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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Main Authors: 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
Format: Article
Language:English
Published: SpringerOpen 2020-05-01
Series:Earth, Planets and Space
Subjects:
Online Access:http://link.springer.com/article/10.1186/s40623-020-01188-0
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spelling 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
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