Electromagnetic Properties of Sea Ice

Abstract

Investigations of the in situ complex dielectric constant of sea ice were made using time-domain spectroscopy. It was found that (1) for sea ice with a preferred horizontal crystal c-axis alignment, the anisotropy of polarizing properties of the ice increased with depth, (2) brine inclusion conductivity increased with decreasing temperature down to about -8 C, at which point the conductivity decreased with decreasing temperature, (3) the DC conductivity of sea ice increased with increasing brine volume, (4) the real part of the complex dielectric constant is strongly dependent upon brine volume but less dependent upon the brine inclusion orientation, (5) the imaginary part of the complex dielectric constant was strongly dependent upon brine inclusion orientation but much less dependent upon brine volume. Because the electromagnetic (EM) properties of sea ice are dependent upon the physical state of the ice, which is continually changing, it appears that only trends in the relationships between the EM properties of natural sea ice and its brine volume and brine inclusion microstructure can be established.

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Document Details

Document Type
Technical Report
Publication Date
Jan 01, 1984
Accession Number
ADA140330

Entities

People

  • Andras Kovacs
  • G. F. Cox
  • R. M. Morey

Organizations

  • Cold Regions Research and Engineering Laboratory

Tags

DTIC Thesaurus Topics

  • Air Gaps
  • Coaxial Cables
  • Crystal Structure
  • Dielectric Permittivity
  • Dielectric Properties
  • Dielectrics
  • Electric Fields
  • Electromagnetic Properties
  • Electromagnetic Radiation
  • Engineering
  • Filter Paper
  • Geometric Forms
  • Geometry
  • Salt Water
  • Sea Water
  • Time-Domain Reflectometry
  • Transmission Lines

Readers

  • Electromagnetic Wave Scattering and Antenna Radiation Engineering
  • Materials Science and Engineering.
  • Polar and Arctic Studies