In Larry Milberry’s text on CAELarry Milberry’s text on CAE (Canadian Aviation Electronics), in a discussion of the development of digital radar land mass simulation (DRLMS) for the Dutch Lynx mission simulator, far-shore brightening is described as “coastlines [appearing] brighter, because there are two different radar returns—one directly from the radar scanning the coast, the other caused by the radar reflecting off the water onto the shore.”(p.240)
Now I know this would seem to answer my question, but I have had difficulty finding any other definitions of the phenomenon.
Specifically, I am wondering if there are other important details about far-shore brightening that are being missed?
- Is far-shore brightening specific to aircraft radar due to the high angle relative to the ground? Or is far-shore brightening also a marine radar and land-based radar phenomenon?
- Is far-shore brightening common on contemporary radar? Or has there been advancements to compensate?
- Is far-shore brightening helpful when reading the radar?
If you might be able to direct me to further resources that would be very helpful.