Corrigendum to “A field study of suspended frazil ice particles” [Cold Regions Science Technology. Volume 55/1 (2008) pp. 86–102]

This note is written to correct an erroneous interpretation of acoustic intensity made by the authors during the writing of the paper “A field study of suspended frazil ice particles” by Brian Morse and Martin Richard. The correct interpretation is presented and the impacts on the findings are quantified.