[760] - PARSIVEL Snow Observations: A Critical Assessment

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Citation
Battaglia, A., Rustemeier, E., Tokay, A., Blahak, U., Simmer, C., 2010. PARSIVEL Snow Observations: A Critical Assessment. Journal of Atmosperic and Oceanographic Technology, 27 (2), 333 - 344. DOI: 10.1175/2009JTECHA1332.1.
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Identification
Title(s):Main Title: PARSIVEL Snow Observations: A Critical Assessment
Description(s):Abstract: The performance of the laser-optical Particle Size Velocity (PARSIVEL) disdrometer is evaluated to determine the characteristics of falling snow. PARSIVEL’s measuring principle is reexamined to detect its limitations and pitfalls when applied to solid precipitation. This study uses snow observations taken during the Canadian Cloudsat/Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Validation Project (C3VP) campaign, when two PARSIVEL instruments were collocated with a single twodimensional disdrometer (2-DVD), which allows more detailed observation of snowflakes. When characterizing the snowflake size, PARSIVEL instruments inherently retrieve only one size parameter, which is approximately equal to the widest horizontal dimension (more accurately with large snowflakes) and that has no microphysical meaning. Unlike for raindrops, the equivolume PARSIVEL diameter—the PARSIVEL output variable—has no physical counterpart for snowflakes. PARSIVEL’s fall velocity measurement may not be accurate for a single snowflake particle. This is due to the internally assumed relationship between horizontal and vertical snow particle dimensions. The uncertainty originates from the shape-related factor, which tends to depart more and more from unity with increasing snowflake sizes and can produce large errors. When averaging over a large number of snowflakes, the correction factor is size dependent with a systematic tendency to an underestimation of the fall speed (but never exceeding 20%). Compared to a collocated 2-DVD for long-lasting events, PARSIVEL seems to overestimate the number of small snowflakes and large particles. The disagreement between PARSIVEL and 2-DVD snow measurements can only be partly ascribed to PARSIVEL intrinsic limitations (border effects and sizing problems), but it has to deal with the difficulties and drawbacks of both instruments in fully characterizing snow properties.
Identifier(s):DOI: 10.1175/2009JTECHA1332.1
Responsible Party
Creator(s):Author: Alessandro Battaglia
Author: Elke Rustemeier
Author: Ali Tokay
Author: Ulrich Blahak
Author: Clemens Simmer
Publisher:American Meteorological Society
Topic
TR32 Topic:Other
Subject(s):CRC/TR32 Keywords: Sensor, Disdrometer, Meteorology
File Details
File Name:2010_Battaglia_JoAOT.pdf
Data Type:Text
Size(s):12 Pages
File Size:1935 kB (1.89 MB)
Date(s):Date Submitted: 2009-09-10
Mime Type:application/pdf
Data Format:PDF
Language:English
Status:Completed
Constraints
Download Permission:OnlyTR32
General Access and Use Conditions:For internal use only
Access Limitations:For internal use only
Licence:TR32DB Data policy agreement
Geographic
North:-no map data
East:-
South:-
West:-
Measurement Region:Other
Measurement Location:--Other--
Specific Informations - Publication
Status:Published
Review:PeerReview
Year:2010
Type:Article
Article Type:Journal
Source:Journal of Atmosperic and Oceanographic Technology
Issue:2
Volume:27
Number Of Pages:12
Page Range:333 - 344
Metadata Details
Metadata Creator:Alessandro Battaglia
Metadata Created:2013-12-03
Metadata Last Updated:2013-12-03
Subproject:D5
Funding Phase:1
Metadata Language:English
Metadata Version:V40
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