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2.5. SATELLITE GROUP 69<br />

2.5 Satellite Group<br />

Participating scientist Steffen Beirle, Tim Deutschmann, Barbara Dix, Ossama Ibrahim, Christian<br />

Frankenberg, Michael Grzegorski, Klaus-Peter Heue, Jens Hollwedel, Muhammad Fahim Khokhar,<br />

Sven Kühl, Thiery Marbach, Janis Pukite, Suniti Sanghavi, Thomas Wagner, and Walburga Wilms-<br />

Grabe<br />

Abstract The Satellitegroup is part of the researchgroup Atmospheric Physics of Prof. Dr. Ulrich<br />

Platt. The satellite born remote sensing of the Earth’s atmosphere at the University of Heidelberg<br />

started in 1996 with the retrieval of atmospheric trace gases, namely NO2 and BrO. Today a wide variety<br />

of trace gases and other atmospheric parameters (Aerosols, Clouds, Radiative Transfer) from different<br />

satellite instruments are investigated at the IUP (see also http://satellite.iup.uni-heidelberg.de).<br />

Figure 2.34: Satellite measurement of the reflected and scattered sun light (yellow). The spectral<br />

signatures of several atmospheric trace gases are analysed in selected spectral ranges using the DOAS<br />

method. Displayed are the fitting results for various species analysed in the satellite group.<br />

Overarching topic and Background For about 10 years now, a new generation of UV/vis/NIR<br />

satellite instruments (GOME, SCIAMACHY, OMI) with moderate spectral resolution allows the<br />

retrieval of a large variety of atmospheric trace gases. In particular, global maps of several tropospheric<br />

trace gases like O3, BrO, NO2, CO, CH4, CO2, HCHO, SO2, H2O, O2, O4, and cloud properties can<br />

be analysed from observations in nadir viewing mode. The most important advantage of such satellite<br />

observations is their spatial (horizontal) coverage and resolution. The latest generation of nadir looking<br />

UV/vis satellite instruments (e.g. OMI) achieves global coverage within one day and has a horizontal<br />

resolution of about 13 x 24 km 2 . From such satellite observations, various individual sources like large<br />

cities can be identified. In addition, the observation of scattered sun light in limb geometry allows to<br />

retrieve vertical profiles of several stratospheric trace gases like O3, NO2, BrO and OClO.<br />

Funding The group activities are funded through various national and international projects, e.g.<br />

SCIAMACHY validation, FORMAT, STAR, Tropische Tropopause, NOXTRAM, EVERGREEN, AC-<br />

CENT<br />

Main methods From the measured spectra, the narowband absorption features of several trace<br />

gases are analysed using the DOAS method (see Figure). The result of the spectral analysis represents<br />

the trace gas absorption integrated along the absorption path. In addition, also the broad band<br />

spectral features are analysed; they yield information in particular on the cloud cover, aerosol load and<br />

ground albedo. Various algorithms for the analysis of satellite spectra were developed in the satellite<br />

group within the last years. For the detailed interpretation of the analysed spectral information,<br />

radiative transfer modelling is needed. A 3-D Monte-Carlo radiative transfer model (TRACY) was<br />

developed in our group, which allows to simulate various complex viewing geometries and atmospheric<br />

properties. The retrieved global data sets are further investigated using image sequence techniques.

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