CAMEX-3 Atmospheric Emitted Radiance Interferometer (AERI) Table of Contents
The Atmospheric Emitted Radiance Interferometer (AERI) is a two band BOMEM-100 Michelson interferometer consisting of two detectors (5-20 um and 3-5 um), scene imaging scan mirror, and a two point calibration system. Every ten minutes a spectrum at one wavenumber resolution is produced from 3-20 um with an absolute accuracy of 10f ambient radiance determined by intercomparisons between other AERI instrument and a NIST blackbody reference. AERI measured atmospheric radiances can be used to retrieve:
AERI radiances have several useful scientific purposes for the study of the atmosphere. Firstly AERI provides absolutely calibrated radiances which can be used for forward calculation comparisons of radiosonde and LIDAR profiles. This provides a reference to the airborne and ground based remote sensing instruments used in CAMEX-3, which profile atmospheric state. Secondly AERI radiances contain valuable temperature and water vapor information which can be used to retrieve planetary boundary layer thermodynamics. This information is found on the AERI Engineering page. Data Naming Conventions and Data FormatAERI data are located in three directories: aerirad, aerigoes and aerisonde. aerirad
aerigoes
aerisonde
AERI radiance, retrieval and sounding data are stored in netcdf (.cdf) format. Libraries to read this format from Unidata are available for Fortran and C. This format can easily be read in both IDL and Matlab. Additionally, all of the images: radiance (as in aerirad/browse above), mixing ratio/potential temperature (in the aerigoes/data directory) and the skew-T log P diagrams (in aerisonde) are available on line at: https://camex.nsstc.nasa.gov/camex3/cmx3aeri/ Other Andros Island Sonde DataThere was another rawinsonde dataset collected at Andros Island during the CAMEX-3 campaign. Collected by the Wallops Island Test Group, it is contained in the dataset CAMEX-3 Andros Island Radiosonde/Rawindsonde Data. Order by contacting GHRC User Services. Selected ReferencesThe AERI instrument and software has several references available. The most pertinent to the temperature and moisture retrieval algorithm are: Feltz, W. F., W. L. Smith, R. O. Knuteson, H. R. Revercomb, H. B. Howell, Harold H. Woolf, 1998: Meteorological Applications of Temperature and Water Vapor Retrievals from the Ground-Based Atmospheric Emitted Radiance Interferometer (AERI). Jour. Appl. Meteor., 37, 857-875. Smith, W. L., W. F. Feltz, R. O. Knuteson, H. R. Revercomb, H. B. Howell, Harold H. Woolf, 1998: The Retrieval of Planetary Boundary Layer Structure Using Ground Based Infrared Spectral Radiance Measurements. Journal of Atmospheric and Oceanic Technology, 16, 323-333. Contact InformationTo order these data or for further information, please contact:
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