Marine Boundary Layer Refractive Effects in the Infrared
Abstract
An experiment was conducted to determine whether ducting phenomena (gradients in refractivity) occur close to the ocean surface at infrared wavelengths. A CO2 laser beam (10.6 microns) was transmitted and received over an 8.5 km path in San Diego Bay. For the cases investigated (sea warmer than the air), the results of the study indicate that for air temperature gradients less than 1 C/meter, the distance to the infrared horizon was only 60% of the normal geometrical horizon.
Document Details
- Document Type
- Technical Report
- Publication Date
- Oct 01, 1994
- Accession Number
- ADA285717
Entities
People
- H. G. Hughes
- H. V. Hitney
- R. Feinberg
Organizations
- Naval Command, Control and Ocean Surveillance Center