Can liquid cloud microphysical processes be used for vertically pointing cloud radar calibration?

Cloud radars are unique instruments for observing cloud processes, but uncertainties in radar calibration have frequently limited data quality. Thus far, no single robust method exists for assessing the calibration of past cloud radar data sets. Here, we investigate whether observations of microphys...

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Published in:Atmospheric Measurement Techniques
Main Authors: M. Maahn, F. Hoffmann, M. D. Shupe, G. de Boer, S. Y. Matrosov, E. P. Luke
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2019
Subjects:
Online Access:https://doi.org/10.5194/amt-12-3151-2019
https://doaj.org/article/32f3a5ab115141a0b0e8e51379327686
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spelling ftdoajarticles:oai:doaj.org/article:32f3a5ab115141a0b0e8e51379327686 2023-05-15T17:40:15+02:00 Can liquid cloud microphysical processes be used for vertically pointing cloud radar calibration? M. Maahn F. Hoffmann M. D. Shupe G. de Boer S. Y. Matrosov E. P. Luke 2019-06-01T00:00:00Z https://doi.org/10.5194/amt-12-3151-2019 https://doaj.org/article/32f3a5ab115141a0b0e8e51379327686 EN eng Copernicus Publications https://www.atmos-meas-tech.net/12/3151/2019/amt-12-3151-2019.pdf https://doaj.org/toc/1867-1381 https://doaj.org/toc/1867-8548 doi:10.5194/amt-12-3151-2019 1867-1381 1867-8548 https://doaj.org/article/32f3a5ab115141a0b0e8e51379327686 Atmospheric Measurement Techniques, Vol 12, Pp 3151-3171 (2019) Environmental engineering TA170-171 Earthwork. Foundations TA715-787 article 2019 ftdoajarticles https://doi.org/10.5194/amt-12-3151-2019 2022-12-31T03:47:08Z Cloud radars are unique instruments for observing cloud processes, but uncertainties in radar calibration have frequently limited data quality. Thus far, no single robust method exists for assessing the calibration of past cloud radar data sets. Here, we investigate whether observations of microphysical processes in liquid clouds such as the transition of cloud droplets to drizzle drops can be used to calibrate cloud radars. Specifically, we study the relationships between the radar reflectivity factor and three variables not affected by absolute radar calibration: the skewness of the radar Doppler spectrum ( γ ), the radar mean Doppler velocity ( W ), and the liquid water path (LWP). For each relation, we evaluate the potential for radar calibration. For γ and W , we use box model simulations to determine typical radar reflectivity values for reference points. We apply the new methods to observations at the Atmospheric Radiation Measurement (ARM) sites North Slope of Alaska (NSA) and Oliktok Point (OLI) in 2016 using two 35 GHz K a -band ARM Zenith Radars (KAZR). For periods with a sufficient number of liquid cloud observations, we find that liquid cloud processes are robust enough for cloud radar calibration, with the LWP-based method performing best. We estimate that, in 2016, the radar reflectivity at NSA was about 1±1 dB too low but stable. For OLI, we identify serious problems with maintaining an accurate calibration including a sudden decrease of 5 to 7 dB in June 2016. Article in Journal/Newspaper north slope Alaska Directory of Open Access Journals: DOAJ Articles Atmospheric Measurement Techniques 12 6 3151 3171
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental engineering
TA170-171
Earthwork. Foundations
TA715-787
spellingShingle Environmental engineering
TA170-171
Earthwork. Foundations
TA715-787
M. Maahn
F. Hoffmann
M. D. Shupe
G. de Boer
S. Y. Matrosov
E. P. Luke
Can liquid cloud microphysical processes be used for vertically pointing cloud radar calibration?
topic_facet Environmental engineering
TA170-171
Earthwork. Foundations
TA715-787
description Cloud radars are unique instruments for observing cloud processes, but uncertainties in radar calibration have frequently limited data quality. Thus far, no single robust method exists for assessing the calibration of past cloud radar data sets. Here, we investigate whether observations of microphysical processes in liquid clouds such as the transition of cloud droplets to drizzle drops can be used to calibrate cloud radars. Specifically, we study the relationships between the radar reflectivity factor and three variables not affected by absolute radar calibration: the skewness of the radar Doppler spectrum ( γ ), the radar mean Doppler velocity ( W ), and the liquid water path (LWP). For each relation, we evaluate the potential for radar calibration. For γ and W , we use box model simulations to determine typical radar reflectivity values for reference points. We apply the new methods to observations at the Atmospheric Radiation Measurement (ARM) sites North Slope of Alaska (NSA) and Oliktok Point (OLI) in 2016 using two 35 GHz K a -band ARM Zenith Radars (KAZR). For periods with a sufficient number of liquid cloud observations, we find that liquid cloud processes are robust enough for cloud radar calibration, with the LWP-based method performing best. We estimate that, in 2016, the radar reflectivity at NSA was about 1±1 dB too low but stable. For OLI, we identify serious problems with maintaining an accurate calibration including a sudden decrease of 5 to 7 dB in June 2016.
format Article in Journal/Newspaper
author M. Maahn
F. Hoffmann
M. D. Shupe
G. de Boer
S. Y. Matrosov
E. P. Luke
author_facet M. Maahn
F. Hoffmann
M. D. Shupe
G. de Boer
S. Y. Matrosov
E. P. Luke
author_sort M. Maahn
title Can liquid cloud microphysical processes be used for vertically pointing cloud radar calibration?
title_short Can liquid cloud microphysical processes be used for vertically pointing cloud radar calibration?
title_full Can liquid cloud microphysical processes be used for vertically pointing cloud radar calibration?
title_fullStr Can liquid cloud microphysical processes be used for vertically pointing cloud radar calibration?
title_full_unstemmed Can liquid cloud microphysical processes be used for vertically pointing cloud radar calibration?
title_sort can liquid cloud microphysical processes be used for vertically pointing cloud radar calibration?
publisher Copernicus Publications
publishDate 2019
url https://doi.org/10.5194/amt-12-3151-2019
https://doaj.org/article/32f3a5ab115141a0b0e8e51379327686
genre north slope
Alaska
genre_facet north slope
Alaska
op_source Atmospheric Measurement Techniques, Vol 12, Pp 3151-3171 (2019)
op_relation https://www.atmos-meas-tech.net/12/3151/2019/amt-12-3151-2019.pdf
https://doaj.org/toc/1867-1381
https://doaj.org/toc/1867-8548
doi:10.5194/amt-12-3151-2019
1867-1381
1867-8548
https://doaj.org/article/32f3a5ab115141a0b0e8e51379327686
op_doi https://doi.org/10.5194/amt-12-3151-2019
container_title Atmospheric Measurement Techniques
container_volume 12
container_issue 6
container_start_page 3151
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