Potential of Higher-Order Moments and Slopes of the Radar Doppler Spectrum for Retrieving Microphysical and Kinematic Properties of Arctic Ice Clouds

Retrievals of ice-cloud properties from cloud-radar observations are challenging because the retrieval methods are typically underdetermined. Here, the authors investigate whether additional information can be obtained from higher-order moments and the slopes of the radar Doppler spectrum such as sk...

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Main Authors: Maahn, Maximilian, Loehnert, Ulrich
Format: Article in Journal/Newspaper
Language:English
Published: AMER METEOROLOGICAL SOC 2017
Subjects:
Online Access:https://kups.ub.uni-koeln.de/24050/
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spelling ftubkoeln:oai:USBKOELN.ub.uni-koeln.de:24050 2023-05-15T14:25:34+02:00 Potential of Higher-Order Moments and Slopes of the Radar Doppler Spectrum for Retrieving Microphysical and Kinematic Properties of Arctic Ice Clouds Maahn, Maximilian Loehnert, Ulrich 2017 https://kups.ub.uni-koeln.de/24050/ eng eng AMER METEOROLOGICAL SOC Maahn, Maximilian orcid:0000-0002-2580-9100 and Loehnert, Ulrich (2017). Potential of Higher-Order Moments and Slopes of the Radar Doppler Spectrum for Retrieving Microphysical and Kinematic Properties of Arctic Ice Clouds. J. Appl. Meteorol. Climatol., 56 (2). S. 263 - 283. BOSTON: AMER METEOROLOGICAL SOC. ISSN 1558-8432 ddc:no doc-type:article publishedVersion 2017 ftubkoeln 2022-11-09T07:19:34Z Retrievals of ice-cloud properties from cloud-radar observations are challenging because the retrieval methods are typically underdetermined. Here, the authors investigate whether additional information can be obtained from higher-order moments and the slopes of the radar Doppler spectrum such as skewness and kurtosis as well as the slopes of the Doppler peak. To estimate quantitatively the additional information content, a generalized Bayesian retrieval framework that is based on optimal estimation is developed. Real and synthetic cloud-radar observations of the Indirect and Semi-Direct Aerosol Campaign (ISDAC) dataset obtained around Barrow, Alaska, are used in this study. The state vector consists of the microphysical (particle-size distribution, mass-size relation, and cross section-area relation) and kinematic (vertical wind and turbulence) quantities required to forward model the moments and slopes of the radar Doppler spectrum. It is found that, for a single radar frequency, more information can be retrieved when including higher-order moments and slopes than when using only reflectivity and mean Doppler velocity but two radar frequencies. When using all moments and slopes with two or even three frequencies, the uncertainties of all state variables, including the mass-size relation, can be considerably reduced with respect to the prior knowledge. Article in Journal/Newspaper Arctic Arctic Barrow Alaska Cologne University: KUPS Arctic
institution Open Polar
collection Cologne University: KUPS
op_collection_id ftubkoeln
language English
topic ddc:no
spellingShingle ddc:no
Maahn, Maximilian
Loehnert, Ulrich
Potential of Higher-Order Moments and Slopes of the Radar Doppler Spectrum for Retrieving Microphysical and Kinematic Properties of Arctic Ice Clouds
topic_facet ddc:no
description Retrievals of ice-cloud properties from cloud-radar observations are challenging because the retrieval methods are typically underdetermined. Here, the authors investigate whether additional information can be obtained from higher-order moments and the slopes of the radar Doppler spectrum such as skewness and kurtosis as well as the slopes of the Doppler peak. To estimate quantitatively the additional information content, a generalized Bayesian retrieval framework that is based on optimal estimation is developed. Real and synthetic cloud-radar observations of the Indirect and Semi-Direct Aerosol Campaign (ISDAC) dataset obtained around Barrow, Alaska, are used in this study. The state vector consists of the microphysical (particle-size distribution, mass-size relation, and cross section-area relation) and kinematic (vertical wind and turbulence) quantities required to forward model the moments and slopes of the radar Doppler spectrum. It is found that, for a single radar frequency, more information can be retrieved when including higher-order moments and slopes than when using only reflectivity and mean Doppler velocity but two radar frequencies. When using all moments and slopes with two or even three frequencies, the uncertainties of all state variables, including the mass-size relation, can be considerably reduced with respect to the prior knowledge.
format Article in Journal/Newspaper
author Maahn, Maximilian
Loehnert, Ulrich
author_facet Maahn, Maximilian
Loehnert, Ulrich
author_sort Maahn, Maximilian
title Potential of Higher-Order Moments and Slopes of the Radar Doppler Spectrum for Retrieving Microphysical and Kinematic Properties of Arctic Ice Clouds
title_short Potential of Higher-Order Moments and Slopes of the Radar Doppler Spectrum for Retrieving Microphysical and Kinematic Properties of Arctic Ice Clouds
title_full Potential of Higher-Order Moments and Slopes of the Radar Doppler Spectrum for Retrieving Microphysical and Kinematic Properties of Arctic Ice Clouds
title_fullStr Potential of Higher-Order Moments and Slopes of the Radar Doppler Spectrum for Retrieving Microphysical and Kinematic Properties of Arctic Ice Clouds
title_full_unstemmed Potential of Higher-Order Moments and Slopes of the Radar Doppler Spectrum for Retrieving Microphysical and Kinematic Properties of Arctic Ice Clouds
title_sort potential of higher-order moments and slopes of the radar doppler spectrum for retrieving microphysical and kinematic properties of arctic ice clouds
publisher AMER METEOROLOGICAL SOC
publishDate 2017
url https://kups.ub.uni-koeln.de/24050/
geographic Arctic
geographic_facet Arctic
genre Arctic
Arctic
Barrow
Alaska
genre_facet Arctic
Arctic
Barrow
Alaska
op_relation Maahn, Maximilian orcid:0000-0002-2580-9100 and Loehnert, Ulrich (2017). Potential of Higher-Order Moments and Slopes of the Radar Doppler Spectrum for Retrieving Microphysical and Kinematic Properties of Arctic Ice Clouds. J. Appl. Meteorol. Climatol., 56 (2). S. 263 - 283. BOSTON: AMER METEOROLOGICAL SOC. ISSN 1558-8432
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