Exploring relations between cloud morphology, cloud phase, and cloud radiative properties in Southern Ocean's stratocumulus clouds

<p>Marine stratocumuli are the most dominant cloud type by area coverage in the Southern Ocean (SO). They can be divided into different self-organized cellular morphological regimes known as open and closed mesoscale-cellular convective (MCC) clouds. Open and closed cells are the two most freq...

Full description

Bibliographic Details
Main Authors: J. Danker, O. Sourdeval, I. L. McCoy, R. Wood, A. Possner
Format: Article
Language:English
Published: Copernicus Publications 2022-08-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/22/10247/2022/acp-22-10247-2022.pdf
_version_ 1798037946093273088
author J. Danker
O. Sourdeval
I. L. McCoy
I. L. McCoy
R. Wood
A. Possner
author_facet J. Danker
O. Sourdeval
I. L. McCoy
I. L. McCoy
R. Wood
A. Possner
author_sort J. Danker
collection DOAJ
description <p>Marine stratocumuli are the most dominant cloud type by area coverage in the Southern Ocean (SO). They can be divided into different self-organized cellular morphological regimes known as open and closed mesoscale-cellular convective (MCC) clouds. Open and closed cells are the two most frequent types of organizational regimes in the SO. Using the liDAR-raDAR (DARDAR) version 2 retrievals, we quantify 59 % of all MCC clouds in this region as mixed-phase clouds (MPCs) during a 4-year time period from 2007 to 2010. The net radiative effect of SO MCC clouds is governed by changes in cloud albedo. Both cloud morphology and phase have previously been shown to impact cloud albedo individually, but their interactions and their combined impact on cloud albedo remain unclear.</p> <p>Here, we investigate the relationships between cloud phase, organizational patterns, and their differences regarding their cloud radiative properties in the SO. The mixed-phase fraction, which is defined as the number of MPCs divided by the sum of MPC and supercooled liquid cloud (SLC) pixels, of all MCC clouds at a given cloud-top temperature (CTT) varies considerably between austral summer and winter. We further find that seasonal changes in cloud phase at a given CTT across all latitudes are largely independent of cloud morphology and are thus seemingly constrained by other external factors. Overall, our results show a stronger dependence of cloud phase on cloud-top height (CTH) than CTT for clouds below 2.5 km in altitude.</p> <p>Preconditioning through ice-phase processes in MPCs has been observed to accelerate individual closed-to-open cell transitions in extratropical stratocumuli. The hypothesis of preconditioning has been further substantiated in large-eddy simulations of open and closed MPCs. In this study, we do not find preconditioning to primarily impact climatological cloud morphology statistics in the SO. Meanwhile, in-cloud albedo analysis reveals stronger changes in open and closed cell albedo in SLCs than in MPCs. In particular, few optically thick (cloud optical thickness <span class="inline-formula">&gt;10</span>) open cell stratocumuli are characterized as ice-free SLCs. These differences in in-cloud albedo are found to alter the cloud radiative effect in the SO by 21 to 39 W m<span class="inline-formula"><sup>−2</sup></span> depending on season and cloud phase.</p>
first_indexed 2024-04-11T21:33:30Z
format Article
id doaj.art-e8443b920842469fa2703c243709c14d
institution Directory Open Access Journal
issn 1680-7316
1680-7324
language English
last_indexed 2024-04-11T21:33:30Z
publishDate 2022-08-01
publisher Copernicus Publications
record_format Article
series Atmospheric Chemistry and Physics
spelling doaj.art-e8443b920842469fa2703c243709c14d2022-12-22T04:01:51ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242022-08-0122102471026510.5194/acp-22-10247-2022Exploring relations between cloud morphology, cloud phase, and cloud radiative properties in Southern Ocean's stratocumulus cloudsJ. Danker0O. Sourdeval1I. L. McCoy2I. L. McCoy3R. Wood4A. Possner5Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt, GermanyUniv. Lille, CNRS, UMR 8518 – LOA – Laboratoire d'Optique Atmosphérique, 59000 Lille, FranceCooperative Programs for the Advancement of Earth System Science, University Corporation for Atmospheric Research, Boulder, Colorado, USARosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida, USAAtmospheric Sciences, University of