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Evidence of ice crystals at cloud top of Arctic boundary-layer mixed-phase clouds derived from airborne remote sensing

Ehrlich, A. and Wendisch, M. and Bierwirth, E. and Gayet, J.-F. and Mioche, G. and Lampert, A. and Mayer, B. (2009) Evidence of ice crystals at cloud top of Arctic boundary-layer mixed-phase clouds derived from airborne remote sensing. Atmospheric Chemistry and Physics (9), pp. 9401-9416. Copernicus Publications.

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Official URL: http://www.atmos-chem-phys.net/9/9401/2009/acp-9-9401-2009.html

Abstract

The vertical distribution of ice crystals in Arctic boundary-layer mixed-phase (ABM) clouds was investigated by airborne remote-sensing and in situ measurements during the Arctic Study of Tropospheric Aerosol, Clouds and Radiation (ASTAR) campaign in March and April 2007. Information on the spectral absorption of solar radiation by ice and liquid water cloud particles is derived from airborne measurements of solar spectral radiation reflected by these clouds. It is shown by calculation of the vertical weighting function of the measurements that the observed absorption of solar radiation is dominated by the upper cloud layers (50% within 200 m from cloud top). This vertical weighting function is shifted even closer to cloud top for wavelengths where absorption by ice dominates. On this basis an indicator of the vertical distribution of ice crystals in ABM clouds is designed. Applying in situ measured microphysical properties, the cloud-top reflectivity was calculated by radiative transfer simulations and compared to the measurements. It is found that ice crystals near cloud top (mixed-phase cloud top layer) are necessary to reproduce the measurements at wavelengths where absorption by ice dominates. The observation of backscatter glories on the cloud top generally indicating liquid water droplets does not contradict the postulated presence of ice crystals. Radiative transfer simulations reproduce the observed glories even if the cloud top layer is of mixed-phase character.

Item URL in elib:https://elib.dlr.de/61871/
Document Type:Article
Title:Evidence of ice crystals at cloud top of Arctic boundary-layer mixed-phase clouds derived from airborne remote sensing
Authors:
AuthorsInstitution or Email of AuthorsAuthors ORCID iD
Ehrlich, A.Johannes Gutenberg-Univ. Mainz, MainzUNSPECIFIED
Wendisch, M.Johannes Gutenberg-Univ. Mainz, MainzUNSPECIFIED
Bierwirth, E.Univ. of Colorado, Boulder, USAUNSPECIFIED
Gayet, J.-F.Univ. Blaise Pascal, Aubière Cedex, FUNSPECIFIED
Mioche, G.Univ. Blaise Pascal, Aubière Cedex, FUNSPECIFIED
Lampert, A.AWI, PotsdamUNSPECIFIED
Mayer, B.DLRUNSPECIFIED
Date:2009
Journal or Publication Title:Atmospheric Chemistry and Physics
Refereed publication:Yes
Open Access:Yes
Gold Open Access:Yes
In SCOPUS:Yes
In ISI Web of Science:Yes
Page Range:pp. 9401-9416
Publisher:Copernicus Publications
Status:Published
Keywords:Mixed phase clouds, ice phase, radiative transfer, backscatter glory
HGF - Research field:Aeronautics, Space and Transport (old)
HGF - Program:Space (old)
HGF - Program Themes:W EO - Erdbeobachtung
DLR - Research area:Space
DLR - Program:W EO - Erdbeobachtung
DLR - Research theme (Project):W - Vorhaben Atmosphären- und Klimaforschung (old)
Location: Oberpfaffenhofen
Institutes and Institutions:Institute of Atmospheric Physics > Atmospheric Remote Sensing
Deposited By: Mayer, Dr.rer.nat. Bernhard
Deposited On:16 Dec 2009 12:14
Last Modified:02 May 2019 14:03

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