Navigation by Moon Doppler Effect

As a back-up navigation method for Polaris submarines, the feasibility of moon doppler navigation on abistatic basis is investigated. The problem is that of finding the latitude and longitude of a vessel by measuring doppler shift and time rate of change of doppler shift in radio waves transmitted f...

Full description

Bibliographic Details
Main Author: Corum, C. E.
Other Authors: NAVAL RESEARCH LAB WASHINGTON DC
Format: Text
Language:English
Published: 1959
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA511170
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA511170
id ftdtic:ADA511170
record_format openpolar
spelling ftdtic:ADA511170 2023-05-15T17:47:04+02:00 Navigation by Moon Doppler Effect Corum, C. E. NAVAL RESEARCH LAB WASHINGTON DC 1959-01-20 text/html http://www.dtic.mil/docs/citations/ADA511170 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA511170 en eng http://www.dtic.mil/docs/citations/ADA511170 Approved for public release; distribution is unlimited. DTIC Astronomy Acoustics *MOON *DOPPLER NAVIGATION *DOPPLER EFFECT FINITE DIFFERENCE THEORY ERRORS NUMERICAL METHODS AND PROCEDURES DOPPLER SYSTEMS RADIO WAVES NORWEGIAN SEA LATITUDE LONGITUDE PROBABILITY MEASUREMENT FREQUENCY PROPAGATION PROPAGATION EFFECTS Text 1959 ftdtic 2016-02-22T22:35:53Z As a back-up navigation method for Polaris submarines, the feasibility of moon doppler navigation on abistatic basis is investigated. The problem is that of finding the latitude and longitude of a vessel by measuring doppler shift and time rate of change of doppler shift in radio waves transmitted from a fixed site and reflected from the moon. For a prescribed navigation accuracy, one must determine the necessary precision in measuring doppler frequency and time rate of change of doppler frequency. A sample calculation is made for a location on the western edge of the Norwegian Sea, and it is found that if the probable error in latitude is specified to be 0.8 naut mi and the probable error in longitude to be 1.3 naut mi, the probable error which can be allowed in doppler shift is 0.796 cps and the permissible probable error in time rate of change of doppler shift is 9.511 x 10' cpsps, with a transmitted frequency of 2200 Mc. The calculated value for doppler frequency was 2459 cps, and that for doppler rate was 0.1381 cpsps. This means that doppler frequency must be measured to an accuracy of 0.0324 percent and doppler rate to an accuracy of 0.0689 percent, for this particular example. The measurement of doppler frequency seems within the realm of technical capability in the near future. The accuracy of the measurement of doppler rate is still in question. However, it appears that the rate can be computed within the required accuracy by fitting an approximate analytical expression to the set of points representing the measured doppler shift and differentiating the expression, or by using finite difference methods with the observed data to get the time derivative. Propagation effects due to variation of index of refraction in the atmosphere have not been taken into account. These effects may be important, and should probably be the subject of investigation in the near future. BuOrd no. SP 271-12. Text Norwegian Sea Defense Technical Information Center: DTIC Technical Reports database Norwegian Sea
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Astronomy
Acoustics
*MOON
*DOPPLER NAVIGATION
*DOPPLER EFFECT
FINITE DIFFERENCE THEORY
ERRORS
NUMERICAL METHODS AND PROCEDURES
DOPPLER SYSTEMS
RADIO WAVES
NORWEGIAN SEA
LATITUDE
LONGITUDE
PROBABILITY
MEASUREMENT
FREQUENCY
PROPAGATION
PROPAGATION EFFECTS
spellingShingle Astronomy
Acoustics
*MOON
*DOPPLER NAVIGATION
*DOPPLER EFFECT
FINITE DIFFERENCE THEORY
ERRORS
NUMERICAL METHODS AND PROCEDURES
DOPPLER SYSTEMS
RADIO WAVES
NORWEGIAN SEA
LATITUDE
LONGITUDE
PROBABILITY
MEASUREMENT
FREQUENCY
PROPAGATION
PROPAGATION EFFECTS
Corum, C. E.
Navigation by Moon Doppler Effect
topic_facet Astronomy
Acoustics
*MOON
*DOPPLER NAVIGATION
*DOPPLER EFFECT
FINITE DIFFERENCE THEORY
ERRORS
NUMERICAL METHODS AND PROCEDURES
DOPPLER SYSTEMS
RADIO WAVES
NORWEGIAN SEA
LATITUDE
LONGITUDE
PROBABILITY
MEASUREMENT
FREQUENCY
PROPAGATION
PROPAGATION EFFECTS
description As a back-up navigation method for Polaris submarines, the feasibility of moon doppler navigation on abistatic basis is investigated. The problem is that of finding the latitude and longitude of a vessel by measuring doppler shift and time rate of change of doppler shift in radio waves transmitted from a fixed site and reflected from the moon. For a prescribed navigation accuracy, one must determine the necessary precision in measuring doppler frequency and time rate of change of doppler frequency. A sample calculation is made for a location on the western edge of the Norwegian Sea, and it is found that if the probable error in latitude is specified to be 0.8 naut mi and the probable error in longitude to be 1.3 naut mi, the probable error which can be allowed in doppler shift is 0.796 cps and the permissible probable error in time rate of change of doppler shift is 9.511 x 10' cpsps, with a transmitted frequency of 2200 Mc. The calculated value for doppler frequency was 2459 cps, and that for doppler rate was 0.1381 cpsps. This means that doppler frequency must be measured to an accuracy of 0.0324 percent and doppler rate to an accuracy of 0.0689 percent, for this particular example. The measurement of doppler frequency seems within the realm of technical capability in the near future. The accuracy of the measurement of doppler rate is still in question. However, it appears that the rate can be computed within the required accuracy by fitting an approximate analytical expression to the set of points representing the measured doppler shift and differentiating the expression, or by using finite difference methods with the observed data to get the time derivative. Propagation effects due to variation of index of refraction in the atmosphere have not been taken into account. These effects may be important, and should probably be the subject of investigation in the near future. BuOrd no. SP 271-12.
author2 NAVAL RESEARCH LAB WASHINGTON DC
format Text
author Corum, C. E.
author_facet Corum, C. E.
author_sort Corum, C. E.
title Navigation by Moon Doppler Effect
title_short Navigation by Moon Doppler Effect
title_full Navigation by Moon Doppler Effect
title_fullStr Navigation by Moon Doppler Effect
title_full_unstemmed Navigation by Moon Doppler Effect
title_sort navigation by moon doppler effect
publishDate 1959
url http://www.dtic.mil/docs/citations/ADA511170
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA511170
geographic Norwegian Sea
geographic_facet Norwegian Sea
genre Norwegian Sea
genre_facet Norwegian Sea
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA511170
op_rights Approved for public release; distribution is unlimited.
_version_ 1766151372842991616