Washington, Seattle, WA, USAInstitute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt, Germany<p>Marine stratocumuli are the most dominant cloud type by area coverage in the Southern Ocean (SO). They can be divided into different self-organized cellular morphological regimes known as open and closed mesoscale-cellular convective (MCC) clouds. Open and closed cells are the two most frequent types of organizational regimes in the SO. Using the liDAR-raDAR (DARDAR) version 2 retrievals, we quantify 59 % of all MCC clouds in this region as mixed-phase clouds (MPCs) during a 4-year time period from 2007 to 2010. The net radiative effect of SO MCC clouds is governed by changes in cloud albedo. Both cloud morphology and phase have previously been shown to impact cloud albedo individually, but their interactions and their combined impact on cloud albedo remain unclear.</p> <p>Here, we investigate the relationships between cloud phase, organizational patterns, and their differences regarding their cloud radiative properties in the SO. The mixed-phase fraction, which is defined as the number of MPCs divided by the sum of MPC and supercooled liquid cloud (SLC) pixels, of all MCC clouds at a given cloud-top temperature (CTT) varies considerably between austral summer and winter. We further find that seasonal changes in cloud phase at a given CTT across all latitudes are largely independent of cloud morphology and are thus seemingly constrained by other external factors. Overall, our results show a stronger dependence of cloud phase on cloud-top height (CTH) than CTT for clouds below 2.5 km in altitude.</p> <p>Preconditioning through ice-phase processes in MPCs has been observed to accelerate individual closed-to-open cell transitions in extratropical stratocumuli. The hypothesis of preconditioning has been further substantiated in large-eddy simulations of open and closed MPCs. In this study, we do not find preconditioning to primarily impact climatological cloud morphology statistics in the SO. Meanwhile, in-cloud albedo analysis reveals stronger changes in open and closed cell albedo in SLCs than in MPCs. In particular, few optically thick (cloud optical thickness <span class="inline-formula">&gt;10</span>) open cell stratocumuli are characterized as ice-free SLCs. These differences in in-cloud albedo are found to alter the cloud radiative effect in the SO by 21 to 39 W m<span class="inline-formula"><sup>−2</sup></span> depending on season and cloud phase.</p>https://acp.copernicus.org/articles/22/10247/2022/acp-22-10247-2022.pdf
spellingShingle J. Danker
O. Sourdeval
I. L. McCoy
I. L. McCoy
R. Wood
A. Possner
Exploring relations between cloud morphology, cloud phase, and cloud radiative properties in Southern Ocean's stratocumulus clouds
Atmospheric Chemistry and Physics
title Exploring relations between cloud morphology, cloud phase, and cloud radiative properties in Southern Ocean's stratocumulus clouds
title_full Exploring relations between cloud morphology, cloud phase, and cloud radiative properties in Southern Ocean's stratocumulus clouds
title_fullStr Exploring relations between cloud morphology, cloud phase, and cloud radiative properties in Southern Ocean's stratocumulus clouds
title_full_unstemmed Exploring relations between cloud morphology, cloud phase, and cloud radiative properties in Southern Ocean's stratocumulus clouds
title_short Exploring relations between cloud morphology, cloud phase, and cloud radiative properties in Southern Ocean's stratocumulus clouds
title_sort exploring relations between cloud morphology cloud phase and cloud radiative properties in southern ocean s stratocumulus clouds
url https://acp.copernicus.org/articles/22/10247/2022/acp-22-10247-2022.pdf
work_keys_str_mv AT jdanker exploringrelationsbetweencloudmorphologycloudphaseandcloudradiativepropertiesinsouthernoceansstratocumulusclouds
AT osourdeval exploringrelationsbetweencloudmorphologycloudphaseandcloudradiativepropertiesinsouthernoceansstratocumulusclouds
AT ilmccoy exploringrelationsbetweencloudmorphologycloudphaseandcloudradiativepropertiesinsouthernoceansstratocumulusclouds
AT ilmccoy exploringrelationsbetweencloudmorphologycloudphaseandcloudradiativepropertiesinsouthernoceansstratocumulusclouds
AT rwood exploringrelationsbetweencloudmorphologycloudphaseandcloudradiativepropertiesinsouthernoceansstratocumulusclouds
AT apossner exploringrelationsbetweencloudmorphologycloudphaseandcloudradiativepropertiesinsouthernoceansstratocumulusclouds