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Toward understanding of differences in current cloud retrievals of ARM ground‐based measurements

Identifieur interne : 001585 ( Istex/Corpus ); précédent : 001584; suivant : 001586

Toward understanding of differences in current cloud retrievals of ARM ground‐based measurements

Auteurs : Chuanfeng Zhao ; Shaocheng Xie ; Stephen A. Klein ; Alain Protat ; Matthew D. Shupe ; Sally A. Mcfarlane ; Jennifer M. Comstock ; Julien Delanoë ; Min Deng ; Maureen Dunn ; Robin J. Hogan ; Dong Huang ; Michael P. Jensen ; Gerald G. Mace ; Renata Mccoy ; Ewan J. O'Connor ; David D. Turner ; Zhien Wang

Source :

RBID : ISTEX:73F4A0165A4ED262F3B63F601EAD8E0B98542726

English descriptors

Abstract

Accurate observations of cloud microphysical properties are needed for evaluating and improving the representation of cloud processes in climate models and better estimate of the Earth radiative budget. However, large differences are found in current cloud products retrieved from ground‐based remote sensing measurements using various retrieval algorithms. Understanding the differences is an important step to address uncertainties in the cloud retrievals. In this study, an in‐depth analysis of nine existing ground‐based cloud retrievals using ARM remote sensing measurements is carried out. We place emphasis on boundary layer overcast clouds and high level ice clouds, which are the focus of many current retrieval development efforts due to their radiative importance and relatively simple structure. Large systematic discrepancies in cloud microphysical properties are found in these two types of clouds among the nine cloud retrieval products, particularly for the cloud liquid and ice particle effective radius. Note that the differences among some retrieval products are even larger than the prescribed uncertainties reported by the retrieval algorithm developers. It is shown that most of these large differences have their roots in the retrieval theoretical bases, assumptions, as well as input and constraint parameters. This study suggests the need to further validate current retrieval theories and assumptions and even the development of new retrieval algorithms with more observations under different cloud regimes.

