Open AccessLarge‐scale distribution of CH 4 in the western North Pacific: Sources and transport from the Asian continent
Author(s) -
Bartlett Karen B.,
Sachse Glen W.,
Slate Thomas,
Harward Charles,
Blake Donald R.
Publication year - 2003
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2002jd003076
Subject(s) - trace gas , environmental science , latitude , tracer , outflow , chemical transport model , mixing ratio , troposphere , atmospheric sciences , methane , geology , climatology , oceanography , chemistry , physics , geodesy , organic chemistry , nuclear physics
Methane (CH 4 ) mixing ratios in the northern Pacific Basin were sampled from two aircraft during the TRACE‐P mission (Transport and Chemical Evolution over the Pacific) from late February through early April 2001 using a tunable diode laser system. Described in more detail by Jacob et al. [2003], the mission was designed to characterize Asian outflow to the Pacific, determine its chemical evolution, and assess changes to the atmosphere resulting from the rapid industrialization and increased energy usage on the Asian continent. The high‐resolution, high‐precision data set of roughly 13,800 CH 4 measurements ranged between 1602 ppbv in stratospherically influenced air and 2149 ppbv in highly polluted air. Overall, CH 4 mixing ratios were highly correlated with a variety of other trace gases characteristic of a mix of anthropogenic industrial and combustion sources and were strikingly correlated with ethane (C 2 H 6 ) in particular. Averages with latitude in the near‐surface (0–2 km) show that CH 4 was elevated well above background levels north of 15°N close to the Asian continent. In the central and eastern Pacific, levels of CH 4 were lower as continental inputs were mixed horizontally and vertically during transport. Overall, the correlation between CH 4 and other hydrocarbons such as ethane (C 2 H 6 ), ethyne (C 2 H 2 ), and propane (C 3 H 8 ) as well as the urban/industrial tracer perchloroethene (C 2 Cl 4 ), suggests that for CH 4 colocated sources such as landfills, wastewater treatment, and fossil fuel use associated with urban areas dominate regional inputs at this time. Comparisons between measurements made during TRACE‐P and those of PEM‐West B, flown during roughly the same time of year and under a similar meteorological setting 7 years earlier, suggest that although the TRACE‐P CH 4 observations are higher, the changes are not significantly greater than the increases seen in background air over this time interval.