TY - JOUR
T1 - Nocturnal sink of NOx via NO3 and N2O5 in the outflow from a source area in Japan
AU - Matsumoto, Jun
AU - Imagawa, Kousuke
AU - Imai, Hidekazu
AU - Kosugi, Naohiro
AU - Ideguchi, Masumi
AU - Kato, Shungo
AU - Kajii, Yoshizumi
N1 - Funding Information:
The authors acknowledge members of the Oshima Park Office for their help in the practical setup of this campaign. This study was supported by Core Research for Evolutional Science and Technology (CREST) of Japan Science and Technology Agency.
PY - 2006/10
Y1 - 2006/10
N2 - To understand the nocturnal sink of NOx in the outflow from the Asian source area, simultaneous observations of NO3, N2O5, and related compounds were conducted utilizing an instrument based on laser-induced fluorescence at Izu-Oshima Island, Japan, during June 2004. Consequently, significant levels of NO3 and N2O5 were successfully observed, particularly in the polluted air mass originating from Tokyo. This observation concurred with the equilibrium among NO3, NO2, and N2O5 gases. As a result of steady-state analysis, nocturnal NOx losses were evaluated as 1.8 and 0.2 ppbv night-1 for polluted and maritime air, respectively. It was confirmed that the nocturnal NOx sink during the observation was promoted by the NO3 loss by VOC. DMS is significant for nocturnal loss of NOx over the sea.
AB - To understand the nocturnal sink of NOx in the outflow from the Asian source area, simultaneous observations of NO3, N2O5, and related compounds were conducted utilizing an instrument based on laser-induced fluorescence at Izu-Oshima Island, Japan, during June 2004. Consequently, significant levels of NO3 and N2O5 were successfully observed, particularly in the polluted air mass originating from Tokyo. This observation concurred with the equilibrium among NO3, NO2, and N2O5 gases. As a result of steady-state analysis, nocturnal NOx losses were evaluated as 1.8 and 0.2 ppbv night-1 for polluted and maritime air, respectively. It was confirmed that the nocturnal NOx sink during the observation was promoted by the NO3 loss by VOC. DMS is significant for nocturnal loss of NOx over the sea.
KW - Dinitrogen pentoxide
KW - Laser-induced fluorescence
KW - NO sink in the outflow
KW - Nitrate radical
KW - Nocturnal atmosphere
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U2 - 10.1016/j.atmosenv.2006.05.045
DO - 10.1016/j.atmosenv.2006.05.045
M3 - Article
AN - SCOPUS:33748309161
SN - 1352-2310
VL - 40
SP - 6294
EP - 6302
JO - Atmospheric Environment
JF - Atmospheric Environment
IS - 33
ER -