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Comparison of nitric oxide measurements in the mesosphere and lower thermosphere from ACE-FTS, MIPAS, SCIAMACHY, and SMR

Stefan Bender ; M. Sinnhuber ; T. von Clarmann ; G. Stiller ; B. Funke ; M. López-Puertas ; Joachim Urban (Institutionen för rymd- och geovetenskap, Global miljömätteknik och modellering) ; Kristell Pérot (Institutionen för rymd- och geovetenskap, Global miljömätteknik och modellering) ; K. Walker ; J. Burrows
Atmospheric Measurement Techniques (1867-8548). Vol. 8 (2015), 10, p. 4171-4195.
[Artikel, refereegranskad vetenskaplig]

We compare the nitric oxide measurements in the mesosphere and lower thermosphere (60 to 150 km) from four instruments: the Atmospheric Chemistry Experiment–Fourier Transform Spectrometer (ACE-FTS), the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS), the SCanning Imaging Absorption spectroMeter for Atmospheric CHartographY (SCIAMACHY), and the Sub-Millimetre Radiometer (SMR). We use the daily zonal mean data in that altitude range for the years 2004–2010 (ACE-FTS), 2005–2012 (MIPAS), 2008–2012 (SCIAMACHY), and 2003–2012 (SMR). We first compare the data qualitatively with respect to the morphology, focussing on the major features, and then compare the time series directly and quantitatively. In three geographical regions, we compare the vertical density profiles on coincident measurement days. Since none of the instruments delivers continuous daily measurements in this altitude region, we carried out a multi-linear regression analysis. This regression analysis considers annual and semi-annual variability in the form of harmonic terms and inter-annual variability by responding linearly to the solar Lyman-α radiation index and the geomagnetic Kp index. This analysis helps to find similarities and differences in the individual data sets with respect to the inter-annual variations caused by geomagnetic and solar variability.

Nyckelord: Nitric Oxide, Middle atmosphere, Energetic Particle Precipitation, Odin/SMR



Denna post skapades 2015-10-12. Senast ändrad 2016-01-27.
CPL Pubid: 224075

 

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