Ozone Cues Mitigate Reflected Downwelling Radiance in LWIR Absorption-Based Ranging

Passive long-wave infrared (LWIR) absorption-based ranging relies on atmospheric absorption to estimate distances to objects from their emitted thermal radiation. First demonstrated decades ago for objects much hotter than the air and recently extended to scenes with low temperature variations, this ranging has depended on reflected radiance being negligible. Downwelling radiance is especially problematic, sometimes causing large inaccuracies. In two new ranging methods, we use characteristic features from ozone absorption to estimate the contribution of reflected downwelling radiance. The quadspectral method gives a simple closed-form range estimate from four narrowband measurements, two at a water vapor absorption line and two at an ozone absorption line. The hyperspectral method uses a broader spectral range to improve accuracy while also providing estimates of temperature, emissivity profiles, and contributions of downwelling from a collection of zenith angles. Experimental results demonstrate improved ranging accuracy, in one case reducing error from over 100 m when reflected light is not modeled to 6.8 m with the quadspectral method and 1.2 m with the hyperspectral method.

Absorption-Based, Passive Range Imaging from Hyperspectral Thermal Measurements

Passive hyperspectral long-wave infrared measurements are remarkably informative about the surroundings, such as remote object material composition, temperature, and range; and air temperature and gas concentrations. Remote object material and temperature determine the spectrum of thermal radiance, and range, air temperature, and gas concentrations determine how this spectrum is modified by propagation to the sensor. We computationally separate these phenomena, introducing a novel passive range imaging method based on atmospheric absorption of ambient thermal radiance. Previously demonstrated passive absorption-based ranging methods assume hot and highly emitting objects. However, the temperature variation in natural scenes is usually low, making range imaging challenging. Our method benefits from explicit consideration of air emission and parametric modeling of atmospheric absorption. To mitigate noise in low-contrast scenarios, we jointly estimate range and intrinsic object properties by exploiting a variety of absorption lines spread over the infrared spectrum. Along with Monte Carlo simulations that demonstrate the importance of regularization, temperature differentials, and availability of many spectral bands, we apply this method to long-wave infrared (8--13 $\mu$m) hyperspectral image data acquired from natural scenes with no active illumination. Range features from 15m to 150m are recovered, with good qualitative match to unaligned lidar data.