Articles | Volume 18, issue 2
https://doi.org/10.5194/acp-18-833-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-18-833-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
23 Jan 2018
Research article |
| 23 Jan 2018
Vertical distributions of N2O isotopocules in the equatorial stratosphere
Sakae Toyoda
CORRESPONDING AUTHOR
Department of Chemical Science and Engineering, School of Materials
and Chemical Technology, Tokyo Institute of Technology, Yokohama 226-8502,
Japan
Naohiro Yoshida
Department of Chemical Science and Engineering, School of Materials
and Chemical Technology, Tokyo Institute of Technology, Yokohama 226-8502,
Japan
Earth-Life Science Institute, Tokyo Institute of Technology, Tokyo
152-8550, Japan
Shinji Morimoto
Center for Atmospheric and Oceanic Studies, Graduate School of
Science, Tohoku University, Sendai 980-8578, Japan
Shuji Aoki
Center for Atmospheric and Oceanic Studies, Graduate School of
Science, Tohoku University, Sendai 980-8578, Japan
Takakiyo Nakazawa
Center for Atmospheric and Oceanic Studies, Graduate School of
Science, Tohoku University, Sendai 980-8578, Japan
Satoshi Sugawara
Miyagi University of Education, Sendai 980-0845, Japan
Shigeyuki Ishidoya
National Institute of Advanced Industrial Science and Technology
(AIST), Tsukuba 305-8569, Japan
Mitsuo Uematsu
Atmosphere and Ocean Research Institute (AORI), The University of
Tokyo, Kashiwa 277-8564, Japan
Yoichi Inai
Center for Atmospheric and Oceanic Studies, Graduate School of
Science, Tohoku University, Sendai 980-8578, Japan
Fumio Hasebe
Faculty of Environmental Earth Science, Hokkaido University, Sapporo 060-0810, Japan
Chusaku Ikeda
Institute of Space and Astronautical Sciences (ISAS), Japan
Aerospace Exploration Agency (JAXA), Sagamihara 252-5210, Japan
Hideyuki Honda
Institute of Space and Astronautical Sciences (ISAS), Japan
Aerospace Exploration Agency (JAXA), Sagamihara 252-5210, Japan
Kentaro Ishijima
Project Team for HPC Advanced Predictions Using Big Data, Japan
Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama
236-0001, Japan
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Cited
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- Photolytic fractionation of seven singly and doubly substituted nitrous oxide isotopocules measured by quantum cascade laser absorption spectroscopy K. Kantnerová et al. 10.1016/j.aeaoa.2020.100094
- Balloon-borne tropospheric CO2 observations over the equatorial eastern and western Pacific Y. Inai et al. 10.1016/j.atmosenv.2018.04.016
- Coordinated Upper-Troposphere-to-Stratosphere Balloon Experiment in Biak F. Hasebe et al. 10.1175/BAMS-D-16-0289.1
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- A Near‐Global Atmospheric Distribution of N2O Isotopologues P. Bernath et al. 10.1002/2017GL075122
6 citations as recorded by crossref.
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- Nitrous Oxide Formation by Corona Discharge: Isotopic Composition Measurements and Atmospheric Applications M. Smith et al. 10.1029/2020JD033927
- Photolytic fractionation of seven singly and doubly substituted nitrous oxide isotopocules measured by quantum cascade laser absorption spectroscopy K. Kantnerová et al. 10.1016/j.aeaoa.2020.100094
- Balloon-borne tropospheric CO2 observations over the equatorial eastern and western Pacific Y. Inai et al. 10.1016/j.atmosenv.2018.04.016
- Coordinated Upper-Troposphere-to-Stratosphere Balloon Experiment in Biak F. Hasebe et al. 10.1175/BAMS-D-16-0289.1
- Stratospheric carbon isotope fractionation and tropospheric histories of CFC-11, CFC-12, and CFC-113 isotopologues M. Thomas et al. 10.5194/acp-21-6857-2021
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Latest update: 04 Jul 2025
Short summary
By analysis of whole air samples collected by balloon-borne compact cryogenic samplers, we found that apparent isotope effect for stratospheric N2O between 25 and 30 km over the Equator is larger than that observed in other latitudes and that it is almost equal to the effect predicted by laboratory simulation experiments. These results suggest that equatorial middle stratosphere can be treated as an isolated region when we consider the decomposition of N2O by photochemical processes.
By analysis of whole air samples collected by balloon-borne compact cryogenic samplers, we found...
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