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Impact of equatorial and continental airflow on primary greenhouse gases in the northern South China Sea

Bibliographic Data

ID15547964
AuthorsChang‐Feng Ou‐Yang (0000-0002-8477-3013, National Central University), Ming‐Cheng Yen (0000-0001-7852-980X, National Central University), Tang-Huang Lin (0000-0003-1045-3196, National Central University, corresponding author), Jia‐Lin Wang (0000-0001-8662-2019, National Central University), R C Schnell (0000-0002-5792-6205, National Oceanic and Atmospheric Administration), Patricia Lang (National Oceanic and Atmospheric Administration), Somporn Chantara (0000-0003-2617-7800, Chiang Mai University), Neng‐Huei Lin (0000-0001-8549-3059, National Central University, corresponding author)
Year2015
Volume10
Issue6
Pages065005-065005
Publication date2015-06-01
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/10/6/065005
OpenAlexW2108120487
LanguageEN

Four-year ground-level measurements of the two primary greenhouse gases (carbon dioxide (CO _2 ) and methane (CH _4 )) were conducted at Dongsha Island (DSI), situated in the northern South China Sea (SCS), from March 2010 to February 2014. Their mean mixing ratios are calculated to be 396.3 ± 5.4 ppm and 1863.6 ± 50.5 ppb, with an annual growth rate of +2.19 ± 0.5 ppm yr ^–1 and +4.70 ± 4.4 ppb yr ^–1 for CO _2 and CH _4 , respectively, over the study period. Our results suggest that the Asian continental outflow driven by the winter northeast monsoon could have brought air pollutants into the northern SCS, as denoted by significantly elevated levels of 6.5 ppm for CO _2 and 59.6 ppb for CH _4 , which are greater than the marine boundary layer references at Cape Kumukahi (KUM) in the tropical northern Pacific in January. By contrast, the summertime CH _4 at DSI is shown to be lower than that at KUM by 19.7 ppb, whereas CO _2 is shown to have no differences (<0.42 ppm in July) during the same period. Positive biases of the Greenhouse Gases Observing Satellite (GOSAT) L4B data against the surface measurements are estimated to be 2.4 ± 3.4 ppm for CO _2 and 43.2 ± 36.8 ppb for CH _4 . The satellite products retrieved from the GOSAT showed the effects of anthropogenic emissions and vegetative sinks on land on a vertical profiling basis. The prevailing southeasterly winds originating from as far south as the equator or Southern Hemisphere pass through the lower troposphere in the northern SCS, forming a tunnel of relatively clean air masses as indicated by the low CH _4 mixing ratios observed on the DSI in summer

Atmospheric methane · Atmospheric sciences · Carbon dioxide · Climatology · Greenhouse gas · Methane · Monsoon · Northern Hemisphere · Southern Hemisphere · Atmospheric and Environmental Gas Dynamics · Atmospheric chemistry and aerosols · Climate variability and models · Environmental Science · Geology · Oceanography

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