatically improve the sensitivity of ultra-high energy (UHE; >EeV) neutrino experiments via detection of radio waves trapped along the air-ice surface. Detectors designed to observe the Askaryan effect currently search for RF electromagnetic pulses propagating through bulk ice, and could therefore gain sensitivity if signals are confined to the ice-air boundary. To test the feasibilty of this scenario, measurements of the complex radio-frequency properties of several air-dielectric interfaces were performed for a variety of materials. Two-dimensional surfaces of granulated fused silica (sand), both in the lab as well as occurring naturally, water doped with varying concentrations of salt, natural rock salt formations, granulated salt and ice itself were studied, both in North America and also Antarctica. In no experiment do we observe unambiguous surface wave propagation, as would be evidenced by signals travelling with reduced signal loss and/or superluminal velocities, compared to conventional EM wave propagation.
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