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...

Full description

Bibliographic Details
Main Authors: J. Tiira, D. Moisseev
Format: Article
Language:English
Published: Copernicus Publications 2020-03-01
Series:Atmospheric Measurement Techniques
Online Access:https://www.atmos-meas-tech.net/13/1227/2020/amt-13-1227-2020.pdf
id doaj-e7c254c43c8542f0b5935d1231e1ab20
record_format Article
spelling 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&thinsp;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&thinsp;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
_version_ 1724735864009916416