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Atmospheric, Oceanic & Planetary Physics, University of Oxford A Dudhia MIPAS QWG13 Firenze 12-14 June 2007 Page 1 Azimuth Dependence of LOS Pointing Anu.

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Presentation on theme: "Atmospheric, Oceanic & Planetary Physics, University of Oxford A Dudhia MIPAS QWG13 Firenze 12-14 June 2007 Page 1 Azimuth Dependence of LOS Pointing Anu."— Presentation transcript:

1 Atmospheric, Oceanic & Planetary Physics, University of Oxford A Dudhia MIPAS QWG13 Firenze 12-14 June 2007 Page 1 Azimuth Dependence of LOS Pointing Anu Dudhia University of Oxford

2 Atmospheric, Oceanic & Planetary Physics, University of Oxford A Dudhia MIPAS QWG13 Firenze 12-14 June 2007 Page 2  Kiefer et al have noted a MIPAS absolute pointing bias which varies approximately linearly with latitude, with N.Pole about 1.5 km lower than S.Pole (orbit 2881, 18 Sep 2002)  They suggest this is linked to the MIPAS azimuth scan and coupled with a bias in the roll angle.  However, since MIPAS has always operated with azimuth scanning, could not separate latitude effects from azimuth scan angle  On 19 March 2007 the MIPAS azimuth scan was switched off for a day …

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4 Atmospheric, Oceanic & Planetary Physics, University of Oxford A Dudhia MIPAS QWG13 Firenze 12-14 June 2007 Page 4

5 Atmospheric, Oceanic & Planetary Physics, University of Oxford A Dudhia MIPAS QWG13 Firenze 12-14 June 2007 Page 5

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7 Atmospheric, Oceanic & Planetary Physics, University of Oxford A Dudhia MIPAS QWG13 Firenze 12-14 June 2007 Page 7

8 Atmospheric, Oceanic & Planetary Physics, University of Oxford A Dudhia MIPAS QWG13 Firenze 12-14 June 2007 Page 8

9 Atmospheric, Oceanic & Planetary Physics, University of Oxford A Dudhia MIPAS QWG13 Firenze 12-14 June 2007 Page 9  Adding the azimuth scan produces a shift of +1km at S Pole and between -0.5 and -1.0 km at N Pole  Using CIRA climatology as ‘truth’, pointing without azimuth scanning appears more accurate  Results are consistent with 1.5km net difference observed by Kiefer et al and confirm that variation is linked to azimuth scan angle rather than latitude Conclusions


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