Dynamics and chemistry of marine stratocumulus - Dycoms-II

被引:301
作者
Stevens, B [1 ]
Lenschow, DH
Vali, G
Gerber, H
Bandy, A
Blomquist, B
Brenguier, JL
Bretherton, CS
Burnet, F
Campos, T
Chai, S
Faloona, I
Friesen, D
Haimov, S
Laursen, K
Lilly, DK
Loehrer, SM
Malinowski, SP
Morley, B
Petters, MD
Rogers, DC
Russell, L
Savic-Jovac, V
Snider, JR
Straub, D
Szumowski, MJ
Takagi, H
Thornton, DC
Tschudi, M
Twohy, C
Wetzel, M
van Zanten, MC
机构
[1] Univ Calif Los Angeles, Dept Atmospher Sci, 405 Hilgard Ave,Box 951565, Los Angeles, CA 90095 USA
[2] Natl Ctr Atmospher Res, Colorado Springs, CO USA
[3] Univ Wyoming, Dept Atmospher Sci, Laramie, WY 82071 USA
[4] Gerber Sci Inc, Reston, VA USA
[5] Drexel Univ, Dept Chem, Philadelphia, PA 19104 USA
[6] CNRM Meteo France, Toulouse, France
[7] Univ Washington, Dept Atmospher Sci, Seattle, WA 98195 USA
[8] Univ Nevada, Desert Res Inst, Reno, NV 89506 USA
[9] Univ Oklahoma, Sch Meteorol, Norman, OK 73019 USA
[10] Univ Colorado, Corp Atmospher Res, Joint Off Sci Support, Boulder, CO USA
[11] Warsaw Univ, Inst Geophys, Warsaw, Poland
[12] Princeton Univ, Princeton, NJ 08544 USA
[13] Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA
[14] Oregon State Univ, Coll Oceanog & Atmospher Sci, Corvallis, OR 97331 USA
关键词
D O I
10.1175/BAMS-84-5-579
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The second Dynamics and Chemistry of Marine Stratocumulus (DYCOMS-II) field study is described. The field program consisted of nine flights in marine stratocumulus west-southwest of San Diego, California. The objective of the program was to better understand the physics and dynamics of marine stratocumulus. Toward this end special flight strategies, including predominantly nocturnal flights, were employed to optimize estimates of entrainment velocities at cloud-top, large-scale divergence within the boundary layer, drizzle processes in the cloud, cloud microstructure, and aerosol-cloud interactions. Cloud conditions during DYCOMS-II were excellent with almost every flight having uniformly overcast clouds topping a well-mixed boundary layer. Although the emphasis of the manuscript is on the goals and methodologies of DYCOMS-II, some preliminary findings are also presented-the most significant being that the cloud layers appear to entrain less and drizzle more than previous theoretical work led investigators to expect.
引用
收藏
页码:579 / 593
页数:15
相关论文
共 82 条
[1]   DISSIPATION OF MARINE STRATIFORM CLOUDS AND COLLAPSE OF THE MARINE BOUNDARY-LAYER DUE TO THE DEPLETION OF CLOUD CONDENSATION NUCLEI BY CLOUDS [J].
ACKERMAN, AS ;
TOON, OB ;
HOBBS, PV .
SCIENCE, 1993, 262 (5131) :226-229
[2]   AEROSOLS, CLOUD MICROPHYSICS, AND FRACTIONAL CLOUDINESS [J].
ALBRECHT, BA .
SCIENCE, 1989, 245 (4923) :1227-1230
[3]  
ALBRECHT BA, 1988, B AM METEOROL SOC, V69, P618, DOI 10.1175/1520-0477(1988)069<0618:OOMSCD>2.0.CO
[4]  
2
[5]  
ALBRECHT BA, 1995, B AM METEOROL SOC, V76, P889, DOI 10.1175/1520-0477(1995)076<0889:TASTE>2.0.CO
[6]  
2
[7]  
[Anonymous], CLOUD CHEM CLIMATE
[8]  
AUSTIN P, 1995, J ATMOS SCI, V52, P2329, DOI 10.1175/1520-0469(1995)052<2329:PISCOA>2.0.CO
[9]  
2
[10]  
Bigg E. K., 1986, Atmospheric Research, V20, P82