Evaluation of a method to retrieve temperature and wind velocity profiles of the Venusian nightside mesosphere from mid-infrared CO2 absorption line observed by heterodyne spectroscopy
Abstract We evaluated a method for retrieving vertical temperature and Doppler wind velocity profiles of the Venusian nightside mesosphere from the CO2 absorption line resolved by mid-infrared heterodyne spectroscopy. The achievable sensitive altitude and retrieval accuracy were derived with multipl...
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doaj-53d28fdf1f114ca1a207fc09c3df6e602020-11-25T02:00:30ZengSpringerOpenEarth, Planets and Space1880-59812020-05-0172111910.1186/s40623-020-01188-0Evaluation of a method to retrieve temperature and wind velocity profiles of the Venusian nightside mesosphere from mid-infrared CO2 absorption line observed by heterodyne spectroscopyKosuke Takami0Hiromu Nakagawa1Hideo Sagawa2Pia Krause3Isao Murata4Yasumasa Kasaba5Takeshi Kuroda6Shohei Aoki7Toru Kouyama8Theodor Kostiuk9Timothy A. Livengood10Gabriella Gilli11Department of Geophysics, Graduate School of Science, Tohoku UniversityDepartment of Geophysics, Graduate School of Science, Tohoku UniversityFaculty of Science, Kyoto Sangyo UniversityPhysical Institute, Universität zu KölnGraduate School of Environmental Studies, Tohoku UniversityPlanetary Plasma and Atmospheric Research Center, Graduate School of Science, Tohoku UniversityDepartment of Geophysics, Graduate School of Science, Tohoku UniversityPlanetary Aeronomy, Belgian Institute for Space AeronomyArtificial Intelligence Research Center, National Institute of Advanced Industrial Science and TechnologyNASA Goddard Space Flight CenterNASA Goddard Space Flight CenterInstituto de Astrofísica e Ciências do Espaço (IA)Abstract We evaluated a method for retrieving vertical temperature and Doppler wind velocity profiles of the Venusian nightside mesosphere from the CO2 absorption line resolved by mid-infrared heterodyne spectroscopy. The achievable sensitive altitude and retrieval accuracy were derived with multiple model spectra generated from various temperature and wind velocity profiles with several noise levels. The temperature profiles were retrieved at altitudes of 70–100 km with a vertical resolution of 5 km and a retrieval accuracy of ± 15 K. The wind velocity was also retrieved at an altitude of approximately 85 km with a vertical resolution of 10 km and a retrieval accuracy of ± 25–50 m/s. In addition, we studied an event and applied our method to spectra obtained by the HIPWAC instrument attached to the NASA/IRTF 3-m telescope on May 19–22, 2012. Retrieved wind velocities in a latitude of 33° S at 3:00 LT were interpreted as subsolar-to-antisolar (SS-AS) flows at altitudes of 84 ± 6 km and 94 ± 7 km, and they were stronger than expected. This result suggested that the transition between the retrograde superrotational zonal (RSZ) wind and SS-AS flow may occur at altitudes below 90 km which previously was predicted to be the transition region. This work provides a basis for our analysis of further observations obtained by a mid-infrared heterodyne spectrometer MILAHI attached to the Tohoku University 60-cm telescope at Haleakalā, Hawaii.http://link.springer.com/article/10.1186/s40623-020-01188-0VenusMesosphereTemperatureWind velocityMid-infrared heterodyne spectroscopyCO2 absorption line |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Kosuke Takami Hiromu Nakagawa Hideo Sagawa Pia Krause Isao Murata Yasumasa Kasaba Takeshi Kuroda Shohei Aoki Toru Kouyama Theodor Kostiuk Timothy A. Livengood Gabriella Gilli |
spellingShingle |
Kosuke Takami Hiromu Nakagawa Hideo Sagawa Pia Krause Isao Murata Yasumasa Kasaba Takeshi Kuroda Shohei Aoki Toru Kouyama Theodor Kostiuk Timothy A. Livengood Gabriella Gilli Evaluation of a method to retrieve temperature and wind velocity profiles of the Venusian nightside mesosphere from mid-infrared CO2 absorption line observed by heterodyne spectroscopy Earth, Planets and Space Venus Mesosphere Temperature Wind velocity Mid-infrared heterodyne spectroscopy CO2 absorption line |
author_facet |
Kosuke Takami Hiromu Nakagawa Hideo Sagawa Pia Krause Isao Murata Yasumasa Kasaba Takeshi Kuroda Shohei Aoki Toru Kouyama Theodor Kostiuk Timothy A. Livengood Gabriella Gilli |
author_sort |
Kosuke Takami |
title |
Evaluation of a method to retrieve temperature and wind velocity profiles of the Venusian nightside mesosphere from mid-infrared CO2 absorption line observed by heterodyne spectroscopy |
title_short |
Evaluation of a method to retrieve temperature and wind velocity profiles of the Venusian nightside mesosphere from mid-infrared CO2 absorption line observed by heterodyne spectroscopy |
title_full |
Evaluation of a method to retrieve temperature and wind velocity profiles of the Venusian nightside mesosphere from mid-infrared CO2 absorption line observed by heterodyne spectroscopy |
title_fullStr |
Evaluation of a method to retrieve temperature and wind velocity profiles of the Venusian nightside mesosphere from mid-infrared CO2 absorption line observed by heterodyne spectroscopy |
title_full_unstemmed |
Evaluation of a method to retrieve temperature and wind velocity profiles of the Venusian nightside mesosphere from mid-infrared CO2 absorption line observed by heterodyne spectroscopy |
title_sort |
evaluation of a method to retrieve temperature and wind velocity profiles of the venusian nightside mesosphere from mid-infrared co2 absorption line observed by heterodyne spectroscopy |
publisher |
SpringerOpen |
series |
Earth, Planets and Space |
issn |
1880-5981 |
publishDate |
2020-05-01 |
description |
Abstract We evaluated a method for retrieving vertical temperature and Doppler wind velocity profiles of the Venusian nightside mesosphere from the CO2 absorption line resolved by mid-infrared heterodyne spectroscopy. The achievable sensitive altitude and retrieval accuracy were derived with multiple model spectra generated from various temperature and wind velocity profiles with several noise levels. The temperature profiles were retrieved at altitudes of 70–100 km with a vertical resolution of 5 km and a retrieval accuracy of ± 15 K. The wind velocity was also retrieved at an altitude of approximately 85 km with a vertical resolution of 10 km and a retrieval accuracy of ± 25–50 m/s. In addition, we studied an event and applied our method to spectra obtained by the HIPWAC instrument attached to the NASA/IRTF 3-m telescope on May 19–22, 2012. Retrieved wind velocities in a latitude of 33° S at 3:00 LT were interpreted as subsolar-to-antisolar (SS-AS) flows at altitudes of 84 ± 6 km and 94 ± 7 km, and they were stronger than expected. This result suggested that the transition between the retrograde superrotational zonal (RSZ) wind and SS-AS flow may occur at altitudes below 90 km which previously was predicted to be the transition region. This work provides a basis for our analysis of further observations obtained by a mid-infrared heterodyne spectrometer MILAHI attached to the Tohoku University 60-cm telescope at Haleakalā, Hawaii. |
topic |
Venus Mesosphere Temperature Wind velocity Mid-infrared heterodyne spectroscopy CO2 absorption line |
url |
http://link.springer.com/article/10.1186/s40623-020-01188-0 |
work_keys_str_mv |
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