Effective flow resistivity is the dominant ground absorption parameter.

Evidence

These examples show that hard boundaries, i.e., those with a high effective flow resistivity, act as good reflectors and have little effect on pulse waveforms, while soft, absorbent boundaries with low effective flow resistivities can produce radically different waveforms by absorbing the higher frequencies. Additional calculations (omitted here) revealed that the three other parameters involved in Attenborough’s model have an influence on the waveforms smaller than that of the effective flow resistivity. — Donald G. Albert and John A. Orcutt, Acoustic Pulse Propagation Above…, 73

Categorization

  • XREF: Directly satisfies the polyad need: explains the physical mechanism of why snow (low resistivity surface) absorbs high frequencies and elongates late-season recordings — directly relevant to Soundscape Ethnography ground-impedance confounds. — connects to: Snow exceeds other natural surfaces in sound absorption by a large margin. — Donald G. Albert and John A. Orcutt, Acoustic Pulse Propagation Above…, 6; Snow grounds require a layered porous-medium impedance model. — Donald G. Albert and John A. Orcutt, Acoustic Pulse Propagation Above…, 26; Ground impedance, not foliage, governs low-band attenuation by vegetation. — Donald Aylor, Noise Reduction by Vegetation and Ground, 2

Broader Connections