Url:
DOI: 10.1029/2011JD016792

Links to Exploration step

ISTEX:73F4A0165A4ED262F3B63F601EAD8E0B98542726

Le document en format XML

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<div type="abstract">Accurate observations of cloud microphysical properties are needed for evaluating and improving the representation of cloud processes in climate models and better estimate of the Earth radiative budget. However, large differences are found in current cloud products retrieved from ground‐based remote sensing measurements using various retrieval algorithms. Understanding the differences is an important step to address uncertainties in the cloud retrievals. In this study, an in‐depth analysis of nine existing ground‐based cloud retrievals using ARM remote sensing measurements is carried out. We place emphasis on boundary layer overcast clouds and high level ice clouds, which are the focus of many current retrieval development efforts due to their radiative importance and relatively simple structure. Large systematic discrepancies in cloud microphysical properties are found in these two types of clouds among the nine cloud retrieval products, particularly for the cloud liquid and ice particle effective radius. Note that the differences among some retrieval products are even larger than the prescribed uncertainties reported by the retrieval algorithm developers. It is shown that most of these large differences have their roots in the retrieval theoretical bases, assumptions, as well as input and constraint parameters. This study suggests the need to further validate current retrieval theories and assumptions and even the development of new retrieval algorithms with more observations under different cloud regimes.</div>
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<abstract>Accurate observations of cloud microphysical properties are needed for evaluating and improving the representation of cloud processes in climate models and better estimate of the Earth radiative budget. However, large differences are found in current cloud products retrieved from ground‐based remote sensing measurements using various retrieval algorithms. Understanding the differences is an important step to address uncertainties in the cloud retrievals. In this study, an in‐depth analysis of nine existing ground‐based cloud retrievals using ARM remote sensing measurements is carried out. We place emphasis on boundary layer overcast clouds and high level ice clouds, which are the focus of many current retrieval development efforts due to their radiative importance and relatively simple structure. Large systematic discrepancies in cloud microphysical properties are found in these two types of clouds among the nine cloud retrieval products, particularly for the cloud liquid and ice particle effective radius. Note that the differences among some retrieval products are even larger than the prescribed uncertainties reported by the retrieval algorithm developers. It is shown that most of these large differences have their roots in the retrieval theoretical bases, assumptions, as well as input and constraint parameters. This study suggests the need to further validate current retrieval theories and assumptions and even the development of new retrieval algorithms with more observations under different cloud regimes.</abstract>
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<name type="personal">
<namePart type="given">Robin J.</namePart>
<namePart type="family">Hogan</namePart>
<affiliation>Department of Meteorology, University of Reading, Reading, UK</affiliation>
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<name type="personal">
<namePart type="given">Dong</namePart>
<namePart type="family">Huang</namePart>
<affiliation>Brookhaven National Laboratory, Upton, New York, USA</affiliation>
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<name type="personal">
<namePart type="given">Michael P.</namePart>
<namePart type="family">Jensen</namePart>
<affiliation>Brookhaven National Laboratory, Upton, New York, USA</affiliation>
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<name type="personal">
<namePart type="given">Gerald G.</namePart>
<namePart type="family">Mace</namePart>
<affiliation>Department of Atmospheric Sciences, University of Utah, Salt Lake City, Utah, USA</affiliation>
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<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Renata</namePart>
<namePart type="family">McCoy</namePart>
<affiliation>Lawrence Livermore National Laboratory, Livermore, California, USA</affiliation>
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</role>
</name>
<name type="personal">
<namePart type="given">Ewan J.</namePart>
<namePart type="family">O'Connor</namePart>
<affiliation>Department of Meteorology, University of Reading, Reading, UK</affiliation>
<affiliation>Finnish Meteorological Institute, Helsinki, Finland</affiliation>
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</role>
</name>
<name type="personal">
<namePart type="given">David D.</namePart>
<namePart type="family">Turner</namePart>
<affiliation>National Severe Storms Laboratory, NOAA, Norman, Oklahoma, USA</affiliation>
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<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Zhien</namePart>
<namePart type="family">Wang</namePart>
<affiliation>University of Wyoming, Laramie, Wyoming, USA</affiliation>
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<edition>Zhao, C., et al. (2012), Toward understanding of differences in current cloud retrievals of ARM ground‐based measurements, J. Geophys. Res., 117, D10206, doi:10.1029/2011JD016792.</edition>
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<abstract>Accurate observations of cloud microphysical properties are needed for evaluating and improving the representation of cloud processes in climate models and better estimate of the Earth radiative budget. However, large differences are found in current cloud products retrieved from ground‐based remote sensing measurements using various retrieval algorithms. Understanding the differences is an important step to address uncertainties in the cloud retrievals. In this study, an in‐depth analysis of nine existing ground‐based cloud retrievals using ARM remote sensing measurements is carried out. We place emphasis on boundary layer overcast clouds and high level ice clouds, which are the focus of many current retrieval development efforts due to their radiative importance and relatively simple structure. Large systematic discrepancies in cloud microphysical properties are found in these two types of clouds among the nine cloud retrieval products, particularly for the cloud liquid and ice particle effective radius. Note that the differences among some retrieval products are even larger than the prescribed uncertainties reported by the retrieval algorithm developers. It is shown that most of these large differences have their roots in the retrieval theoretical bases, assumptions, as well as input and constraint parameters. This study suggests the need to further validate current retrieval theories and assumptions and even the development of new retrieval algorithms with more observations under different cloud regimes.</abstract>
<abstract type="short">Large differences exist for cloud properties retrieved from various techniques These differences are highly related to the algorithm details and inputs Cloud retrieval uncertainties need to be further understood and quantified</abstract>
<note type="additional physical form">Tab‐delimited Table 1.Tab‐delimited Table 2.Tab‐delimited Table 3.</note>
<subject>
<genre>keywords</genre>
<topic>cloud retrievals</topic>
<topic>effective radius</topic>
<topic>ice water content</topic>
<topic>liquid water content</topic>
<topic>uncertainties</topic>
</subject>
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<title>Journal of Geophysical Research: Atmospheres</title>
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<title>J. Geophys. Res.</title>
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<topic authorityURI="http://psi.agu.org/subset/AAC">Aerosol and Clouds</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0300">ATMOSPHERIC COMPOSITION AND STRUCTURE</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0320">Cloud physics and chemistry</topic>
</subject>
<subject>
<genre>article-category</genre>
<topic>Aerosol and Clouds</topic>
</subject>
<identifier type="ISSN">0148-0227</identifier>
<identifier type="eISSN">2156-2202</identifier>
<identifier type="DOI">10.1002/(ISSN)2156-2202d</identifier>
<identifier type="CODEN">JGREA2</identifier>
<identifier type="PublisherID">JGRD</identifier>
<part>
<date>2012</date>
<detail type="volume">
<caption>vol.</caption>
<number>117</number>
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<detail type="issue">
<caption>no.</caption>
<number>D10</number>
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<start>n/a</start>
<end>n/a</end>
<total>21</total>
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<identifier type="ark">ark:/67375/WNG-14DN652M-M</identifier>
<identifier type="DOI">10.1029/2011JD016792</identifier>
<identifier type="ArticleID">2011JD016792</identifier>
<accessCondition type="use and reproduction" contentType="copyright">Copyright 2012 by the American Geophysical Union</accessCondition>
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