Seasonal evaluation of tropospheric CO<sub>2</sub> over the Asia-Pacific region observed by the CONTRAIL commercial airliner measurements

oleh: T. Umezawa, H. Matsueda, Y. Sawa, Y. Niwa, Y. Niwa, T. Machida, L. Zhou

Format: Article
Diterbitkan: Copernicus Publications 2018-10-01

Deskripsi

<p>Measurement of atmospheric carbon dioxide (CO<sub>2</sub>) is indispensable for top-down estimation of surface CO<sub>2</sub> sources/sinks by an atmospheric transport model. Despite the growing importance of Asia in the global carbon budget, the region has only been sparsely monitored for atmospheric CO<sub>2</sub> and our understanding of atmospheric CO<sub>2</sub> variations in the region (and thereby that of the regional carbon budget) is still limited. In this study, we present climatological CO<sub>2</sub> distributions over the Asia-Pacific region obtained from the CONTRAIL (Comprehensive Observation Network for TRace gases by AIrLiner) measurements. The high-frequency in-flight CO<sub>2</sub> measurements over 10 years reveal a clear seasonal variation in CO<sub>2</sub> in the upper troposphere (UT), with a maximum occurring in April–May and a minimum in August–September. The CO<sub>2</sub> mole fraction in the UT north of 40°&thinsp;N is low and highly variable in June–August due to the arrival of air parcels with seasonally low CO<sub>2</sub> caused by the summertime biospheric uptake in boreal Eurasia. For August–September in particular, the UT CO<sub>2</sub> is noticeably low within the Asian summer monsoon anticyclone associated with the convective transport of strong biospheric CO<sub>2</sub> uptake signal over South Asia. During September as the anticyclone decays, a spreading of this low-CO<sub>2</sub> area in the UT is observed in the vertical profiles of CO<sub>2</sub> over the Pacific Rim of continental East Asia. Simulation results identify the influence of anthropogenic and biospheric CO<sub>2</sub> fluxes in the seasonal evolution of the spatial CO<sub>2</sub> distribution over the Asia-Pacific region. It is inferred that a substantial contribution to the UT CO<sub>2</sub> over the northwestern Pacific comes from continental East Asian emissions in spring; but in the summer monsoon season, the prominent air mass origin switches to South Asia and/or Southeast Asia with a distinct imprint of the biospheric CO<sub>2</sub> uptake. The CONTRAIL CO<sub>2</sub> data provide useful constraints to model estimates of surface fluxes and to the evaluation of the satellite observations, in particular for the Asia-Pacific region.</p>