Abstract
Initial observations with the Global Ultraviolet Imager (GUVI) in the NASA TIMED satellite mission
Space Science Applications Laboratory, Aerospace Corporation, El Segundo, California, USA
Applied Physics Laboratory, Johns Hopkins University, Laurel, Maryland, USA
University of Colorado, Boulder, Colorado, USA
University of Alaska, Fairbanks, Alaska, USA
Southwest Research Institute, San Antonio, Texas, USA
Applied Physics Laboratory, Johns Hopkins University, Laurel, Maryland, USA
Applied Physics Laboratory, Johns Hopkins University, Laurel, Maryland, USA
E.O. Hulburt Center for Space Research, Naval Research Laboratory, Washington D.C., USA
Applied Physics Laboratory, Johns Hopkins University, Laurel, Maryland, USA
Applied Physics Laboratory, Johns Hopkins University, Laurel, Maryland, USA
Applied Physics Laboratory, Johns Hopkins University, Laurel, Maryland, USA
Space Science Applications Laboratory, Aerospace Corporation, El Segundo, California, USA
Computational Physics, Inc, Springfield, Virginia, USA
Utah State University, Logan, Utah, USA
Space Science Applications Laboratory, Aerospace Corporation, El Segundo, California, USA
Applied Physics Laboratory, Johns Hopkins University, Laurel, Maryland, USA
Applied Physics Laboratory, Johns Hopkins University, Laurel, Maryland, USA
The Global Ultraviolet Imager (GUVI) instrument carried aboard the NASA TIMED satellite measures the spectral radiance of
the Earth's far ultraviolet airglow in the spectral region from 120 to 180 nm using a cross-track scanning spectrometer design.
Continuous operation of the instrument provides images of the Earth's disk and limb in five selectable spectral bands. Also,
spectra at fixed scanning mirror position can be obtained. Initial results demonstrate the quantitative functionality of the
instrument for studies of the Earth's dayglow, aurora, and ionosphere. Moreover, through forward modeling, the abundance of
the major constituents of the thermosphere, O, N2, and O2 and thermospheric temperatures can be retrieved from observations of the limb radiance. Variations of the column O/N2 ratio can be deduced from sunlit disk observations. In regions of auroral precipitation not only can the aurora regions be
geographically located and the auroral boundaries identified, but also the energy flux Q, the characteristic energy Eo, and a parameter fo that scales the abundance of neutral atomic oxygen can be derived. Radiance due to radiative recombination in the ionospheric
F region is evident from both dayside and nightside observations of the Earth's limb and disk, respectively. Regions of depleted
F-region electron density are evident in the tropical Appleton anomaly regions, associated with so-called ionospheric “bubbles.”
Access to the GUVI data is provided through the GUVI website
Received 1 March 2003; accepted 3 October 2003; published 23 December 2003.
Citation: (2003), Initial observations with the Global Ultraviolet Imager (GUVI) in the NASA TIMED satellite mission, J. Geophys. Res., 108(A12), 1451, doi:10.1029/2003JA009918.
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