1 / 13

Nominal SVP (Sound Velocity Profile)

winter. Speed of Sound. 4850ft/s 4900 ft/s 4950 ft/s 5000ft/s. Surface Layer. 300 600 3000 6000 9000. Seasonal Thermocline. Main Thermocline. Deep Isothermal Layer. Nominal SVP (Sound Velocity Profile). “Layer”.

Download Presentation

Nominal SVP (Sound Velocity Profile)

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. winter Speed of Sound 4850ft/s 4900 ft/s 4950 ft/s 5000ft/s Surface Layer 300 600 3000 6000 9000 Seasonal Thermocline Main Thermocline Deep Isothermal Layer Nominal SVP (Sound Velocity Profile) “Layer”

  2. Typical SVP

  3. c  z  c  z  c z  Gradients and Bending Iso-speed positive negative

  4. Surface Duct – Surface Shadow Zone SVP positive SVP negative

  5. Surface Shadow Zone Implications Originally called the “afternoon effect”

  6. Convergence Zone Depth Excess > 300 fathoms

  7. CZ Effect on Transmission Loss (TL) TL (dB)

  8. Deep Shadow Zones • BD = 17(LD)1/2 if LD < 60m. • BD = LD + 60m if LD > 60m.

  9. Deep sound channel range Sound speed depth

  10. Mixed Layer Example D = 40 m L = 100 m C1 = 1500 m/s g = 0.017 s-1 • Find sound speed at S and at bottom of layer • Angle of the rays at the source • Angle of the rays at the surface • Radius of curvature of the ray • Skip distance , X S

  11. Mixed Layer

  12. x2 x1 R c1 z1 q1 z2 c2 q2 Positive gradient, g Summary

More Related