Atmospheric Measurement Techniques www.atmos-meas-tech.net 1867-1381 1867-8548 3 1 2010 10.5194/amt-3-283-2010 http://www.atmos-meas-tech.net/3/283/2010/ http://www.atmos-meas-tech.net/3/283/2010/amt-3-283-2010.html http://www.atmos-meas-tech.net/3/283/2010/amt-3-283-2010.pdf 283 299 2010-02-25 Retrieval of tropospheric column densities of NO₂ from combined SCIAMACHY nadir/limb measurements S. Beirle steffen.beirle@mpic.de S. Kühl J. PuÄ·Ä«te T. Wagner Max-Planck-Institut für Chemie, Mainz, Germany The SCIAMACHY instrument onboard the ESA satellite ENVISAT allows measurements of various atmospheric trace gases, such as NO₂. A unique feature of SCIAMACHY is that measurements are made alternately in limb and nadir mode. The limb measurements provide an opportunity for directly determining stratospheric column densities (CDs), which are needed to extract tropospheric CDs from the total CD measurements performed in (quasi simultaneous) nadir geometry.<br> <br> Here we discuss the potential and limitations of SCIAMACHY limb measurements for estimating stratospheric CDs of NO₂ in comparison to a simple reference sector method, and the consequences for the resulting tropospheric CDs. A direct, absolute limb correction scheme is presented that improves spatial patterns of tropospheric NO₂ column densities at high latitudes, but results in artificial zonal stripes at low latitudes. Subsequently, a <i>relative</i> limb correction scheme is introduced that successfully reduces stratospheric artefacts in the tropospheric data product without introducing new ones. This relative limb correction scheme is rather simple, robust, and, in essence, based on measurements alone.<br> <br> The effects of the different stratospheric estimation schemes on tropospheric CDs are discussed with respect to zonal and temporal dependencies. In addition, we define error quantities from the nadir/limb measurements that indicate remaining systematic errors as a function of latitude and day.<br> <br> Our new suggested stratospheric estimation scheme, the relative limb correction, improves mean tropospheric slant CDs significantly, e.g. from &minus;1&times;10¹⁵ molec/cm² (using a reference sector method) to &asymp;0 in the Atlantic ocean, and from +1&times;10¹⁵ molec/cm² to &asymp;0 over Siberia, at 50&deg; N in January 2003–2008. Beirle, S., Platt, U., Wenig, M., and Wagner, T.: Weekly cycle of NO₂ by GOME measurements: a signature of anthropogenic sources, Atmos. Chem. Phys., 3, 2225–2232, 2003. 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