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Quasi-Vertical Profiles—A New Way to Look at Polarimetric Radar Data
A novel methodology is introduced for processing and presenting polarimetric data collected by weather surveillance radars. It involves azimuthal averaging of radar reflectivity Z, differential reflectivity Z sub(DR), cross-correlation coefficient rho sub(hv), and differential phase Phi sub(DP) at h...
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Published in: | Journal of atmospheric and oceanic technology 2016-03, Vol.33 (3), p.551-562 |
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container_title | Journal of atmospheric and oceanic technology |
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creator | Ryzhkov, Alexander Zhang, Pengfei Reeves, Heather Kumjian, Matthew Tschallener, Timo Trömel, Silke Simmer, Clemens |
description | A novel methodology is introduced for processing and presenting polarimetric data collected by weather surveillance radars. It involves azimuthal averaging of radar reflectivity Z, differential reflectivity Z sub(DR), cross-correlation coefficient rho sub(hv), and differential phase Phi sub(DP) at high antenna elevation, and presenting resulting quasi-vertical profiles (QVPs) in a height-versus-time format. Multiple examples of QVPs retrieved from the data collected by S-, C-, and X-band dual-polarization radars at elevations ranging from 6.4 degree to 28 degree illustrate advantages of the QVP technique. The benefits include an ability to examine the temporal evolution of microphysical processes governing precipitation production and to compare polarimetric data obtained from the scanning surveillance weather radars with observations made by vertically looking remote sensors, such as wind profilers, lidars, radiometers, cloud radars, and radars operating on spaceborne and airborne platforms. Continuous monitoring of the melting layer and the layer of dendritic growth with high vertical resolution, and the possible opportunity to discriminate between the processes of snow aggregation and riming, constitute other potential benefits of the suggested methodology. |
doi_str_mv | 10.1175/JTECH-D-15-0020.1 |
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It involves azimuthal averaging of radar reflectivity Z, differential reflectivity Z sub(DR), cross-correlation coefficient rho sub(hv), and differential phase Phi sub(DP) at high antenna elevation, and presenting resulting quasi-vertical profiles (QVPs) in a height-versus-time format. Multiple examples of QVPs retrieved from the data collected by S-, C-, and X-band dual-polarization radars at elevations ranging from 6.4 degree to 28 degree illustrate advantages of the QVP technique. The benefits include an ability to examine the temporal evolution of microphysical processes governing precipitation production and to compare polarimetric data obtained from the scanning surveillance weather radars with observations made by vertically looking remote sensors, such as wind profilers, lidars, radiometers, cloud radars, and radars operating on spaceborne and airborne platforms. Continuous monitoring of the melting layer and the layer of dendritic growth with high vertical resolution, and the possible opportunity to discriminate between the processes of snow aggregation and riming, constitute other potential benefits of the suggested methodology.</description><identifier>ISSN: 0739-0572</identifier><identifier>EISSN: 1520-0426</identifier><identifier>DOI: 10.1175/JTECH-D-15-0020.1</identifier><language>eng</language><publisher>Boston: American Meteorological Society</publisher><subject>Aggregation ; Antennas ; Clouds ; Correlation coefficient ; Correlation coefficients ; Cross correlation ; Dual polarization radar ; Elevation ; Estimates ; Marine ; Methodology ; Methods ; Microwave imagery ; Polarimetric radar ; Polarimetry ; Precipitation ; Profilers ; Radar ; Radar data ; Radar polarimetry ; Radar reflectivity ; Radiometers ; Reflectance ; Remote sensors ; Snow ; Standard deviation ; Superhigh frequencies ; Surveillance ; Variables ; Vertical profiles ; Weather ; Work platforms ; X-band</subject><ispartof>Journal of atmospheric and oceanic technology, 2016-03, Vol.33 (3), p.551-562</ispartof><rights>Copyright American Meteorological Society Mar 2016</rights><rights>Copyright American Meteorological Society 