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

IF 3 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Quarterly Journal of the Royal Meteorological Society Pub Date : 2023-10-17 DOI:10.1002/qj.4586
Jae Min Yeom, Kai‐Erik Szodry, Holger Siebert, André Ehrlich, Juan Pedro Mellado, Raymond A. Shaw, Seong Soo Yum
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Abstract

Abstract 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.

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海洋层积云微物理和夹带的高分辨率测量
摘要:本文分析了亚速尔群岛层积云辐射、湍流和气溶胶测量(acres)活动期间机载云湍流观测系统(ACTOS)的高分辨率测量数据,以研究海洋层积云的微物理特性和夹带速度(W e)的垂直剖面。垂直剖面表现为从阴云层向自由对流层的过渡,总水混合比、液态水势温度和虚势温度的分布近似线性,但夹带界面层厚度变化较大。在一个层积云系统中,在单个水平飞行腿内发现了云微物理和光学性质的急剧转变。它们似乎与当地的环境条件有关,如风切变和湍流耗散率。三种方法估算的W值总体上呈现一致的趋势,且与局地环境条件(如水平风的垂直切变和湍流强度)有明显的关系。然而,根据不同的方法,W - e值的大小相差高达两个数量级,这表明从原位测量中估计W - e仍然是一个挑战。对夹带的微物理响应分析表明,主要发生非均匀混合。另一方面,在较湿润的条件下,云的分析结果表明均匀混合的可能性更高。
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来源期刊
CiteScore
16.80
自引率
4.50%
发文量
163
审稿时长
3-8 weeks
期刊介绍: The Quarterly Journal of the Royal Meteorological Society is a journal published by the Royal Meteorological Society. It aims to communicate and document new research in the atmospheric sciences and related fields. The journal is considered one of the leading publications in meteorology worldwide. It accepts articles, comprehensive review articles, and comments on published papers. It is published eight times a year, with additional special issues. The Quarterly Journal has a wide readership of scientists in the atmospheric and related fields. It is indexed and abstracted in various databases, including Advanced Polymers Abstracts, Agricultural Engineering Abstracts, CAB Abstracts, CABDirect, COMPENDEX, CSA Civil Engineering Abstracts, Earthquake Engineering Abstracts, Engineered Materials Abstracts, Science Citation Index, SCOPUS, Web of Science, and more.
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