RUSSIAN JOURNAL OF EARTH SCIENCES,  VOL. 19, ES5003, doi:10.2205/2019ES000667, 2019
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Far fields of internal gravity waves from a source moving in the ocean with an arbitrary buoyancy frequency distribution
Figures
- Figure 1.  Brunt-Vaisala frequency distribution.
 
- Figure 2.  Function $\mu' (\nu)$ at different values $M$: (a) – $M...
 
- Figure 3.  Dependences $q_i (M)$ and its approximation: line 1 –...
 
- Figure 4.  Dependences $\varphi_i (M)$: line 1 – $\varphi_1 (M)$,...
 
- Figure 5.  Elevation $\eta$ at $y=0.25$ km, $M=0.4 < M_0$.
 
- Figure 6.  Elevation $\eta$ at $y = 3$ km, $M=0.4 < M_0$.
 
- Figure 7.  Elevation $\eta$ at $y = 3$ km, $M = M_0$.
 
- Figure 8.  Elevation $\eta$ at $y = 3$ km, $M=0.7 > M_0$.
 
- Figure 9.  Elevation $\eta$ at $y = 3$ km, $M=1.7 > M_0$.
 
- Figure 10.  Elevation $\eta$ at $\xi = 1$ km, $M=0.4 < M_0$.
 
- Figure 11.  Elevation $\eta$ at $\xi = 20$ km, $M=1.7 > M_0$.
 
Tables
- Table 1.  Wave Fronts Positions Along $x$-axis for the Different Values...
 
- Table 2.  Wave Fronts Positions Along $y$-axis for the Different Values...
 
               
 
Citation: Bulatov V. V., Yu. V. Vladimirov, I. Yu. Vladimirov (2019), Far fields of internal gravity waves from a source moving in the ocean with an arbitrary buoyancy frequency distribution, Russ. J. Earth Sci., 19, ES5003, doi:10.2205/2019ES000667.
 
Copyright  2019  by the  Geophysical Center RAS.
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