Large XCH<sub>4</sub> anomaly in summer 2013 over northeast Asia observed by GOSAT

Extremely high levels of column-averaged dry-air mole fractions of atmospheric methane (XCH<sub>4</sub>) were detected in August and September 2013 over northeast Asia (∼  20 ppb above the averaged summertime XCH<sub>4</sub> over 2009–2012, after removing a long-term trend...

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Bibliographic Details
Main Authors: M. Ishizawa, O. Uchino, I. Morino, M. Inoue, Y. Yoshida, K. Mabuchi, T. Shirai, Y. Tohjima, S. Maksyutov, H. Ohyama, S. Kawakami, A. Takizawa, D. Belikov
Format: Article
Language:English
Published: Copernicus Publications 2016-07-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/16/9149/2016/acp-16-9149-2016.pdf
Description
Summary:Extremely high levels of column-averaged dry-air mole fractions of atmospheric methane (XCH<sub>4</sub>) were detected in August and September 2013 over northeast Asia (∼  20 ppb above the averaged summertime XCH<sub>4</sub> over 2009–2012, after removing a long-term trend), as being retrieved from the Short-Wavelength InfraRed (SWIR) spectral data observed with the Thermal And Near-infrared Sensor for carbon Observation – Fourier Transform Spectrometer (TANSO-FTS) onboard Greenhouse Gases Observing Satellite (GOSAT). Similar enhancements of XCH<sub>4</sub> were also observed by the ground-based measurements at two Total Carbon Column Observing Network (TCCON) sites in Japan.<br><br> The analysis of surface CH<sub>4</sub> concentrations observed at three monitoring sites around the Japan archipelago suggest that the extreme increase of XCH<sub>4</sub> has occurred in a limited area. The model analysis was conducted to investigate this anomalously high XCH<sub>4</sub> event, using an atmospheric transport model. The results indicate that the extreme increase of XCH<sub>4</sub> is attributed to the anomalous atmospheric pressure pattern over East Asia during the summer of 2013, which effectively transported the CH<sub>4</sub>-rich air to Japan from the strong CH<sub>4</sub> source areas in east China. The two Japanese TCCON sites, ∼  1000 km east–west apart each other, coincidentally located along the substantially CH<sub>4</sub>-rich air flow from east China. This analysis demonstrates the capability of GOSAT to monitor an XCH<sub>4</sub> event on a synoptic scale. We anticipate that the synoptic information of XCH<sub>4</sub> from GOSAT data contributes to improve our understanding of regional carbon cycle and the regional flux estimation.
ISSN:1680-7316
1680-7324