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...
Main Authors: | , , , , , , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2016-07-01
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Series: | Atmospheric Chemistry and Physics |
Online Access: | https://www.atmos-chem-phys.net/16/9149/2016/acp-16-9149-2016.pdf |
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. |
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ISSN: | 1680-7316 1680-7324 |