Potential for the measurement of mesosphere and lower thermosphere (MLT) wind, temperature, density and geomagnetic field with Superconducting Submillimeter-Wave Limb-Emission Sounder 2 (SMILES-2)

oleh: P. Baron, S. Ochiai, E. Dupuy, R. Larsson, H. Liu, N. Manago, D. Murtagh, S. Oyama, S. Oyama, S. Oyama, H. Sagawa, A. Saito, T. Sakazaki, M. Shiotani, M. Suzuki

Format: Article
Diterbitkan: Copernicus Publications 2020-01-01

Deskripsi

<p>Submillimeter-Wave Limb-Emission Sounder 2 (SMILES-2) is a satellite mission proposed in Japan to probe the middle and upper atmosphere (20–160&thinsp;km). The main instrument is composed of 4&thinsp;K cooled radiometers operating near 0.7 and 2&thinsp;THz. It could measure the diurnal changes of the horizontal wind above 30&thinsp;km, temperature above 20&thinsp;km, ground-state atomic oxygen above 90&thinsp;km and atmospheric density near the mesopause, as well as abundance of about 15 chemical species. In this study we have conducted simulations to assess the wind, temperature and density retrieval performance in the mesosphere and lower thermosphere (60–110&thinsp;km) using the radiometer at 760&thinsp;GHz. It contains lines of water vapor (<span class="inline-formula">H<sub>2</sub>O</span>), molecular oxygen (<span class="inline-formula">O<sub>2</sub></span>) and nitric oxide (NO) that are the strongest signals measured with SMILES-2 at these altitudes. The Zeeman effect on the <span class="inline-formula">O<sub>2</sub></span> line due to the geomagnetic field (<span class="inline-formula"><strong><em>B</em></strong></span>) is considered; otherwise, the retrieval errors would be underestimated by a factor of 2 above 90&thinsp;km. The optimal configuration for the radiometer’s polarization is found to be vertical linear. Considering a retrieval vertical resolution of 2.5&thinsp;km, the line-of-sight wind is retrieved with a precision of 2–5&thinsp;m&thinsp;s<span class="inline-formula"><sup>−1</sup></span> up to 90&thinsp;km and 30&thinsp;m&thinsp;s<span class="inline-formula"><sup>−1</sup></span> at 110&thinsp;km. Temperature and atmospheric density are retrieved with a precision better than 5&thinsp;K and 7&thinsp;% up to 90&thinsp;km (30&thinsp;K and 20&thinsp;% at 110&thinsp;km). Errors induced by uncertainties on the vector <span class="inline-formula"><strong><em>B</em></strong></span> are mitigated by retrieving it. The retrieval of <span class="inline-formula"><strong><em>B</em></strong></span> is described as a side-product of the mission. At high latitudes, precisions of 30–100&thinsp;nT on the vertical component and 100–300&thinsp;nT on the horizontal one could be obtained at 85 and 105&thinsp;km (vertical resolution of 20&thinsp;km). SMILES-2 could therefore provide the first measurements of <span class="inline-formula"><strong><em>B</em></strong></span> close to the electrojets' altitude, and the precision is enough to measure variations induced by solar storms in the auroral regions.</p>