2016</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c476t-149c2c42e2b140558011131f12b6d5c1a000035c03f05b91f65768910572feb13</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,786,790,27957,27958</link.rule.ids></links><search><creatorcontrib>Ryzhkov, Alexander</creatorcontrib><creatorcontrib>Zhang, Pengfei</creatorcontrib><creatorcontrib>Reeves, Heather</creatorcontrib><creatorcontrib>Kumjian, Matthew</creatorcontrib><creatorcontrib>Tschallener, Timo</creatorcontrib><creatorcontrib>Trömel, Silke</creatorcontrib><creatorcontrib>Simmer, Clemens</creatorcontrib><title>Quasi-Vertical Profiles—A New Way to Look at Polarimetric Radar Data</title><title>Journal of atmospheric and oceanic technology</title><description>A novel methodology is introduced for processing and presenting polarimetric data collected by weather surveillance radars. It involves azimuthal averaging of radar reflectivity Z, differential reflectivity Z sub(DR), cross-correlation coefficient rho sub(hv), and differential phase Phi sub(DP) at high antenna elevation, and presenting resulting quasi-vertical profiles (QVPs) in a height-versus-time format. Multiple examples of QVPs retrieved from the data collected by S-, C-, and X-band dual-polarization radars at elevations ranging from 6.4 degree to 28 degree illustrate advantages of the QVP technique. The benefits include an ability to examine the temporal evolution of microphysical processes governing precipitation production and to compare polarimetric data obtained from the scanning surveillance weather radars with observations made by vertically looking remote sensors, such as wind profilers, lidars, radiometers, cloud radars, and radars operating on spaceborne and airborne platforms. 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reflectivity</subject><subject>Radiometers</subject><subject>Reflectance</subject><subject>Remote sensors</subject><subject>Snow</subject><subject>Standard deviation</subject><subject>Superhigh frequencies</subject><subject>Surveillance</subject><subject>Variables</subject><subject>Vertical profiles</subject><subject>Weather</subject><subject>Work 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Matthew</au><au>Tschallener, Timo</au><au>Trömel, Silke</au><au>Simmer, Clemens</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Quasi-Vertical Profiles—A New Way to Look at Polarimetric Radar Data</atitle><jtitle>Journal of atmospheric and oceanic technology</jtitle><date>2016-03-01</date><risdate>2016</risdate><volume>33</volume><issue>3</issue><spage>551</spage><epage>562</epage><pages>551-562</pages><issn>0739-0572</issn><eissn>1520-0426</eissn><notes>ObjectType-Article-1</notes><notes>SourceType-Scholarly Journals-1</notes><notes>ObjectType-Feature-2</notes><notes>content type line 23</notes><abstract>A novel methodology is introduced for processing and presenting polarimetric data collected by weather surveillance radars. It involves azimuthal averaging of radar reflectivity Z, differential reflectivity Z sub(DR), cross-correlation coefficient rho sub(hv), and differential phase Phi sub(DP) at high antenna elevation, and presenting resulting quasi-vertical profiles (QVPs) in a height-versus-time format. Multiple examples of QVPs retrieved from the data collected by S-, C-, and X-band dual-polarization radars at elevations ranging from 6.4 degree to 28 degree illustrate advantages of the QVP technique. The benefits include an ability to examine the temporal evolution of microphysical processes governing precipitation production and to compare polarimetric data obtained from the scanning surveillance weather radars with observations made by vertically looking remote sensors, such as wind profilers, lidars, radiometers, cloud radars, and radars operating on spaceborne and airborne platforms. Continuous monitoring of the melting layer and the layer of dendritic growth with high vertical resolution, and the possible opportunity to discriminate between the processes of snow aggregation and riming, constitute other potential benefits of the suggested methodology.</abstract><cop>Boston</cop><pub>American Meteorological Society</pub><doi>10.1175/JTECH-D-15-0020.1</doi><tpages>12</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Aggregation Antennas Clouds Correlation coefficient Correlation coefficients Cross correlation Dual polarization radar Elevation Estimates Marine Methodology Methods Microwave imagery Polarimetric radar Polarimetry Precipitation Profilers Radar Radar data Radar polarimetry Radar reflectivity Radiometers Reflectance Remote sensors Snow Standard deviation Superhigh frequencies Surveillance Variables Vertical profiles Weather Work platforms X-band |
title | Quasi-Vertical Profiles—A New Way to Look at Polarimetric Radar Data |
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