Environmental Correlates of Arctic Ice-edge Noise
Abstract
Temporal variations of low-frequency, broadband ambient noise measured in early summer under drifting ice floes of the marginal ice zone (MIZ) are cross correlated with local environmental forces and ice field descriptors. Surface gravity wave forcing is the primary correlate of the noise; its interaction with ice floes generates sound, most likely via flexural flow failure, and unloading motion, within a few kilometers of the ice edge.
Document Details
- Document Type
- Technical Report
- Publication Date
- Dec 01, 1991
- Accession Number
- ADA637275
Entities
People
- Ira Dyer
- Nicholas C. Makris
Organizations
- Massachusetts Institute of Technology