DocumentCode
2828739
Title
Time Difference Raytrace Method For Ranging And Sound Channel Probing
Author
Maltz, F.H.
Author_Institution
Naval Underwater Systems Center, New London, CT, USA
fYear
1983
fDate
Aug. 29 1983-Sept. 1 1983
Firstpage
42
Lastpage
44
Abstract
A method for time delay ranging in the deep sound channel is outlined here. The method is based on modeling sound channel SSP by an N-layer model. The parameters of the model are reference sound speed
. layer thickness
Z and sound speed gradient vector
. For ranging purposes, it is only necessary to determine the composite parameter(
). As shown, this can be done by differential ray trace or by using two distinct bearing angles. Another alternative is to use an analytical profile and to differentiate axial range with respect to the vertical arrival angle
. The same methodology is proposed to solve the inverse problem, namely the gradient set is obtained from
independent observations of the phase gradient parameter(
). The explicit transformation of SSP to phase gradient for an axial configuration of sources and receivers for the layered model is outlined. A simple transposition method is discussed to obtain an off-axis configuration of source/receiver allocations. All the results presented here have been restricted to ray trajectories having a single upper and single lower rapath loop. This propagation mode is generally associated with first convergence zone ranges, that is to say ranges of the order of 50km.
. layer thickness
Z and sound speed gradient vector
. For ranging purposes, it is only necessary to determine the composite parameter(
). As shown, this can be done by differential ray trace or by using two distinct bearing angles. Another alternative is to use an analytical profile and to differentiate axial range with respect to the vertical arrival angle
. The same methodology is proposed to solve the inverse problem, namely the gradient set is obtained from
independent observations of the phase gradient parameter(
). The explicit transformation of SSP to phase gradient for an axial configuration of sources and receivers for the layered model is outlined. A simple transposition method is discussed to obtain an off-axis configuration of source/receiver allocations. All the results presented here have been restricted to ray trajectories having a single upper and single lower rapath loop. This propagation mode is generally associated with first convergence zone ranges, that is to say ranges of the order of 50km.Keywords
Delay effects; Delay estimation; Inverse problems; Phase estimation; Phase measurement; Remote sensing; Sea measurements; Time difference of arrival; Time measurement; Velocity measurement;
fLanguage
English
Publisher
ieee
Conference_Titel
OCEANS '83, Proceedings
Conference_Location
San Francisco, CA, USA
Type
conf
DOI
10.1109/OCEANS.1983.1152121
Filename
1152121
Link To Document