Unsupervised classification of vertical profiles of dual polarization radar variables
<p>Vertical profiles of polarimetric radar variables can be used to identify fingerprints of snow growth processes. In order to systematically study such manifestations of precipitation processes, we have developed an unsupervised classification method. The method is based on <span class=&q...
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doaj-e7c254c43c8542f0b5935d1231e1ab202020-11-25T02:51:11ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482020-03-01131227124110.5194/amt-13-1227-2020Unsupervised classification of vertical profiles of dual polarization radar variablesJ. Tiira0D. Moisseev1D. Moisseev2Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, FinlandInstitute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, FinlandFinnish Meteorological Institute, Helsinki, Finland<p>Vertical profiles of polarimetric radar variables can be used to identify fingerprints of snow growth processes. In order to systematically study such manifestations of precipitation processes, we have developed an unsupervised classification method. The method is based on <span class="inline-formula"><i>k</i></span>-means clustering of vertical profiles of polarimetric radar variables, namely reflectivity, differential reflectivity and specific differential phase. For rain events, the classification is applied to radar profiles truncated at the melting layer top. For the snowfall cases, the surface air temperature is used as an additional input parameter. The proposed unsupervised classification was applied to 3.5 years of data collected by the Finnish Meteorological Institute Ikaalinen radar. The vertical profiles of radar variables were computed above the University of Helsinki Hyytiälä station, located 64 km east of the radar. Using these data, we show that the profiles of radar variables can be grouped into 10 and 16 classes for rainfall and snowfall events, respectively. These classes seem to capture most important snow growth and ice cloud processes. Using this classification, the main features of the precipitation formation processes, as observed in Finland, are presented.</p>https://www.atmos-meas-tech.net/13/1227/2020/amt-13-1227-2020.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
J. Tiira D. Moisseev D. Moisseev |
spellingShingle |
J. Tiira D. Moisseev D. Moisseev Unsupervised classification of vertical profiles of dual polarization radar variables Atmospheric Measurement Techniques |
author_facet |
J. Tiira D. Moisseev D. Moisseev |
author_sort |
J. Tiira |
title |
Unsupervised classification of vertical profiles of dual polarization radar variables |
title_short |
Unsupervised classification of vertical profiles of dual polarization radar variables |
title_full |
Unsupervised classification of vertical profiles of dual polarization radar variables |
title_fullStr |
Unsupervised classification of vertical profiles of dual polarization radar variables |
title_full_unstemmed |
Unsupervised classification of vertical profiles of dual polarization radar variables |
title_sort |
unsupervised classification of vertical profiles of dual polarization radar variables |
publisher |
Copernicus Publications |
series |
Atmospheric Measurement Techniques |
issn |
1867-1381 1867-8548 |
publishDate |
2020-03-01 |
description |
<p>Vertical profiles of polarimetric radar variables can be used to identify fingerprints of snow growth processes. In order to systematically study such manifestations of precipitation processes, we have developed an unsupervised classification method. The method is based on <span class="inline-formula"><i>k</i></span>-means clustering of vertical profiles of polarimetric radar variables, namely reflectivity, differential reflectivity and specific differential phase. For rain events, the classification is applied to radar profiles truncated at the melting layer top. For the snowfall cases, the surface air temperature is used as an additional input parameter.
The proposed unsupervised classification was applied to 3.5 years of data collected by the Finnish Meteorological Institute Ikaalinen radar. The vertical profiles of radar variables were computed above the University of Helsinki Hyytiälä station, located 64 km east of the radar. Using these data, we show that the profiles of radar variables can be grouped into 10 and 16 classes for rainfall and snowfall events, respectively. These classes seem to capture most important snow growth and ice cloud processes. Using this classification, the main features of the precipitation formation processes, as observed in Finland, are presented.</p> |
url |
https://www.atmos-meas-tech.net/13/1227/2020/amt-13-1227-2020.pdf |
work_keys_str_mv |
AT jtiira unsupervisedclassificationofverticalprofilesofdualpolarizationradarvariables AT dmoisseev unsupervisedclassificationofverticalprofilesofdualpolarizationradarvariables AT dmoisseev unsupervisedclassificationofverticalprofilesofdualpolarizationradarvariables |
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1724735864009916416 |