Synergistic radar and radiometer retrievals of ice hydrometeors

<p>Remote sensing observations at sub-millimeter wavelengths provide higher sensitivity to small hydrometeors and low water content than observations at millimeter wavelengths, which are traditionally used to observe clouds and precipitation. They are employed increasingly in field campaigns t...

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Main Authors: S. Pfreundschuh, P. Eriksson, S. A. Buehler, M. Brath, D. Duncan, R. Larsson, R. Ekelund
Format: Article
Language:English
Published: Copernicus Publications 2020-08-01
Series:Atmospheric Measurement Techniques
Online Access:https://amt.copernicus.org/articles/13/4219/2020/amt-13-4219-2020.pdf
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author S. Pfreundschuh
P. Eriksson
S. A. Buehler
M. Brath
D. Duncan
D. Duncan
R. Larsson
R. Ekelund
author_facet S. Pfreundschuh
P. Eriksson
S. A. Buehler
M. Brath
D. Duncan
D. Duncan
R. Larsson
R. Ekelund
author_sort S. Pfreundschuh
collection DOAJ
description <p>Remote sensing observations at sub-millimeter wavelengths provide higher sensitivity to small hydrometeors and low water content than observations at millimeter wavelengths, which are traditionally used to observe clouds and precipitation. They are employed increasingly in field campaigns to study cloud microphysics and will be integrated into the global meteorological observing system to measure the global distribution of ice in the atmosphere with the launch of the Ice Cloud Imager (ICI) radiometer on board the second generation of European operational meteorological satellites (Metop-SG). Observations at these novel wavelengths provide valuable information not only on their own but also in combination with complementary observations at other wavelengths. This study investigates the potential of combining passive sub-millimeter radiometer observations with a hypothetical W-band cloud radar for the retrieval of frozen hydrometeors. An idealized cloud model is used to investigate the information content of the combined observations and establish their capacity to constrain the microphysical properties of ice hydrometeors. A synergistic retrieval algorithm for airborne observations is proposed and applied to simulated observations from a cloud-resolving model. Results from the synergistic retrieval are compared to equivalent radar- and passive-only implementations in order to assess the benefits of the synergistic sensor configuration. The impact of the assumed ice particle shape on the retrieval results is assessed for all retrieval implementations. We find that the combined observations better constrain the microphysical properties of ice hydrometeors, which reduces uncertainties in retrieved ice water content and particle number concentrations for suitable choices of the ice particle model. Analysis of the retrieval information content shows that, although the radar contributes the largest part of the information in the combined retrieval, the radiometer observations provide complementary information over a wide range of atmospheric states. Furthermore, the combined observations yield slightly improved retrievals of liquid cloud water in mixed-phase clouds, pointing towards another potential application of combined radar–radiometer observations.</p>
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spelling doaj.art-f50748aacfb24be3a78225763b6c0b7c2022-12-22T01:55:26ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482020-08-01134219424510.5194/amt-13-4219-2020Synergistic radar and radiometer retrievals of ice hydrometeorsS. Pfreundschuh0P. Eriksson1S. A. Buehler2M. Brath3D. Duncan4D. Duncan5R. Larsson6R. Ekelund7Department of Space, Earth and Environment, Chalmers University of Technology, 41296 Gothenburg, SwedenDepartment of Space, Earth and Environment, Chalmers University of Technology, 41296 Gothenburg, SwedenMeteorologisches Institut, Fachbereich Geowissenschaften, Centrum für Erdsystem und Nachhaltigkeitsforschung (CEN), Universität Hamburg, Bundesstraße 55, 20146 Hamburg, GermanyMeteorologisches Institut, Fachbereich Geowissenschaften, Centrum für Erdsystem und Nachhaltigkeitsforschung (CEN), Universität Hamburg, Bundesstraße 55, 20146 Hamburg, GermanyDepartment of Space, Earth and Environment, Chalmers University of Technology, 41296 Gothenburg, Swedennow at: European Centre for Medium-Range Weather Forecasts, Shinfield Park, Reading RG2 9AX, UKMax Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, 37077 Göttingen, GermanyDepartment of Space, Earth and Environment, Chalmers University of Technology, 41296 Gothenburg, Sweden<p>Remote sensing observations at sub-millimeter wavelengths provide higher sensitivity to small hydrometeors and low water content than observations at millimeter wavelengths, which are traditionally used to observe clouds and precipitation. They are employed increasingly in field campaigns to study cloud microphysics and will be integrated into the global meteorological observing system to measure the global distribution of ice in the atmosphere with the launch of the Ice Cloud Imager (ICI) radiometer on board the second generation of European operational meteorological satellites (Metop-SG). Observations at these novel wavelengths provide valuable information not only on their own but also in combination with complementary observations at other wavelengths. This study investigates the potential of combining passive sub-millimeter radiometer observations with a hypothetical W-band cloud radar for the retrieval of frozen hydrometeors. An idealized cloud model is used to investigate the information content of the combined observations and establish their capacity to constrain the microphysical properties of ice hydrometeors. A synergistic retrieval algorithm for airborne observations is proposed and applied to simulated observations from a cloud-resolving model. Results from the synergistic retrieval are compared to equivalent radar- and passive-only implementations in order to assess the benefits of the synergistic sensor configuration. The impact of the assumed ice particle shape on the retrieval results is assessed for all retrieval implementations. We find that the combined observations better constrain the microphysical properties of ice hydrometeors, which reduces uncertainties in retrieved ice water content and particle number concentrations for suitable choices of the ice particle model. Analysis of the retrieval information content shows that, although the radar contributes the largest part of the information in the combined retrieval, the radiometer observations provide complementary information over a wide range of atmospheric states. Furthermore, the combined observations yield slightly improved retrievals of liquid cloud water in mixed-phase clouds, pointing towards another potential application of combined radar–radiometer observations.</p>https://amt.copernicus.org/articles/13/4219/2020/amt-13-4219-2020.pdf
spellingShingle S. Pfreundschuh
P. Eriksson
S. A. Buehler
M. Brath
D. Duncan
D. Duncan
R. Larsson
R. Ekelund
Synergistic radar and radiometer retrievals of ice hydrometeors
Atmospheric Measurement Techniques
title Synergistic radar and radiometer retrievals of ice hydrometeors
title_full Synergistic radar and radiometer retrievals of ice hydrometeors
title_fullStr Synergistic radar and radiometer retrievals of ice hydrometeors
title_full_unstemmed Synergistic radar and radiometer retrievals of ice hydrometeors
title_short Synergistic radar and radiometer retrievals of ice hydrometeors
title_sort synergistic radar and radiometer retrievals of ice hydrometeors
url https://amt.copernicus.org/articles/13/4219/2020/amt-13-4219-2020.pdf
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