HR: 0800h
AN: A21D-0735 [Abstracts]
TI: Tropospheric ozone-enhanced layers observed over the equatorial Pacific Ocean and the contribution of transport of midlatitude UT/LS air
AU: * Kita, K
EM: kita@mx.ibaraki.ac.jp
AF: College of Science, Ibaraki University, 2-1-1 Bunkyo, Mito, 310-8512, Japan
AU: Hayashi, H
EM: nd5407g@mcs.ibaraki.ac.jp
AF: College of Science, Ibaraki University, 2-1-1 Bunkyo, Mito, 310-8512, Japan
AU: Taguchi, S
EM: s.taguchi@aist.go.jp
AF: Research Institute for Environmental Management Technology, National Institute of
Advanced Industrial Science and Technology, 16-1 Onogawa, Tsukuba, 305-8569, Japan
AB:
Occurrence and its seasonal variation of ozone (O3)-enhanced layers in the troposphere over the equatorial
Pacific Ocean were investigated based on ozonesonde data obtained at three Southern Hemisphere ADditional
OZonesondes (SHADOZ) sites, Watukosek, American Samoa and San Cristobal, for 6 years between 1998 and
2003. The O3-enhanced layers were frequently observed at the three sites, and their occurrence was about 50%
on average. The formation processes of O3-enhanced layers were investigated by meteorological analyses
including backward trajectories. Several O3-enhanced layers resulted from the transport of air masses affected
by biomass burning. The contribution of this process was about 30% at San Cristobal during February to March
period and August to September period, while it was relatively low, about 10%, at Watukosek and Samoa. A
significant part of the O3-enhanced layers were attributed to the transport of midlatitude upper-troposphere and
lower-stratosphere (UT/LS) air. Meteorological analyses indicated that these layers were originated from
equatorward and downward transport of the midlatitude UT/LS air masses through a narrow region between high
and low pressure systems around subtropical jet stream. This process accounts for about 50% of observed
O3-enhanced layers at Watukosek, about 80% of those at Samoa, and about 30% of those at San Cristobal,
indicating that it was important for O3 budget over the equatorial Pacific Ocean.
DE: 0365 Troposphere: composition and chemistry
DE: 0368 Troposphere: constituent transport and chemistry
SC: Atmospheric Sciences [A]
MN: 2007 Fall Meeting