Optical waves propagating through atmospheric turbulence develop spatial and temporal variations in their phase. For sufficiently strong turbulence, these phase differences can lead to interference in the propagating wave and the formation of branch points; positions of zero amplitude. Under the assumption of a layered turbulence model, we show that these branch points can be used to estimate the number and velocities of atmospheric layers. We describe how to carry out this estimation process and demonstrate its robustness in the presence of sensor noise.
Download full-text PDF |
Source |
---|---|
http://dx.doi.org/10.1364/OE.18.022377 | DOI Listing |
Enter search terms and have AI summaries delivered each week - change queries or unsubscribe any time!