Evaluating cloud liquid detection using cloud radar Doppler spectra in a pre-trained artificial neural network against Cloudnet liquid detection
Detection of liquid-containing cloud layers in thick mixed-phase clouds or multi-layer cloud situations from ground-based remote sensing instruments still pose observational challenges yet improvements are crucial since the existence of multi-layer liquid layers in mixed-phase cloud situations influe...
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ftcopernicus:oai:publications.copernicus.org:amtd93252 2023-05-15T15:19:13+02:00 Evaluating cloud liquid detection using cloud radar Doppler spectra in a pre-trained artificial neural network against Cloudnet liquid detection Kalesse-Los, Heike Schimmel, Willi Luke, Edward Seifert, Patric 2021-06-07 application/pdf https://doi.org/10.5194/amt-2021-60 https://amt.copernicus.org/preprints/amt-2021-60/ eng eng doi:10.5194/amt-2021-60 https://amt.copernicus.org/preprints/amt-2021-60/ eISSN: 1867-8548 Text 2021 ftcopernicus https://doi.org/10.5194/amt-2021-60 2021-06-14T16:22:15Z Detection of liquid-containing cloud layers in thick mixed-phase clouds or multi-layer cloud situations from ground-based remote sensing instruments still pose observational challenges yet improvements are crucial since the existence of multi-layer liquid layers in mixed-phase cloud situations influences cloud radiative effects, cloud life time, and precipitation formation processes. Hydrometeor target classifications such as Cloudnet that require a lidar signal for the classification of liquid are limited to the maximum height of lidar signal penetration and thus often lead to underestimations of liquid-containing cloud layers. Here we evaluate the Cloudnet liquid detection against the approach of Luke et al. (2010) which extracts morphological features in cloud-penetrating cloud radar Doppler spectra measurements in a artificial neural network (ANN) approach to classify liquid beyond full lidar signal attenuation based on the simulation of the two lidar parameters particle backscatter coefficient and particle depolarization ratio. We show that the ANN of Luke et al. (2010) which was trained in Arctic conditions can successfully be applied to observations in the mid-latitudes obtained during the seven-week long ACCEPT field experiment in Cabauw, the Netherlands, 2014. In a sensitivity study covering the whole duration of the ACCEPT campaign, different liquid-detection thresholds for ANN-predicted lidar variables are applied and evaluated against the Cloudnet target classification. Independent validation of the liquid mask from the standard Cloudnet target classification against the ANN-based technique is realized by comparisons to observations of microwave radiometer liquid water path, ceilometer liquid-layer base altitude, and radiosonde relative humidity. Four conclusions were drawn from the investigation: First, it was found that the threshold selection criteria of liquid-related lidar backscatter and depolarization alone control the liquid detection considerably. Second, nevertheless, all threshold values used in the ANN-framework were found to outperform the Cloudnet target classification for deep or multi-layer cloud situations where the lidar signal is fully attenuated within low liquid layers and the cloud reflectivity in higher cloud layers was sufficiently high to be detectable by the cloud radar. Third, in convective situations for which lidar data is available and for which the imprint of cloud microphysics on the radar Doppler spectrum is decreased, Cloudnet outperforms the ANN retrieval. Fourth, in high-level clouds both approaches (Cloudnet and the ANN technique), are limited. Text Arctic Copernicus Publications: E-Journals Arctic Luke ENVELOPE(-94.855,-94.855,56.296,56.296) |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
Detection of liquid-containing cloud layers in thick mixed-phase clouds or multi-layer cloud situations from ground-based remote sensing instruments still pose observational challenges yet improvements are crucial since the existence of multi-layer liquid layers in mixed-phase cloud situations influences cloud radiative effects, cloud life time, and precipitation formation processes. Hydrometeor target classifications such as Cloudnet that require a lidar signal for the classification of liquid are limited to the maximum height of lidar signal penetration and thus often lead to underestimations of liquid-containing cloud layers. Here we evaluate the Cloudnet liquid detection against the approach of Luke et al. (2010) which extracts morphological features in cloud-penetrating cloud radar Doppler spectra measurements in a artificial neural network (ANN) approach to classify liquid beyond full lidar signal attenuation based on the simulation of the two lidar parameters particle backscatter coefficient and particle depolarization ratio. We show that the ANN of Luke et al. (2010) which was trained in Arctic conditions can successfully be applied to observations in the mid-latitudes obtained during the seven-week long ACCEPT field experiment in Cabauw, the Netherlands, 2014. In a sensitivity study covering the whole duration of the ACCEPT campaign, different liquid-detection thresholds for ANN-predicted lidar variables are applied and evaluated against the Cloudnet target classification. Independent validation of the liquid mask from the standard Cloudnet target classification against the ANN-based technique is realized by comparisons to observations of microwave radiometer liquid water path, ceilometer liquid-layer base altitude, and radiosonde relative humidity. Four conclusions were drawn from the investigation: First, it was found that the threshold selection criteria of liquid-related lidar backscatter and depolarization alone control the liquid detection considerably. Second, nevertheless, all threshold values used in the ANN-framework were found to outperform the Cloudnet target classification for deep or multi-layer cloud situations where the lidar signal is fully attenuated within low liquid layers and the cloud reflectivity in higher cloud layers was sufficiently high to be detectable by the cloud radar. Third, in convective situations for which lidar data is available and for which the imprint of cloud microphysics on the radar Doppler spectrum is decreased, Cloudnet outperforms the ANN retrieval. Fourth, in high-level clouds both approaches (Cloudnet and the ANN technique), are limited. |
format |
Text |
author |
Kalesse-Los, Heike Schimmel, Willi Luke, Edward Seifert, Patric |
spellingShingle |
Kalesse-Los, Heike Schimmel, Willi Luke, Edward Seifert, Patric Evaluating cloud liquid detection using cloud radar Doppler spectra in a pre-trained artificial neural network against Cloudnet liquid detection |
author_facet |
Kalesse-Los, Heike Schimmel, Willi Luke, Edward Seifert, Patric |
author_sort |
Kalesse-Los, Heike |
title |
Evaluating cloud liquid detection using cloud radar Doppler spectra in a pre-trained artificial neural network against Cloudnet liquid detection |
title_short |
Evaluating cloud liquid detection using cloud radar Doppler spectra in a pre-trained artificial neural network against Cloudnet liquid detection |
title_full |
Evaluating cloud liquid detection using cloud radar Doppler spectra in a pre-trained artificial neural network against Cloudnet liquid detection |
title_fullStr |
Evaluating cloud liquid detection using cloud radar Doppler spectra in a pre-trained artificial neural network against Cloudnet liquid detection |
title_full_unstemmed |
Evaluating cloud liquid detection using cloud radar Doppler spectra in a pre-trained artificial neural network against Cloudnet liquid detection |
title_sort |
evaluating cloud liquid detection using cloud radar doppler spectra in a pre-trained artificial neural network against cloudnet liquid detection |
publishDate |
2021 |
url |
https://doi.org/10.5194/amt-2021-60 https://amt.copernicus.org/preprints/amt-2021-60/ |
long_lat |
ENVELOPE(-94.855,-94.855,56.296,56.296) |
geographic |
Arctic Luke |
geographic_facet |
Arctic Luke |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
eISSN: 1867-8548 |
op_relation |
doi:10.5194/amt-2021-60 https://amt.copernicus.org/preprints/amt-2021-60/ |
op_doi |
https://doi.org/10.5194/amt-2021-60 |
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1766349394014109696 |