Lidar observed characteristics of the tropical cirrus clouds

被引:20
作者
Sivakumar, V
Bhavanikumar, Y
Rao, PB
Mizutani, K
Aoki, T
Yasui, M
Itabe, T
机构
[1] Natl MST Radar Facil, Tirupati 517502, Andhra Pradesh, India
[2] Natl Remote Sensing Agcy, Hyderabad 500037, Andhra Pradesh, India
[3] Commun Res Labs, Tokyo 1848795, Japan
关键词
remote sensing; cloud physics and chemistry; cirrus;
D O I
10.1029/2002RS002719
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
[1] Using the polarization diversity lidar data collected during March 1998 to April 2001, the characteristics of the tropical cirrus clouds observed over Gadanki (13.5degreesN; 79.2degreesE) are presented in this paper. Out of 210 nights of observations during this period, cirrus clouds were observed over the lidar site on 170 nights. The cloud mean height is found to be in the range of 8-17 km with peak occurrence at 13-14 km, just below the tropopause. The cloud thickness has values ranging 0.6-4.2 km with maximum occurrence at 0.9-1.2 km. The scattering ratio and the linear depolarization ratio are in the ranges of 1.14-36 and 0.01-0.75 with peak occurrences seen at 1.14-2 and 0.01-0.05, respectively. The optical depth can be as high as 2, but values less than 0.1 account for most (> 80%) of the clouds. The clouds with low optical depth occur most frequently during fall equinox and high optical depth during summer. The formations of thin and thick cirrus clouds are seen to be closely related to the minimum tropospheric temperature and cumulonimbus outflows, respectively.
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页数:9
相关论文
共 49 条
[41]  
2
[42]   Corona-producing ice clouds: a case study of a cold mid-latitude cirrus layer [J].
Sassen, K ;
Mace, GG ;
Hallett, J ;
Poellot, MR .
APPLIED OPTICS, 1998, 37 (09) :1477-1485
[43]   Ice nucleation in cirrus clouds: A model study of the homogeneous and heterogeneous modes [J].
Sassen, K ;
Benson, S .
GEOPHYSICAL RESEARCH LETTERS, 2000, 27 (04) :521-524
[44]  
Sassen K., 1995, REV LASER ENG, V23, P148, DOI DOI 10.2184/LSJ.23.148
[45]   DEPOLARIZATION OF POLARIZED-LIGHT CAUSED BY HIGH-ALTITUDE CLOUDS .1. DEPOLARIZATION OF LIDAR INDUCED BY CIRRUS [J].
SUN, YY ;
LI, ZP ;
BOSENBERG, J .
APPLIED OPTICS, 1989, 28 (17) :3625-3632
[46]  
Uthe E.E., 1977, P IAMAP S RAD ATM GA, P242
[47]   A 6-year climatology of cloud occurrence frequency from stratospheric aerosol and gas experiment II observations (1985-1990) [J].
Wang, PH ;
Minnis, P ;
McCormick, MP ;
Kent, GS ;
Skeens, KM .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D23) :29407-29429
[48]   Tropical high cloud characteristics derived from SAGE II extinction measurements [J].
Wang, Pi-Huan ;
McCormick, M. P. ;
Poole, L. R. ;
Chu, W. P. ;
Yue, G. K. ;
Kent, G. S. ;
Skeens, K. M. .
ATMOSPHERIC RESEARCH, 1994, 34 (1-4) :53-83
[49]   Laminar cirrus observed near the tropical tropopause by LITE [J].
Winker, DM ;
Trepte, CR .
GEOPHYSICAL RESEARCH LETTERS, 1998, 25 (17) :3351-3354