Technical Note: Intercomparison of ILAS-II version 2 and 1.4 trace species with MIPAS-B measurements

• Main Authors: Wetzel, G., Sugita, T., Nakajima, H., Tanaka, T., Yokota, T., Friedl-Vallon, F., Kleinert, A., Maucher, G., Oelhaf, H.
• Other Authors: Institute for Meteorology and Climate Research (IMK), Karlsruhe Institute of Technology (KIT), National Institute for Environmental Studies (NIES)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2008
• Subjects: [SDU.OCEAN]Sciences of the Universe [physics]/Ocean; Atmosphere; Ilas; Kiruna
• Online Access: https://hal.science/hal-00296465; https://hal.science/hal-00296465/document; https://hal.science/hal-00296465/file/acp-8-1119-2008.pdf

International audience The Improved Limb Atmospheric Spectrometer (ILAS)-II sensor aboard the Japanese ADEOS-II satellite was launched into its sun-synchronous orbit on 14 December 2002 and performed solar occultation measurements of trace species, aerosols, temperature, and pressure in the polar stratosphere until 25 October 2003. Vertical trace gas profiles obtained with the balloon version of the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS-B) provide one of the sparse data sets for validating ILAS-II version 2 and 1.4 data. The MIPAS-B limb emission spectra were collected on 20 March 2003 over Kiruna (Sweden, 68° N) at virtually the same location that has been sounded by ILAS-II about 5.5 h prior to the sampling of MIPAS-B. The intercomparison of the new ILAS-II version 2 (Northern Hemispheric sunrise) data to MIPAS-B vertical trace gas profiles shows a good to excellent agreement within the combined error limits for the species O 3 , N 2 O, CH 4 , H 2 O (above 21 km), HNO 3 , ClONO 2 , and CFC-11 (CCl 3 F) in the compared altitude range between 16 and 31 km such that these data appear to be very useful for scientific analysis. With regard to the previous version 1.4 ILAS-II data, significant improvements in the consistency with MIPAS-B are obvious especially for the species CH 4 and H 2 O, but also for O 3 , HNO 3 , ClONO 2 , NO 2 , and N 2 O 5 . However, comparing gases like NO 2 , N 2 O 5 , and CFC-12 (CCl 2 F 2 ) exhibits only poor agreement with MIPAS-B such that these species cannot be assumed to be validated at the present time.