TY - JOUR
T1 - Ground-based network observation of Asian dust events of April 1998 in east Asia
AU - Murayama, Toshiyuki
AU - Sugimoto, Nobuo
AU - Uno, Itsushi
AU - Kinoshita, Kisei
AU - Aoki, Kazuma
AU - Hagiwara, Naseru
AU - Liu, Zhaoyan
AU - Matsui, Ichiro
AU - Sakai, Tetsu
AU - Shibata, Takashi
AU - Arao, Kimio
AU - Sohn, Byung Ju
AU - Won, Jae Gwang
AU - Yoon, Soon Chang
AU - Li, Tao
AU - Zhou, Jun
AU - Hu, Huanling
AU - Abo, Makoto
AU - Iokibe, Kengo
AU - Koga, Ryuji
AU - Iwasaka, Yasunobu
PY - 2001/8/27
Y1 - 2001/8/27
N2 - We coordinated a ground-based network that has been in use since 1997 to observe Asian dust during springtime. Huge Asian dust events that occurred in the middle of April 1998 were captured by this network. In this paper we present the organization of the network; a description of the instruments, including the lidar, sky radiometer, and optical particle counter; and the results of the observation, and offer discussions regarding the transport mechanism of Asian dust in east Asia using an on-line tracer model. We discussed the time series of the surface concentration and the height distribution of the dust. A cutoff cyclone generated during the dust episode was responsible for trapping and sedimentation during the transportation of the Asian dust, particularly in the southern parts of China and Japan. Horizontal dust images derived from NOAA/AVHRR clearly revealed the structure of the vortex. The lidar network observation confirmed the general pattern of dust height distribution in this event; the height of the major dust layer was about 3 km over Japan but was higher (4 to 5 km) in Seoul and Hefei. A thin dust layer in the upper troposphere was also commonly observed in Hefei and Japan. Evidence of the coexistence of dust and cirrus was shown by the polarization lidar. The lidar network observation of Asian dust and satellite remote sensing provide key information for the study of the transport mechanism of Asian dust. Further extension of the lidar network toward the interior of the continent and the Pacific Rim would reveal the greater global mechanism of the transportation.
AB - We coordinated a ground-based network that has been in use since 1997 to observe Asian dust during springtime. Huge Asian dust events that occurred in the middle of April 1998 were captured by this network. In this paper we present the organization of the network; a description of the instruments, including the lidar, sky radiometer, and optical particle counter; and the results of the observation, and offer discussions regarding the transport mechanism of Asian dust in east Asia using an on-line tracer model. We discussed the time series of the surface concentration and the height distribution of the dust. A cutoff cyclone generated during the dust episode was responsible for trapping and sedimentation during the transportation of the Asian dust, particularly in the southern parts of China and Japan. Horizontal dust images derived from NOAA/AVHRR clearly revealed the structure of the vortex. The lidar network observation confirmed the general pattern of dust height distribution in this event; the height of the major dust layer was about 3 km over Japan but was higher (4 to 5 km) in Seoul and Hefei. A thin dust layer in the upper troposphere was also commonly observed in Hefei and Japan. Evidence of the coexistence of dust and cirrus was shown by the polarization lidar. The lidar network observation of Asian dust and satellite remote sensing provide key information for the study of the transport mechanism of Asian dust. Further extension of the lidar network toward the interior of the continent and the Pacific Rim would reveal the greater global mechanism of the transportation.
UR - http://www.scopus.com/inward/record.url?scp=0034803607&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0034803607&partnerID=8YFLogxK
U2 - 10.1029/2000JD900554
DO - 10.1029/2000JD900554
M3 - Article
AN - SCOPUS:0034803607
SN - 0148-0227
VL - 106
SP - 18345
EP - 18359
JO - Journal of Geophysical Research Atmospheres
JF - Journal of Geophysical Research Atmospheres
IS - D16
M1 - 2000JD900554
ER -