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Article Images
Monitoring ozone with GOME-2
 
12 July 2006

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Underneath the thermal insulation cover there is a complex set of telescopes and prisms through which incoming light is initially separated into four main bandwidths. Different gases in the atmosphere absorb different wavelengths of light. The GOME-2 spectrometer is used to split the light into different wavelengths to reveal absorption lines, which correspond to certain gases present the observed sample. GOME-2 covers the 240-790 nm wavelength regions, i.e. wavelengths covering ultraviolet and visible light.

On the side of the GOME-2 instrument that faces the Earth, a mirror, which scans a swath on the surface of the Earth 1920 kilometres x 40 kilometres, directs light reflected from the Earth's atmosphere into a telescope. Behind the entrance slit, the light is bounced around by a number of mirrors before being directed through a quartz prism. The prism separates the light into four bands (red, green, blue and ultraviolet). These four beams are then split further by 'holographic gratings' to resolve the light to 0.5 nm wavelengths and better.

The three large boxes shown in the animation house the scan mirror and electronics; the one at the bottom left of the image holds the scan mirror, the one in mid-right holds the power lines, and the larger one to the back-right holds the data control unit where the data is prepared and downlinked to the ground stations.

Periodically, the scan mirror is pointed towards the black box on the right for calibration purposes; here light is picked up directly from the Sun and used as a reference.

Credits: ESA - AOES Medialab

 
 
GOME-2 data products
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GOME-2 will provide data on profiles of atmospheric ozone, nitrogen dioxide, and sulphur dioxide, as well as other trace gases in the atmosphere. It will also measure harmful ultraviolet light penetrating the atmosphere.

Credits: ESA - AOES Medialab
 
 
GOME-2 observation principle
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As solar radiation reaches the Earth's atmosphere and surface a certain percentage is reflected or backscattered out to space. The degree to which incident light is backscattered depends on the albedo of the surface the light encounters, for example, clouds in the atmosphere have a high albedo so a large proportion of sunlight is reflected back.

GOME-2 is able determine amounts of certain gases present in the atmosphere through the principles of spectrometry, where, in incoming light is split into its spectral components to reveal absorption lines, which correspond to the various gases present the observed sample.

Credits: ESA - AOES Medialab

 
 
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