OBSERVATION OF THE PINATUBO VOLCANIC CLOUD BY LIDAR NETWORK IN JAPAN

被引：12

作者：

UCHINO, O

NAGAI, T

FUJIMOTO, T

FUJIWARA, M

AKIYOSHI, H

YASUMATSU, S

HAYASHIDA, S

SASANO, Y

NAKANE, H

IWASAKA, Y

HASE, M

SHIBATA, T

ITABE, T

ASAI, K

NOMURA, A

SAITO, Y

KANO, T

SAI, Y

TAMAKI, K

NOMURA, R

SUNAGAWA, T

NAGASAWA, C

ABO, M

IDESAKO, Y

KAI, K

机构：

[1] Meteorological Research Institute, Tsukuba, Ibaraki 305

[2] Department of Applied Physics, Fukuoka University, Jounan, Fukuoka, 814-01

[3] The National Institute for Environmental Studies, Tsukuba, Ibaraki 305

[4] Solar-Terrestrial Environment Laboratory, Nagoya University, Toyokawa, Aichi 442

[5] Communications Research Laboratory, Koganei, Tokyo 184

[6] Tohoku Institute of Technology, Taihaku, Sendai, Miyagi 982

[7] Department of Information Engineering, Shinshu University, Nagano 380

[8] Okinawa Weather Station, Naha, Okinawa 900

[9] Department of Electronics and Information Engineering, Tokyo Metropolitan University, Hachioji, Tokyo 192-03

[10] Department of Environment Science, University of Tsukuba, Tsukuba, Ibaraki 305

来源：

JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN | 1993年 / 71卷 / 02期

关键词：

D O I：

10.2151/jmsj1965.71.2_285

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

The latitudinal and vertical distribution of stratospheric aerosols injected by eruptions of Mt. Pinatubo on June 15, 1991 was obtained in Japan by a lidar network extending from Naha (26.2-degrees-N) to Wakkanai (45.4-degrees-N). Results from June to October 1991 are reported. An increase of aerosols originating froin the Pinatubo eruptions was observed first on June 28, 1991, at approximately 16 km. The layer was observed continuously since then. The upper layer, above 20 km. was observed first on July 15, thereafter it disappeared at all stations, but reappeared on August 6. The upper layer was sporadic, and not observed in July over Nagano, some 200 km from Tsukuba, where it was observed. This indicates the non-uniform density of the cloud in the upper region.

引用

页码：285 / 295

页数：11