High-resolution measurements of microphysics and entrainment in marine stratocumulus clouds

被引:4
作者
Yeom, Jae Min [1 ]
Szodry, Kai-Erik [2 ]
Siebert, Holger [2 ]
Ehrlich, Andre [3 ]
Mellado, Juan Pedro [4 ]
Shaw, Raymond A. [1 ]
Yum, Seong Soo [5 ]
机构
[1] Michigan Technol Univ, Dept Phys, Houghton, MI 49931 USA
[2] Leibniz Inst Tropospher Res, Leipzig, Germany
[3] Univ Leipzig, Leipzig, Germany
[4] Univ Hamburg, Hamburg, Germany
[5] Yonsei Univ, Seoul, South Korea
关键词
cloud microphysics; entrainment interfacial layer; entrainment velocity; inhomogeneous mixing; BOUNDARY-LAYER CLOUDS; TOP ENTRAINMENT; AIRBORNE MEASUREMENTS; DISSIPATION RATES; MIXING PROCESS; IN-SITU; TURBULENCE; AEROSOL; CONVECTION; DYNAMICS;
D O I
10.1002/qj.4586
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
High-resolution measurements from the Airborne Cloud-Turbulence Observation System (ACTOS) during the Azores Stratocumulus Measurements of Radiation, Turbulence and Aerosols (ACORES) campaign are analysed for an investigation of the vertical profiles of microphysical properties and entrainment velocity (W-e) in marine stratocumulus clouds. The vertical profiles show the transition from the cloudy layer to free troposphere with nearly linear profiles of total water mixing ratio, liquid water potential temperature and virtual potential temperature, but the thickness of entrainment interfacial layer varies significantly. Sharp transitions of cloud microphysical and optical properties within a single horizontal flight leg are found in one stratocumulus cloud system. They seem to be related to the local environmental conditions, such as the wind shear and turbulent dissipation rate. W-e values estimated by three methods show consistent tendencies in general and are clearly related to the local environmental conditions, such as vertical shear of the horizontal wind and turbulence intensity. However, the magnitudes of W-e values differ by up to two orders of magnitude depending on the methods, which suggests that the estimation of W-e from in situ measurements is still a challenge. Analysis of the microphysical response to entrainment suggests that inhomogeneous mixing occurs dominantly. On the other hand, the analysis results for the clouds under more humid conditions indicate a higher likelihood of homogeneous mixing.
引用
收藏
页码:81 / 97
页数:17
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