JpGU-AGU Joint Meeting 2017

Presentation information

[JJ] Oral

A (Atmospheric and Hydrospheric Sciences) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS11] [JJ] Atmospheric Chemistry

Tue. May 23, 2017 10:45 AM - 12:15 PM A10 (Tokyo Bay Makuhari Hall)

convener:Hitoshi Irie(Center for Environmental Remote Sensing, Chiba University), Toshinobu Machida(National Institute for Environmental Studies), Hiroshi Tanimoto(National Institute for Environmental Studies), Yoko Iwamoto(Graduate School of Biosphere Science, Hiroshima University), Chairperson:Hiroshi Tanimoto(National institute for environmental studies)

11:15 AM - 11:30 AM

[AAS11-03] Climatological variations of tropospheric CO2 over the Asia-Pacific region observed by the CONTRAIL commercial airliner measurements

*Taku Umezawa1, Hidekazu Matsueda2, Yosuke Niwa2, Yousuke Sawa2, Toshinobu Machida1, Lingxi Zhou3 (1.National Institute of Environmental Studies, 2.Meteorological Research Institute, 3.Chinese Academy of Meteorological Sciences)

Keywords:Carbon dioxide, Aircraft observation, Asian monsoon

We present spatial and temporal variations of tropospheric CO2 over the Asia-Pacific region analyzed from 10 years of the CONTRAIL commercial airliner measurements. The CONTRAIL flights with the high-frequency CO2 measurements have covered large part of the Asia-Pacific region. Here we address climatological variations of CO2 from the boundary layer to the upper troposphere across the Asia-Pacific region toward comprehensive understanding of influence of Asian surface fluxes under the varying seasonal meteorology. Highlights of this study are summarized as follows. (1) Seasonally elevated and highly variable CO2 is observed in East Asia to the North Pacific in spring. This is likely explained by active passage of eastward-tracking synoptic systems that sweeps the continental East Asia and uplifts the region’s CO2 emissions up to the free troposphere. (2) The region-wide CO2 decrease is obvious across the Asia-Pacific region and it is principally composed of CO2 drawdowns originating in two distinct regions: boreal Eurasia and South Asia. We observed seasonally largest variability of CO2 in the UT north of 40° N, likely due to heterogeneous spatial distributions of biospheric fluxes combined with sporadic convective vertical transport over the continent. Our observations also characterized distinct CO2 depletion in the upper troposphere over South Asia as a result of strong South Asian biospheric uptakes and confinement in the Asian summer monsoon anticyclone. The development and decay of the anticyclone remarkably contributes to distributing CO2 over the Asia-Pacific region. (3) As the cyclonic activity decays and the monsoon anticyclone develops from spring to summer, CONTRAIL measurements with highest data density over East Asia to the North Pacific serve as better constraints to CO2 fluxes in East Asia in spring and those in South Asia in late summer.