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Title: An Observational Study on Cloud Spectral Width in North China

Abstract

Cloud droplet size distribution (CDSD) is a critical characteristic for a number of processes related to clouds, considering that cloud droplets are formed in different sizes above the cloud-base. This paper analyzes the in-situ aircraft measurements of CDSDs and aerosol concentration ( Na ) performed in stratiform clouds in Hebei, China, in 2015 to reveal the characteristics of cloud spectral width, commonly known as relative dispersion ( ฮต , ratio of standard deviation (ฯƒ) to mean radius (r) of the CDSD). A new algorithm is developed to calculate the contributions of droplets of different sizes to ฮต . It is found that small droplets with the size range of 1 to 5.5 ฮผm and medium droplets with the size range of 5.5 to 10 ฮผm are the major contributors to ฮต, and the medium droplets generally dominate the change of ฮต. The variation of ฮต with Na can be well explained by comparing the normalized changes of ฯƒ and r ( kฯƒ/ฯƒ and kr/r ), rather than kฯƒ and k r only ( kฯƒ is ฮ”ฯƒ/ฮ” Na and kr is ฮ”r/ฮ” Na ). From the perspective of external factors affecting ฮต change, the effects of Na and condensation are examined.more » As a result, it is found that ฮต increases initially and decreases afterward as Na increases, and โ€œcondensational broadeningโ€ occurs up to 1 km above cloud-base, potentially providing observational evidence for recent numerical simulations in the literature.« less

Authors:
ORCiD logo [1];  [1];  [1]; ORCiD logo [2];  [3];  [4]
  1. Nanjing Univ. of Information Science & Technology, Nanjing (China)
  2. Brookhaven National Lab. (BNL), Upton, NY (United States)
  3. Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
  4. Hebei Weather Modification Office, Shijiazhuang (China)
Publication Date:
Research Org.:
Brookhaven National Lab. (BNL), Upton, NY (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
OSTI Identifier:
1497378
Report Number(s):
BNL-211312-2019-JAAM
Journal ID: ISSN 2073-4433; ATMOCZ
Grant/Contract Number:  
SC0012704
Resource Type:
Accepted Manuscript
Journal Name:
Atmosphere (Basel)
Additional Journal Information:
Journal Name: Atmosphere (Basel); Journal Volume: 10; Journal Issue: 3; Journal ID: ISSN 2073-4433
Publisher:
MDPI
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; cloud droplet spectral dispersion; aerosol concentration; height above cloud-base; aircraft observations

Citation Formats

Wang, Yuan, Niu, Shengjie, Lu, Chunsong, Liu, Yangang, Chen, Jingyi, and Yang, Wenxia. An Observational Study on Cloud Spectral Width in North China. United States: N. p., 2019. Web. doi:10.3390/atmos10030109.
Wang, Yuan, Niu, Shengjie, Lu, Chunsong, Liu, Yangang, Chen, Jingyi, & Yang, Wenxia. An Observational Study on Cloud Spectral Width in North China. United States. https://doi.org/10.3390/atmos10030109
Wang, Yuan, Niu, Shengjie, Lu, Chunsong, Liu, Yangang, Chen, Jingyi, and Yang, Wenxia. Fri . "An Observational Study on Cloud Spectral Width in North China". United States. https://doi.org/10.3390/atmos10030109. https://www.osti.gov/servlets/purl/1497378.
@article{osti_1497378,
title = {An Observational Study on Cloud Spectral Width in North China},
author = {Wang, Yuan and Niu, Shengjie and Lu, Chunsong and Liu, Yangang and Chen, Jingyi and Yang, Wenxia},
abstractNote = {Cloud droplet size distribution (CDSD) is a critical characteristic for a number of processes related to clouds, considering that cloud droplets are formed in different sizes above the cloud-base. This paper analyzes the in-situ aircraft measurements of CDSDs and aerosol concentration ( Na ) performed in stratiform clouds in Hebei, China, in 2015 to reveal the characteristics of cloud spectral width, commonly known as relative dispersion ( ฮต , ratio of standard deviation (ฯƒ) to mean radius (r) of the CDSD). A new algorithm is developed to calculate the contributions of droplets of different sizes to ฮต . It is found that small droplets with the size range of 1 to 5.5 ฮผm and medium droplets with the size range of 5.5 to 10 ฮผm are the major contributors to ฮต, and the medium droplets generally dominate the change of ฮต. The variation of ฮต with Na can be well explained by comparing the normalized changes of ฯƒ and r ( kฯƒ/ฯƒ and kr/r ), rather than kฯƒ and k r only ( kฯƒ is ฮ”ฯƒ/ฮ” Na and kr is ฮ”r/ฮ” Na ). From the perspective of external factors affecting ฮต change, the effects of Na and condensation are examined. As a result, it is found that ฮต increases initially and decreases afterward as Na increases, and โ€œcondensational broadeningโ€ occurs up to 1 km above cloud-base, potentially providing observational evidence for recent numerical simulations in the literature.},
doi = {10.3390/atmos10030109},
journal = {Atmosphere (Basel)},
number = 3,
volume = 10,
place = {United States},
year = {Fri Mar 01 00:00:00 EST 2019},
month = {Fri Mar 01 00:00:00 EST 2019}
}

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Figures / Tables:

Figure 1 Figure 1: Vertical profiles of aerosol concentration (๐‘a) and liquid water content (LWC) in the two flights

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