DocumentCode
3347912
Title
Notice of Retraction
Generation of the radar bright band and its stimulation analysis: Effection of the complex refractive index and raindrops final velocity
Author
Wang Zhenhui ; Dong Huijie ; Ji Lei ; Guo Lijun ; Zhang Peichang
Author_Institution
Key Lab. of Meteorol. Disaster of Minist. of Educ., Nanjing Univ. of Inf. Sci. & Technol., Nanjing, China
Volume
4
fYear
2011
fDate
26-28 July 2011
Firstpage
2091
Lastpage
2095
Abstract
Notice of Retraction
After careful and considered review of the content of this paper by a duly constituted expert committee, this paper has been found to be in violation of IEEE´s Publication Principles.
We hereby retract the content of this paper. Reasonable effort should be made to remove all past references to this paper.
The presenting author of this paper has the option to appeal this decision by contacting TPII@ieee.org.
With use of SimRAD2.0, this paper carried out simulation of the raindrops final velocity and the complex refractive index, which are the two factors affecting the bright band. The result shows that drastic changes of complex refractive index due to falling and melting snow and ice particles, contributes to radar echo bloom below zero-centigrade isothermal and growing falling speed of raindrops leads to radar reflectivity factor recession there, which results in a considerable bend of vertical radar reflectivity factor at the melting layer.
After careful and considered review of the content of this paper by a duly constituted expert committee, this paper has been found to be in violation of IEEE´s Publication Principles.
We hereby retract the content of this paper. Reasonable effort should be made to remove all past references to this paper.
The presenting author of this paper has the option to appeal this decision by contacting TPII@ieee.org.
With use of SimRAD2.0, this paper carried out simulation of the raindrops final velocity and the complex refractive index, which are the two factors affecting the bright band. The result shows that drastic changes of complex refractive index due to falling and melting snow and ice particles, contributes to radar echo bloom below zero-centigrade isothermal and growing falling speed of raindrops leads to radar reflectivity factor recession there, which results in a considerable bend of vertical radar reflectivity factor at the melting layer.
Keywords
rain; remote sensing by radar; snow; SimRAD simulator; complex refractive index; falling snow; ice particles; melting snow; radar bright band; radar echo bloom; radar reflectivity factor; raindrops final velocity; stimulation analysis; zero-centigrade isothermal raindrops; Atmospheric modeling; Clouds; Hydrometers; Ice; Radar; Radar scattering; Reflectivity; Melting layer; Particles with outside water films; Radar bright band; Radar reflectivity factor;
fLanguage
English
Publisher
ieee
Conference_Titel
Natural Computation (ICNC), 2011 Seventh International Conference on
Conference_Location
Shanghai
ISSN
2157-9555
Print_ISBN
978-1-4244-9950-2
Type
conf
DOI
10.1109/ICNC.2011.6022393
Filename
6022393
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