Airborne Multi-angle Imaging SpectroRadiometer (AirMISR) Data from the Bartlett 2003 CampaignEntry ID: AIRMISR_BARTLETT_2003
Abstract: The AIRMISR_BARTLETT_2003 data were acquired during a flight over the Bartlett Experimental Forest, New Hampshire, USA, target as part of the AirMISR deployments from the Wallops Flight Facility during the August 2003 campaign. This particular flight took place on August 24, 2003. The Jet Propulsion Laboratory (JPL) in Pasadena, California provided the data.
There were a total of two ... runs during this flight. A run comprises data collected from nine view angles acquired on a fixed flight azimuth angle. Each data file from one run contains either: a) Level 1B1 Radiometric product from one of the 9 camera angles or b) Level 1B2 Georectified radiance product from one of the 9 camera angles. Browse images in PNG format are available for the Level 1B1 product and browse images in JPEG format are available for the Level 1B2 product.
The Airborne Multi-angle Imaging SpectroRadiometer (AirMISR) is an airborne instrument for obtaining multi-angle imagery similar to that of the satellite-borne Multi-angle Imaging SpectroRadiometer (MISR) instrument, which is designed to contribute to studies of the Earth's ecology and climate. AirMISR flies on the NASA ER-2 aircraft. The Jet Propulsion Laboratory in Pasadena, California built the instrument for NASA.
Unlike the satellite-borne MISR instrument, which has nine cameras oriented at various angles, AirMISR uses a single camera in a pivoting gimbal mount. A data run by the ER-2 aircraft is divided into nine segments, each with the camera positioned to a MISR look angle. The gimbal rotates between successive segments, such that each segment acquires data over the same area on the ground as the previous segment. This process is repeated until all nine angles of the target area are collected. The swath width, which varies from 11 km in the nadir to 32 km at the most oblique angle, is governed by the camera's instantaneous field-of-view of 7 meters cross-track x 6 meters along-track in the nadir view and 21 meters x 55 meters at the most oblique angle. The along-track image length at each angle is dictated by the timing required to obtain overlap imagery at all angles, and varies from about 9 km in the nadir to 26 km at the most oblique angle. Thus, the nadir image dictates the area of overlap that is obtained from all nine angles. A complete flight run takes approximately 13 minutes.
The 9 camera viewing angles are:
0 degrees or nadir
26.1 degrees, fore and aft
45.6 degrees, fore and aft
60.0 degrees, fore and aft
70.5 degrees, fore and aft
For each of the camera angles, images are obtained at 4 spectral bands. The spectral bands can be used to identify vegetation and aerosols, estimate surface reflectance and ocean color studies. The center wavelengths of the 4 spectral bands are:
443 nanometers, blue
555 nanometers, green
670 nanometers, red
865 nanometers, near-infrared
Two types of AirMISR data products are available - the Level 1 Radiometric product (L1B1) and the Level 1 Georectified radiance product (L1B2).
The Level 1 Radiometric product contains data that are scaled to convert the digital output of the cameras to radiances and are conditioned to remove instrument-dependent effects. Additionally, all radiances are adjusted to remove slight spectral sensitivity differences among the detector elements of each spectral band. These data have a 7-meter spatial resolution at nadir and around 30-meter at the most oblique 70.5 degree angles.
The Level 1 Georectified radiance product contains the Level 1 radiometric product resampled to a 27.5 meter spatial resolution and mapped into a standard Universal Transverse Mercator (UTM) map projection. Initially the data are registered to each camera angle and to the ground. This processing is necessary because the nine views of each point on the ground are not acquired simultaneously.
Once the map grid center points are located in the AirMISR imagery through the process of georectification, a radiance value obtained from the surrounding AirMISR pixels is assigned to that map grid center. Bilinear interpolation is used as the basis for computing the new radiance. A UTM grid point falling somewhere in the image data will have up to 4 surrounding points. The bilinear interpolated value is obtained using the fractional distance of the interpolation point in the cross-track direction and the fractional distance in the along-track direction.
Start Date: 2003-08-24Stop Date: 2003-08-24
Latitude Resolution: 27.5 Meter
Longitude Resolution: 27.5 Meter
Horizontal Resolution Range: 1 meter - < 30 meters
ISO Topic Category
Data Set Progress
Phone: (818) 354-4956
Email: Carol.J.Bruegge at jpl.nasa.gov
Jet Propulsion Laboratory Mail Stop 169-237 4800 Oak Grove Drive
Province or State: CA
Postal Code: 91109
Role: DIF AUTHOR
Email: support-asdc at earthdata.nasa.gov
NASA Langley Atmospheric Science Data Center User and Data Services NASA Langley Research Center Mail Stop 157D
Province or State: VA
Postal Code: 23681-2199
Bruegge, Carol J., Wedad A. Abdou, Nadine L. Chrien, Barbara J. Gaitley
(1998). AirMISR spectral and radiometric performance studies. In Earth
Observing System III, Proc. SPIE 3439, San Diego, CA, 19-21 July.
Bruegge, C. J., N. L. Chrien, R. A. Kahn, J. V. Martonchik, David Diner
(1998). MISR radiometric uncertainty analyses and their ... utilization
within geophysical retrievals. Conference issue: New Developments and
Applications in Optical Radiometry (NEWRAD '97), Metrologia., 35, 571-579.
Bruegge, C. J., V. G. Duval, N. L. Chrien, R. P. Korechoff, B. J. Gaitley,
and E. B. Hochberg (1998). MISR prelaunch instrument calibration and
characterization results. IEEE Trans. Geosci. Rem. Sens., Vol. 36, pp.
Chrien, Nadine L., Carol J. Bruegge, Barbara J. Gaitley (2000). AirMISR
laboratory calibration and in-flight performance results. Submitted
to Remote Sens. Environment, December 1998.
Diner, David J., et al. (1998). The Airborne Multi-Angle Imaging
SpectroRadiometer (AirMISR): Instrument Description and First Results.
IEEE Trans. Geosci. Rem. Sens., Vol. 36, No. 4.
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Creation and Review Dates
DIF Creation Date: 2004-07-19
Last DIF Revision Date: 2014-04-07