Articles | Volume 11, issue 9
Atmos. Meas. Tech., 11, 5181–5198, 2018
Atmos. Meas. Tech., 11, 5181–5198, 2018
Research article
12 Sep 2018
Research article | 12 Sep 2018

Characterisation of the melting layer variability in an Alpine valley based on polarimetric X-band radar scans

Floor van den Heuvel et al.

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Cited articles

Andrieu, H. and Creutin, J. D.: Identification of Vertical Profiles of Radar Reflectivity for Hydrological Applications Using an Inverse Method, Part I: Formulation, J. Appl. Meteorol., 34, 225–239,<0225:IOVPOR>2.0.CO;2, 1995. a, b
Andrieu, H., Delrieu, G., and Creutin, J. D.: Identification of Vertical Profiles of Radar Reflectivity For Hydrological Applications Using on Inverse Method. Part 2: Sensitivity Analysis And Case-Study, J. Appl. Meteorol., 34, 240–259, 1995. a
Battan, L. J.: Radar observation of the atmosphere, University of Chicago Press, Chicago, USA,, 1973. a
Bell, C.: Detection of the Riming Process with a Vertically Pointing Radar, PhD thesis, McGill University, Montreal, Quebec, Canada, 2000. a
Bellon, A., Lee, G., and Zawadzki, I.: Error statistics of VPR corrections in stratiform precipitation, J. Appl. Meteorol., 44, 998–1015,, 2005. a
Short summary
The paper aims at characterising and quantifying the spatio-temporal variability of the melting layer (ML; transition zone from solid to liquid precipitation). A method based on the Fourier transform is found to accurately describe different ML signatures. Hence, it is applied to characterise the ML variability in a relatively flat area and in an inner Alpine valley in Switzerland, where the variability at smaller spatial scales is found to be relatively more important.