Journal article 416 views
Bright‐band detection from radar vertical reflectivity profiles
M. A Rico‐Ramirez,
I. D Cluckie,
Ian Cluckie
International Journal of Remote Sensing, Volume: 28, Issue: 18, Pages: 4013 - 4025
Swansea University Author: Ian Cluckie
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DOI (Published version): 10.1080/01431160601047797
Abstract
The use of quantitative scanning weather radar for precipitation measurements is a vital element of modern hydrology and limits the development of all distributed models of catchment behaviour. The presence of the so‐called bright band (or melting layer) contaminates the quantitative precipitation e...
| Published in: | International Journal of Remote Sensing |
|---|---|
| ISSN: | 0143-1161 1366-5901 |
| Published: |
2007
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| URI: | https://cronfa.swan.ac.uk/Record/cronfa10536 |
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<?xml version="1.0"?><rfc1807><datestamp>2013-11-21T14:20:22.4342726</datestamp><bib-version>v2</bib-version><id>10536</id><entry>2012-04-06</entry><title>Bright‐band detection from radar vertical reflectivity profiles</title><swanseaauthors><author><sid>d801af52a3cfb625308bd4301583064e</sid><firstname>Ian</firstname><surname>Cluckie</surname><name>Ian Cluckie</name><active>true</active><ethesisStudent>false</ethesisStudent></author></swanseaauthors><date>2012-04-06</date><deptcode>FGSEN</deptcode><abstract>The use of quantitative scanning weather radar for precipitation measurements is a vital element of modern hydrology and limits the development of all distributed models of catchment behaviour. The presence of the so‐called bright band (or melting layer) contaminates the quantitative precipitation estimates and has delayed the widespread take‐up of radar‐based precipitation estimates in operational models. The study of the Vertical Reflectivity Profile (VRP) of precipitation is important in order to develop algorithms to correct scanning weather radar measurements for the variation of the VRP at long ranges. Therefore, this paper presents an algorithm to detect the extent of the bright band using high‐resolution VRP's. The boundaries of the bright band are identified by a new algorithm which utilizes a rotational coordinate system for identifying the upper and lower parts of the bright band. This overcomes some of the difficulties experienced when using the gradient of the reflectivity in conventional bright‐band detection algorithms. The reflectivities above, within, and below the bright band are then used to construct idealized VRP's to correct scanning weather radar measurements.</abstract><type>Journal Article</type><journal>International Journal of Remote Sensing</journal><volume>28</volume><journalNumber>18</journalNumber><paginationStart>4013</paginationStart><paginationEnd>4025</paginationEnd><publisher/><issnPrint>0143-1161</issnPrint><issnElectronic>1366-5901</issnElectronic><keywords/><publishedDay>31</publishedDay><publishedMonth>8</publishedMonth><publishedYear>2007</publishedYear><publishedDate>2007-08-31</publishedDate><doi>10.1080/01431160601047797</doi><url/><notes/><college>COLLEGE NANME</college><department>Science and Engineering - Faculty</department><CollegeCode>COLLEGE CODE</CollegeCode><DepartmentCode>FGSEN</DepartmentCode><institution>Swansea University</institution><apcterm/><lastEdited>2013-11-21T14:20:22.4342726</lastEdited><Created>2012-04-06T18:08:34.9293690</Created><path><level id="1">Faculty of Science and Engineering</level><level id="2">School of Engineering and Applied Sciences - Uncategorised</level></path><authors><author><firstname>M. A</firstname><surname>Rico‐Ramirez</surname><order>1</order></author><author><firstname>I. D</firstname><surname>Cluckie</surname><order>2</order></author><author><firstname>Ian</firstname><surname>Cluckie</surname><order>3</order></author></authors><documents/><OutputDurs/></rfc1807> |
| spelling |
