Atmospheric pressure changes do not stop at the permeable snow surface but rather propagate into it. These pressure changes range from high-amplitude, low-frequency events caused by seasonal cycles and synoptic weather systems to small-amplitude, high-frequency events caused by topographic features and turbulence. The effect of pressure changes on interstitial air...
This dataset was used to determine the attenuation of an audio signal by reticulated foam samples that span the natural range of intrinsic permeability for seasonal snow. Data are audio measurements acquired on a two-channel oscilloscope.