Simulation study for the Stratospheric Inferred Winds (SIW) sub-millimeter limb sounder

• Main Authors: P. Baron, D. Murtagh, P. Eriksson, J. Mendrok, S. Ochiai, K. Pérot, H. Sagawa, M. Suzuki
• Format: Article
• Language: English
• Published: Copernicus Publications 2018-07-01
• Series: Atmospheric Measurement Techniques
• Online Access: https://www.atmos-meas-tech.net/11/4545/2018/amt-11-4545-2018.pdf

<p>Stratospheric Inferred Winds (SIW) is a Swedish mini sub-millimeter limb sounder selected for the 2nd InnoSat platform, with launch planned for around 2022. It is intended to fill the altitude gap between 30 and 70&thinsp;km in atmospheric wind measurements and also aims at pursuing the limb observations of temperature and key atmospheric constituents between 10 and 90&thinsp;km when current satellite missions will probably come to an end. Line-of-sight winds are retrieved from the Doppler shift of molecular emission lines introduced by the wind field. Observations will be performed with two antennas pointing toward the limb in perpendicular directions in order to reconstruct the 2-D horizontal wind vector. Each antenna has a vertical field of view (FOV) of 5&thinsp;km. The chosen spectral band, near 655&thinsp;GHz, contains a dense group of strong O₃ lines suitable for exploiting the small amount of wind information in stratospheric spectra. Using both sidebands of the heterodyne receiver, a large number of chemical species will be measured, including O₃ isotopologues, H₂O, HDO, HCl, ClO, N₂O, HNO₃, NO, NO₂, HCN, CH₃CN and HO₂. This paper presents a simulation study that assesses measurement performance. The line-of-sight winds are retrieved between 30 and 90&thinsp;km with the best sensitivity between 35 and 70&thinsp;km, where the precision (1<i>σ</i>) is 5–10&thinsp;m s⁻¹ for a single scan. Similar performance can be obtained during day and night conditions except in the lower mesosphere, where the photo-dissociation of O₃ in daytime reduces the sensitivity by 50&thinsp;% near 70&thinsp;km. Profiles of O₃, H₂O and temperature are retrieved with high precision up to 50&thinsp;km ( &lt; 1&thinsp;%,  &lt; 2&thinsp;%, 1&thinsp;K, respectively). Systematic errors due to uncertainties in spectroscopic parameters, in the radiometer sideband ratio and in the radiance calibration process are investigated. A large wind retrieval bias of 10–30&thinsp;m s⁻¹ between 30 and 40&thinsp;km could be induced by the air-broadening parameter uncertainties of O₃ lines. This highlights the need for good knowledge of these parameters and for studying methods to mitigate the retrieval bias.</p>