Sound Source Depth Estimation Based on Multipath Time Delay in Deep Water

2018 ◽  
Vol 104 (2) ◽  
pp. 363-368 ◽  
Author(s):  
Qiulong Yang ◽  
Kunde Yang
2021 ◽  
Vol 149 (1) ◽  
pp. 524-539
Author(s):  
Hui Li ◽  
Zhezhen Xu ◽  
Kunde Yang ◽  
Rui Duan

2020 ◽  
Vol 56 (6) ◽  
pp. 4856-4871
Author(s):  
Rui Duan ◽  
Kunde Yang ◽  
Feiyun Wu ◽  
Yuanliang Ma

2016 ◽  
Vol 33 (12) ◽  
pp. 124302 ◽  
Author(s):  
Kun-De Yang ◽  
Qiu-Long Yang ◽  
Xiao-Le Guo ◽  
Ran Cao

2019 ◽  
Vol 145 (2) ◽  
pp. 903-916 ◽  
Author(s):  
Rui Duan ◽  
Kunde Yang ◽  
Hui Li ◽  
Qiulong Yang ◽  
Feiyun Wu ◽  
...  

1984 ◽  
Vol 74 (5) ◽  
pp. 1623-1643
Author(s):  
Falguni Roy

Abstract A depth estimation procedure has been described which essentially attempts to identify depth phases by analyzing multi-station waveform data (hereafter called level II data) in various ways including deconvolution, prediction error filtering, and spectral analysis of the signals. In the absence of such observable phases, other methods based on S-P, ScS-P, and SKS-P travel times are tried to get an estimate of the source depth. The procedure was applied to waveform data collected from 31 globally distributed stations for the period between 1 and 15 October 1980. The digital data were analyzed at the temporary data center facilities of the National Defense Research Institute, Stockholm, Sweden. During this period, a total number of 162 events in the magnitude range 3.5 to 6.2 were defined by analyzing first arrival time data (hereafter called level I data) alone. For 120 of these events, it was possible to estimate depths using the present procedure. The applicability of the procedure was found to be 100 per cent for the events with mb > 4.8 and 88 per cent for the events with mb > 4. A comparison of level I depths and level II depths (the depths as obtained from level I and level II data, respectively) with that of the United States Geological Survey estimates indicated that it will be necessary to have at least one local station (Δ < 10°) among the level I data to obtain reasonable depth estimates from such data alone. Further, it has been shown that S wave travel times could be successfully utilized for the estimation of source depth.


2017 ◽  
Vol 170 ◽  
pp. 169-176 ◽  
Author(s):  
Dhany Arifianto ◽  
Wirawan ◽  
B.T. Atmaja ◽  
Tutug Dhanardhono ◽  
Saptian A. Rahman

2018 ◽  
Vol 143 (1) ◽  
pp. EL8-EL12 ◽  
Author(s):  
Kunde Yang ◽  
Liya Xu ◽  
Qiulong Yang ◽  
Rui Duan

2005 ◽  
Vol 117 (4) ◽  
pp. 2463-2464
Author(s):  
William Lee ◽  
Yung Lee

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