Ground-Wave Path Loss Over Ice-Covered Sea at Frequencies between 0.1 and 10 MHz.

The ground-wave attenuation function has been studied for an involving propagation over an ice-covered sea surface. A review of the techniques that can be used in the analysis of a multilayer ground is presented, and a number of practical sea-ice paths are evaluated numerically. Results are presente...

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Bibliographic Details
Main Author: Kennedy,Edward J.
Other Authors: NAVAL RESEARCH LAB WASHINGTON DC
Format: Text
Language:English
Published: 1987
Subjects:
ICE
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA180819
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA180819
id ftdtic:ADA180819
record_format openpolar
spelling ftdtic:ADA180819 2023-05-15T14:51:35+02:00 Ground-Wave Path Loss Over Ice-Covered Sea at Frequencies between 0.1 and 10 MHz. Kennedy,Edward J. NAVAL RESEARCH LAB WASHINGTON DC 1987-05-06 text/html http://www.dtic.mil/docs/citations/ADA180819 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA180819 en eng http://www.dtic.mil/docs/citations/ADA180819 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Radiofrequency Wave Propagation Snow Ice and Permafrost *GROUND WAVES(ELECTROMAGNETIC) *TRANSMISSION LOSS *SEA ICE ARCTIC REGIONS ATTENUATION ELECTROMAGNETIC WAVE PROPAGATION GROUND LEVEL ICE LAYERS LENGTH LOSSES MEDIUM FREQUENCY OCEANS OPEN WATER PATHS SEA WATER THICKNESS OCEAN SURFACE RADIATION ATTENUATION Ice Cover Arctic Communication PE62721N WUDN291241 Text 1987 ftdtic 2016-02-19T09:41:03Z The ground-wave attenuation function has been studied for an involving propagation over an ice-covered sea surface. A review of the techniques that can be used in the analysis of a multilayer ground is presented, and a number of practical sea-ice paths are evaluated numerically. Results are presented for the 0.1 to 10 MHz frequency range and consist of curves showing propagation loss as a function of distance for various ice thicknesses. It is shown that the variation of the attenuation function with distance and with frequency is significantly different than for the open ocean case. A range of frequencies over which path loss is predicted to be less than for seawater only is dependent on the path length and is shown to lie in the medium frequency range. Keywords: Ground waves(Electromagnetic); Arctic communication; Electromagnetic propagation over ice. Text Arctic Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Radiofrequency Wave Propagation
Snow
Ice and Permafrost
*GROUND WAVES(ELECTROMAGNETIC)
*TRANSMISSION LOSS
*SEA ICE
ARCTIC REGIONS
ATTENUATION
ELECTROMAGNETIC WAVE PROPAGATION
GROUND LEVEL
ICE
LAYERS
LENGTH
LOSSES
MEDIUM FREQUENCY
OCEANS
OPEN WATER
PATHS
SEA WATER
THICKNESS
OCEAN SURFACE
RADIATION ATTENUATION
Ice Cover
Arctic Communication
PE62721N
WUDN291241
spellingShingle Radiofrequency Wave Propagation
Snow
Ice and Permafrost
*GROUND WAVES(ELECTROMAGNETIC)
*TRANSMISSION LOSS
*SEA ICE
ARCTIC REGIONS
ATTENUATION
ELECTROMAGNETIC WAVE PROPAGATION
GROUND LEVEL
ICE
LAYERS
LENGTH
LOSSES
MEDIUM FREQUENCY
OCEANS
OPEN WATER
PATHS
SEA WATER
THICKNESS
OCEAN SURFACE
RADIATION ATTENUATION
Ice Cover
Arctic Communication
PE62721N
WUDN291241
Kennedy,Edward J.
Ground-Wave Path Loss Over Ice-Covered Sea at Frequencies between 0.1 and 10 MHz.
topic_facet Radiofrequency Wave Propagation
Snow
Ice and Permafrost
*GROUND WAVES(ELECTROMAGNETIC)
*TRANSMISSION LOSS
*SEA ICE
ARCTIC REGIONS
ATTENUATION
ELECTROMAGNETIC WAVE PROPAGATION
GROUND LEVEL
ICE
LAYERS
LENGTH
LOSSES
MEDIUM FREQUENCY
OCEANS
OPEN WATER
PATHS
SEA WATER
THICKNESS
OCEAN SURFACE
RADIATION ATTENUATION
Ice Cover
Arctic Communication
PE62721N
WUDN291241
description The ground-wave attenuation function has been studied for an involving propagation over an ice-covered sea surface. A review of the techniques that can be used in the analysis of a multilayer ground is presented, and a number of practical sea-ice paths are evaluated numerically. Results are presented for the 0.1 to 10 MHz frequency range and consist of curves showing propagation loss as a function of distance for various ice thicknesses. It is shown that the variation of the attenuation function with distance and with frequency is significantly different than for the open ocean case. A range of frequencies over which path loss is predicted to be less than for seawater only is dependent on the path length and is shown to lie in the medium frequency range. Keywords: Ground waves(Electromagnetic); Arctic communication; Electromagnetic propagation over ice.
author2 NAVAL RESEARCH LAB WASHINGTON DC
format Text
author Kennedy,Edward J.
author_facet Kennedy,Edward J.
author_sort Kennedy,Edward J.
title Ground-Wave Path Loss Over Ice-Covered Sea at Frequencies between 0.1 and 10 MHz.
title_short Ground-Wave Path Loss Over Ice-Covered Sea at Frequencies between 0.1 and 10 MHz.
title_full Ground-Wave Path Loss Over Ice-Covered Sea at Frequencies between 0.1 and 10 MHz.
title_fullStr Ground-Wave Path Loss Over Ice-Covered Sea at Frequencies between 0.1 and 10 MHz.
title_full_unstemmed Ground-Wave Path Loss Over Ice-Covered Sea at Frequencies between 0.1 and 10 MHz.
title_sort ground-wave path loss over ice-covered sea at frequencies between 0.1 and 10 mhz.
publishDate 1987
url http://www.dtic.mil/docs/citations/ADA180819
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA180819
geographic Arctic
geographic_facet Arctic
genre Arctic
Ice
permafrost
Sea ice
genre_facet Arctic
Ice
permafrost
Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA180819
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766322716719185920