@article{oai:kitami-it.repo.nii.ac.jp:00007558,
 author = {SASAKI, Masafumi and ENDOH, Noboru and IMURA, Satoshi and KUDOH, Sakae and YAMANOUCHI, Takashi and MORIMOTO, Shinji and HASHIDA, Gen},
 issue = {D16313},
 journal = {JOURNAL OF GEOPHYSICAL RESEARCH ATMOSPHERE},
 month = {Aug},
 note = {Dissolved methane concentrations (DM) in 17 lakes were measured as a part of the operations of the 45th Japanese Antarctic Research Expedition in ice-free rocky areas along the eastern coast of Lutzow-Holm Bay (Syowa Oasis) in East Antarctica in the summer of 2003~2004. DM at the surfaces of 14 lakes ranged from the atmospheric equilibrium concentration (about 4 nmol L?1 for fresh water) to 385 nmol L?1. Relatively low DM of less than 50 nmol L?1 were observed at about 60% of the lakes. Many of the lakes (area fraction of 85%) were supersaturated and are thus sources of methane to the atmosphere. The exchange coefficient was calculated using wind speed data at Syowa Station. Area fraction frequency distributions with 4 surface DM ranges were applied to all lakes at Syowa Oasis (110 lakes: total lake area of 9 km2). Extrapolation to the whole Syowa Oasis gives an estimate of total emission of about 1 t-CH4 yr?1. This is the first estimation of methane flux from the surfaces of thawed lakes to the atmosphere in Antarctica. Since methane efflux of about 2 t-CH4 yr?1 from frozen bubbles in lake ice was estimated in our previous study, a total amount of 3 t-CH4 yr?1 would be released to the atmosphere from the lakes during the ice melting season (December ~ January) at Syowa Oasis.},
 pages = {1--14},
 title = {Air-lake exchange of methane during the open water season in Syowa Oasis, East Antarctica},
 volume = {115},
 year = {2010}
}