G. Thulllier et al., The absolute solar spectral irradiance from 200 to 2500 nm as measured by the SOLSPEC spectrometer with the ATLAS and EURECA missions, PHYS CH P C, 25(5-6), 2000, pp. 375-377
Citations number
12
Categorie Soggetti
Earth Sciences
Journal title
PHYSICS AND CHEMISTRY OF THE EARTH PART C-SOLAR-TERRESTIAL AND PLANETARY SCIENCE
The SOLSPEC instrument measures the absolute solar spectral irradiance from
200 to 2500 nn. The instrument flew in March 1992, March 1993 and November
1994 with the three ATLAS missions during 10 days. SOSP is the spare unit
of SOLSPEC. It flew on the EURECA platform from ii August 1992 to May 1993.
SOLSPEC and SOSP are made of three spectrometers and contains several lamp
s allowing to check in flight, the instrument stability and its wavelength
scale.
These two units have an identical design and are made of the same component
s. However, their detectors have different performance leading to a SOSP re
sponsivity smaller than the SOLSPEC responsivity. As during the ATLAS missi
ons two other spectrometers were also observing in the UV and near visible
domain, we took advantage of this situation by choosing SOLSPEC for the thr
ee ATLAS missions. Afterward, it appeared that it was also the good choice
for the IR channel of SOSP on board EURECA.
The calibration of the instrument is performed with the blackbody of the He
idelberg observatory (Mandel et al., 1998). Its temperature is adjusted as
a function of the wavelength domain, ranging from 3000 K for UV calibration
, down to 2700 K for the IR spectrometer calibration. The blackbody tempera
ture is measured with a pyrometer calibrated by the Physikalisch-Technische
Bundesanstalt (PTB) of Berlin (Germany). The mean accuracy of the solar ir
radiance is estimated to be 2 to 3% in UV and 2% in the visible and infrare
d domains. In details, it depends on the spectral interval being better in
the middle of each spectral domain.
We shall present the best data obtained during the ATLAS and EURECA mission
s, e.g., UV and visible spectra from the three ATLAS missions and the IR re
sults from EURECA.
The duration of each ATLAS mission does not allow study of the solar variab
ility. This is why the best spectra are selected. This selection is based o
n several criteria including the thermal conditions, stability of the point
ing, linearity of the measurements, stability of the wavelength scale, posi
tion of the Sun in the field of view and tangent height of the line of sigh
t observations greater than 100 km. The selected spectra are averaged after
ward. A similar procedure was also applied to the SOSP infrared data becaus
e the solar variability in this domain is very small and is not detectable
with SOSP. Special care was dedicated to this channel due to the variable r
esponsivity in the field of view. Spectra which were not measured in the co
ndition of the laboratory calibration, were eliminated. (C) 2000 Elsevier S
cience Ltd. All rights reserved.