In this presentation we will focus on the results obtained during CASPER-West with the CTV, the modified sea-skimming target drone we outfitted with essentially the same proven turbulence instrumentation as that of the TO. The CTV is uniquely equipped with an active height-keeping system using a controllable “wing” (elevator) to maintain its radar altitude as low as 9 m during long flux-runs while towed from the TO flying 300 m above. The CTV was mostly operated at 10 m and at several levels within the surface layer along the CASPER-West EM propagation path defined by the shore site at Pt Mugu and the R/P FLIP moored roughly 50 km offshore . The CTV also flew repeated vertical saw-tooth pattern in and out of the refractive duct and deeper saw-tooth pattern were flown by the TO that together provided a quasi-instantaneous high-resolution depiction of the vertical structure of the propagation environment throughout the surface to well above the MABL.
We will briefly describe the TO and CTV instrumentation and then present air-sea interaction and boundary layer structure results from select fights along the propagation path. We will particularly focus on results obtained from flights during weak, moderate, and strong Santa Ana wind and a flight during strong northwest wind where some unusual perturbations to the environment that may be attributed to island wake effects were observed. The range-dependent EM propagation loss characteristics in these different conditions are explored by analysis of the data of a receiving antennas array on the FLIP corresponding the frequency of the emitted signals by the two X-Band oscillators on the TO and CTV.