AToMS (Airborne Taxonomic Mapping System)
AToMS is an airborne high-resolution imaging instrumentation of CAO (Carnegie Airborne Observatory), a facility of the Carnegie Institution for Science. The CAO instruments are operated onboard a Dornier 228 aircraft with customized avionics, instrument facilities and sensor mounts. The CAO instrumentation is maintained in the Carnegie Institution's Department of Global Ecology on the campus of Stanford University, Stanford, CA, USA. 1) 2) 3) 4) 5)
Table 1: Some background on CAO
The CAO works by combining laser and spectrometer remote sensing technologies, along with high-tech inertial motion sensors to track the aircraft’s position and orientation to exacting tolerances. The laser technology, called LiDAR, measures the 3D structure of the vegetation and terrain. The spectrometers measure the way that sunlight reflects off vegetation, soils, and other ecosystem components, which yields chemical and physiological information.
The newly developed AToMS instrumentation package is regarded a next generation sensor suite (first flight in the summer of 2011). The system will provide higher resolution laser and spectroscopic information extending from the visible through the shortwave-infrared region of the spectrum. It will be operated from its new Dornier 228 aircraft. The dramatic increase in measurement capability provided by AToMS will provide a major leap forward for CAO science in support of Earth science and exploration, biological conservation, and resource policy development.
Figure 1: Photo of the Dornier 228 aircraft (image credit: Carnegie Institution)
AToMS instrumentation package:
The AToMS instrument suite was designed by Greg Asner of the Carnegie Institution and manufasctured by many sub-contractors. NASA/JPL (Jet Propulsion Laboratory), Pasadena, CA is the prime contractor for the VSWIR imaging spectrometer.
The AToMS instrument package is comprised of three custom-built instruments: 6)
1) VSWIR (Visible and Shortwave Infrared) imaging spectrometer, measuring reflected solar radiance from 380-2500 nm in 5 nm increments (> 400 bands); the spatial resolution is 0.5-2.0 m, depending on the flight altitude.
Table 2: Parameters of the AToMS instrument
Figure 2: Schematic view of the VSWIR imaging spectrometer (image credit: Carnegie Institution)
2) Multi-pulse waveform LiDAR (Light Detection and Ranging), a high-resolution waveform LiDAR system providing contiguous ground coverage and full three-dimensional imaging. The instrument measures up to 400,000 pulses/s with dual laser beams; 0.5-1.0 m spatial resolution.
Table 3: Parameters of the multi-pulse waveform LiDAR
Figure 3: Schematic view of the multi-pulse waveform LiDAR (image credit: Carnegie Institution)
3) VNIR (Visible Near Infrared) zoom imaging spectrometer, a high-fidelity imaging system providing contiguous spectral signatures of targets in VNIR. The instrument measures reflected solar radiance from 367-1060 nm in 5 nm increments; 0.5-1.0 m spatial resolution.
Table 4: Parameters of the VNIR instrument
Figure 4: Photo of the AToMS sensor package installed inside CAO (image credit: Carnegie Institution)
To interpret the new data stream coming from AToMS, the team has developed the world's first Spectranomics Database to link the phylogenetic organization of tropical plants to their spectroscopic and chemical signatures. The Spectranomics Database is a critical step required to advance regional and global biodiversity mapping efforts in the coming decades.
Some examples of past CAO observations:
The United Nations REDD (Reduce Emissions from Deforestation and Degradation) program requires high-resolution mapping of tropical forest carbon to support climate change mitigation. With a new integration of satellite imaging, airborne Light Detection and Ranging, and field plots, the CAO project mapped above-ground carbon stocks and emissions at 0.1 ha resolution over 4.3 million ha of the Peruvian Amazon, revealing variation at multiple scales due to geologic substrate, forest type, and land use.
Figure 5: High-resolution example of forest structure (Tambopata rainforest in Peru) as mapped by the CAO Alpha LiDAR (image credit: Carnegie Institution) 7)
Figure 6: CAO image of Santa Cruz Island, part of the Channel Islands off the coast of California, observed in 2009 (image credit: Carnegie Institution)
5) Jeff Tollefson, “A new eye on biodiversity - Airborne observatory will use chemical clues to map and assess tropical ecosystems,” Nature, Vol. 474, pp. 13-14, June 1, 2011, URL: http://www.nature.com/news/2011/110601/full/474013a.html
6) Information provided by Gregory P. Asner of Carnegie Institution's Department of Global Ecology, Stanford University
The information compiled and edited in this article was provided by Herbert J. Kramer from his documentation of: "Observation of the Earth and Its Environment: Survey of Missions and Sensors" (Springer Verlag) as well as many other sources after the publication of the 4th edition in 2002. - Comments and corrections to this article are always welcome for further updates.