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Title: Cloud Edge Properties Measured by the ARM Shortwave Spectrometer Over Ocean and Land

Abstract

In this paper, we use the spectrally invariant method to study the variability of cloud optical thickness (τ) and droplet effective radius (reff) in transition zones between the cloudy and clear-sky columns observed by Shortwave Array Spectroradiometer-Zenith at the Southern Great Plains Central Facility site (SGP C1) and during the Marine ARM GPCI Investigation of Clouds (MAGIC) field campaign. The spectrally invariant method approximates the spectra in the transition zone as a linear combination of definitely clear and definitely cloudy spectra. The slope and intercept of the linear relations characterize τ and reff in the transition region, respectively. The radiative transfer model simulations show that that (i) the slope of the visible band is positively correlated with τ, while (ii) the intercept of the near-infrared band has a high negative correlation with reff. We have analyzed 22 cloud edge cases from the SGP and MAGIC and found that from cloud to clear in the transitions, (a) the slopes of the visible band decrease, indicating the decrease of τ toward cloud edges, and (b) the intercepts of the near-infrared band show a much more significant increase at the SGP than from the MAGIC. The results from observed cases suggest that whilemore » τ decreases for all cases, the decrease in reff is much more significant for cloud over land at the SGP site compared to the ocean counterpart during the MAGIC campaign.« less

Authors:
ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [3]
  1. NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States); Univ. Space Research Association, Columbia, MD (United States)
  2. NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States)
  3. NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States); Morgan State Univ., Baltimore, MD (United States)
Publication Date:
Research Org.:
NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
OSTI Identifier:
1593962
Grant/Contract Number:  
SC0005457; SC0018045
Resource Type:
Accepted Manuscript
Journal Name:
Journal of Geophysical Research: Atmospheres
Additional Journal Information:
Journal Volume: 124; Journal Issue: 15; Journal ID: ISSN 2169-897X
Publisher:
American Geophysical Union
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; cloud edge; ARM; shortwave spectrometer; spectrally invariant; SGP; MAGIC; transition zone; cloud; cloud-aerosol interaction; air entrainment and mixing; spectral invariance; shortwave spectroradiometer

Citation Formats

Yang, Weidong, Marshak, Alexander, and Wen, Guoyong. Cloud Edge Properties Measured by the ARM Shortwave Spectrometer Over Ocean and Land. United States: N. p., 2019. Web. doi:10.1029/2019JD030622.
Yang, Weidong, Marshak, Alexander, & Wen, Guoyong. Cloud Edge Properties Measured by the ARM Shortwave Spectrometer Over Ocean and Land. United States. https://doi.org/10.1029/2019JD030622
Yang, Weidong, Marshak, Alexander, and Wen, Guoyong. Wed . "Cloud Edge Properties Measured by the ARM Shortwave Spectrometer Over Ocean and Land". United States. https://doi.org/10.1029/2019JD030622. https://www.osti.gov/servlets/purl/1593962.
@article{osti_1593962,
title = {Cloud Edge Properties Measured by the ARM Shortwave Spectrometer Over Ocean and Land},
author = {Yang, Weidong and Marshak, Alexander and Wen, Guoyong},
abstractNote = {In this paper, we use the spectrally invariant method to study the variability of cloud optical thickness (τ) and droplet effective radius (reff) in transition zones between the cloudy and clear-sky columns observed by Shortwave Array Spectroradiometer-Zenith at the Southern Great Plains Central Facility site (SGP C1) and during the Marine ARM GPCI Investigation of Clouds (MAGIC) field campaign. The spectrally invariant method approximates the spectra in the transition zone as a linear combination of definitely clear and definitely cloudy spectra. The slope and intercept of the linear relations characterize τ and reff in the transition region, respectively. The radiative transfer model simulations show that that (i) the slope of the visible band is positively correlated with τ, while (ii) the intercept of the near-infrared band has a high negative correlation with reff. We have analyzed 22 cloud edge cases from the SGP and MAGIC and found that from cloud to clear in the transitions, (a) the slopes of the visible band decrease, indicating the decrease of τ toward cloud edges, and (b) the intercepts of the near-infrared band show a much more significant increase at the SGP than from the MAGIC. The results from observed cases suggest that while τ decreases for all cases, the decrease in reff is much more significant for cloud over land at the SGP site compared to the ocean counterpart during the MAGIC campaign.},
doi = {10.1029/2019JD030622},
journal = {Journal of Geophysical Research: Atmospheres},
number = 15,
volume = 124,
place = {United States},
year = {Wed Jul 24 00:00:00 EDT 2019},
month = {Wed Jul 24 00:00:00 EDT 2019}
}

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Figures / Tables:

Figure 1 Figure 1: Schematic illustration of two limiting scenarios of the air entrainment and mixing processes: (a) the homogeneous mixing reduces the size of all droplets but does not substantial change the number of cloud droplets due to quick mixing of cloud and drier air, and no solid line boundary betweenmore » cloud and air in the “starting time” (top panel) to indicate this process; (b) the inhomogeneous mixing reduces the droplet number concentration for droplets of all sizes but does not change the droplet size spectrum as a result of cloud droplets evaporation before dry air penetrates to the entirety of cloud, and a solid line boundary between cloud and air in the starting time (top panel) to indicate this process.« less

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