Hydrometeor classification through statistical clustering of polarimetric radar measurements: a semi-supervised approach
Atmos. Meas. Tech., 9, 4425–4445, 2016
www.atmos-meas-tech.net/9/4425/2016/
doi:10.5194/amt-9-4425-2016
© Author(s) 2016. CC Attribution 3.0 License.
Hydrometeor classification through statistical clustering of
polarimetric radar measurements: a semi-supervised approach
Nikola Besic1,2 , Jordi Figueras i Ventura2 , Jacopo Grazioli1 , Marco Gabella2 , Urs Germann2 , and Alexis Berne1
1 Environmental Remote Sensing Laboratory (LTE), École Polytechnique Fédérale
de Lausanne (EPFL), Lausanne, Switzerland
2 Radar, Satellite and Nowcasting Department, MeteoSwiss, Locarno-Monti, Switzerland
Correspondence to: Nikola Besic ()
Received: 29 March 2016 – Published in Atmos. Meas. Tech. Discuss.: 30 March 2016
Revised: 24 August 2016 – Accepted: 25 August 2016 – Published: 8 September 2016
Abstract. Polarimetric radar-based hydrometeor classification is the procedure of identifying different types of hydrometeors by exploiting polarimetric radar observations.
The main drawback of the existing supervised classification
methods, mostly based on fuzzy logic, is a significant dependency on a presumed electromagnetic behaviour of different hydrometeor types. Namely, the results of the classification largely rely upon the quality of scattering simulations. When it comes to the unsupervised approach, it lacks
the constraints related to the hydrometeor microphysics. The
idea of the proposed method is to compensate for these drawbacks by combining the two approaches in a way that microphysical hypotheses can, to a degree, adjust the content
of the classes obtained statistically from the observations.
This is done by means of an iterative approach, performed
offline, which, in a statistical framework, examines clustered
representative polarimetric observations by comparing them
to the presumed polarimetric properties of each hydrometeor class. Aside from comparing, a routine alters the content of clusters by encouraging further statistical clustering
in case of non-identification. By merging all identified clusters, the multi-dimensional polarimetric signatures of various hydrometeor types are obtained for each of the studied
representative datasets, i.e. for each radar system of interest. These are depicted by sets of centroids which are then
employed in operational labelling of different hydrometeors.
The method has been applied on three C-band datasets, each
acquired by different operational radar from the MeteoSwiss
Rad4Alp network, as well as on two X-band datasets acquired by two research mobile radars. The results are discussed through a comparative analysis which includes a cor-
responding supervised and unsupervised approach, emphasising the operational potential of the proposed method.
1
Introduction
Radar-based hydrometeor classification, that is the proper
identification of different types of hydrometeors from radar
observations, is important for an improved understanding of
atmospheric dynamics, an improved quantitative precipitation estimation (QPE), an improved verification and assimilation in numerical weather prediction models and operational nowcasting applications like aircraft or road safety
(Bringi et al., 2007). The spread of polarimetry for weather
radar has significantly changed the capability of radar systems to identify meteorological and non-meteorological
echoes, as well as to identify different hydrometeor types under the radar umbrella (Bringi et al., 2007). The very first
efforts to overcome the ambiguity arising from the overlap
of measured reflectivity for different hydrometeors relied on
a dual-polarisation parameter – the differential reflectivity
(Seliga and Bringi, 1976; Hall et al., 1984). Since then, various methods, incorporating other Doppler dual-polarisation
(called polarimetric hereafter) parameters, have been developed for the three frequency bands of major interest (S, C
and X) (Bringi et al., 2007). Conceptually, all these methods can be categorised as supervised, unsupervised or semisupervised (Fig. 1).
Being by far the largest (Chandrasekar et al., 2013),
the first category encompasses mostly approaches based on
Boolean logic decision tree, Bayesian theory and the most
Published by Copernicus Publications on behalf of the European Geosciences Union.
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N. Besic et al.: Hydrometeor classification through statistical clustering of polarimetric radar measurements
Figure 1. Schematic generalisation of hydrometeor classification
methods.
intuitive ones, based on fuzzy logic. The common ground
for these seemingly different approaches is a necessity for
a very reliable set of polarimetric signatures (Straka et al.,
2000). These are obtained either by means of simulations
(e.g. Dolan and Rutledge, 2009) or by additionally involving some empirical knowledge (e.g. Al-Sakka et al., 2013).
Boolean logic decision tree methods are part of the earliest efforts to exploit radar polarimetry for the purpose of hydrometeor classification (Straka and Zrnic, 1993; El-Magd
et al., 2000). However, assuming mutual exclusivity of polarimetric parameters for different hydrometeor types, these
methods could not thoroughly exploit the potential of polarimetric measurements.
Fuzzy logic has been considered to be the best way to
make use of polarimetric signatures known a priori in distinguishing between different hydrometeors (Vivekanandan
et al., 1999). Namely, inference combining matching scores
of different parameters with overlapping membership functions precisely overcomes the mutual exclusivity limits of the
Boolean logic decision tree and makes methods less susceptible to the potential presence of noise. Among the number
of methods developed for S, C and X bands we can distinguish between those using reflectivity at horizontal polarisation (ZH ), differential reflectivity (ZDR ), specific differential
phase shift (Kdp ) and correlation coefficient (ρhv ) (e.g. Dolan
et al., 2013) and those using linear depolarisation ratio (LDR)
(e.g. Straka et al., 2000). Also, we can discriminate between
methods using temperature as an external parameter (e.g. Zrnic et al., 2001), rather than relative altitude with respect to
the 0 ◦ C isotherm (e.g. Lim et al., 2005), as well as between
those using two-, or more, dimensional membership functions (e.g. Marzano et al., 2007), rather than one-dimensional
ones (e.g. Liu and Chandrasekar, 2000).
As the most widespread approach in hydrometeor classification, fuzzy-logic classification methods have been subject of several validation campaigns. One of the most exAtmos. Meas. Tech., 9, 4425–4445, 2016
tensive, the Joint Polarization Experiment (Ryzhkov et al.,
2005), demonstrated improved hail detection capabilities using ground measurements with hail-intercept vehicles. A
Bayesian approach proposed by Marzano et al. (2010) is another representative supervised approach, in which each simulated class is characterized by its centre and covariance matrix. The labelling of the observations is done by means of
Bayesian infer (...truncated)