2013-11-21T14:20:22.4342726 v2 10536 2012-04-06 Bright‐band detection from radar vertical reflectivity profiles d801af52a3cfb625308bd4301583064e Ian Cluckie Ian Cluckie true false 2012-04-06 FGSEN The use of quantitative scanning weather radar for precipitation measurements is a vital element of modern hydrology and limits the development of all distributed models of catchment behaviour. The presence of the so‐called bright band (or melting layer) contaminates the quantitative precipitation estimates and has delayed the widespread take‐up of radar‐based precipitation estimates in operational models. The study of the Vertical Reflectivity Profile (VRP) of precipitation is important in order to develop algorithms to correct scanning weather radar measurements for the variation of the VRP at long ranges. Therefore, this paper presents an algorithm to detect the extent of the bright band using high‐resolution VRP's. The boundaries of the bright band are identified by a new algorithm which utilizes a rotational coordinate system for identifying the upper and lower parts of the bright band. This overcomes some of the difficulties experienced when using the gradient of the reflectivity in conventional bright‐band detection algorithms. The reflectivities above, within, and below the bright band are then used to construct idealized VRP's to correct scanning weather radar measurements. Journal Article International Journal of Remote Sensing 28 18 4013 4025 0143-1161 1366-5901 31 8 2007 2007-08-31 10.1080/01431160601047797 COLLEGE NANME Science and Engineering - Faculty COLLEGE CODE FGSEN Swansea University 2013-11-21T14:20:22.4342726 2012-04-06T18:08:34.9293690 Faculty of Science and Engineering School of Engineering and Applied Sciences - Uncategorised M. A Rico‐Ramirez 1 I. D Cluckie 2 Ian Cluckie 3 |
| title |
Bright‐band detection from radar vertical reflectivity profiles |
| spellingShingle |
Bright‐band detection from radar vertical reflectivity profiles Ian Cluckie |
| title_short |
Bright‐band detection from radar vertical reflectivity profiles |
| title_full |
Bright‐band detection from radar vertical reflectivity profiles |
| title_fullStr |
Bright‐band detection from radar vertical reflectivity profiles |
| title_full_unstemmed |
Bright‐band detection from radar vertical reflectivity profiles |
| title_sort |
Bright‐band detection from radar vertical reflectivity profiles |
| author_id_str_mv |
d801af52a3cfb625308bd4301583064e |
| author_id_fullname_str_mv |
d801af52a3cfb625308bd4301583064e_***_Ian Cluckie |
| author |
Ian Cluckie |
| author2 |
M. A Rico‐Ramirez I. D Cluckie Ian Cluckie |
| format |
Journal article |
| container_title |
International Journal of Remote Sensing |
| container_volume |
28 |
| container_issue |
18 |
| container_start_page |
4013 |
| publishDate |
2007 |
| institution |
Swansea University |
| issn |
0143-1161 1366-5901 |
| doi_str_mv |
10.1080/01431160601047797 |
| college_str |
Faculty of Science and Engineering |
| hierarchytype |
|
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facultyofscienceandengineering |
| hierarchy_top_title |
Faculty of Science and Engineering |
| hierarchy_parent_id |
facultyofscienceandengineering |
| hierarchy_parent_title |
Faculty of Science and Engineering |
| department_str |
School of Engineering and Applied Sciences - Uncategorised{{{_:::_}}}Faculty of Science and Engineering{{{_:::_}}}School of Engineering and Applied Sciences - Uncategorised |
| document_store_str |
0 |
| active_str |
0 |
| description |
The use of quantitative scanning weather radar for precipitation measurements is a vital element of modern hydrology and limits the development of all distributed models of catchment behaviour. The presence of the so‐called bright band (or melting layer) contaminates the quantitative precipitation estimates and has delayed the widespread take‐up of radar‐based precipitation estimates in operational models. The study of the Vertical Reflectivity Profile (VRP) of precipitation is important in order to develop algorithms to correct scanning weather radar measurements for the variation of the VRP at long ranges. Therefore, this paper presents an algorithm to detect the extent of the bright band using high‐resolution VRP's. The boundaries of the bright band are identified by a new algorithm which utilizes a rotational coordinate system for identifying the upper and lower parts of the bright band. This overcomes some of the difficulties experienced when using the gradient of the reflectivity in conventional bright‐band detection algorithms. The reflectivities above, within, and below the bright band are then used to construct idealized VRP's to correct scanning weather radar measurements. |
| published_date |
2007-08-31T03:11:56Z |
| _version_ |
1763750042756186112 |
| score |
11.037581 |