Loading…

An alternative coordinate system for solving finite difference ocean models

An alternative ‘compressed’ coordinate system for representing finite difference grids in ocean models is presented and compared with the traditional Cartesian method. The alternative method represents any arbitrary three-dimensional domain as a one-dimensional vector. Advantages of using this metho...

Full description

Saved in:
Bibliographic Details
Published in:Ocean modelling (Oxford) 2006, Vol.14 (3), p.174-196
Main Author: Herzfeld, M.
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-c337t-c60dcdef88ea5c192ae0b152603363279dbe76bdc12b3c23ff25a479aea743ee3
cites cdi_FETCH-LOGICAL-c337t-c60dcdef88ea5c192ae0b152603363279dbe76bdc12b3c23ff25a479aea743ee3
container_end_page 196
container_issue 3
container_start_page 174
container_title Ocean modelling (Oxford)
container_volume 14
creator Herzfeld, M.
description An alternative ‘compressed’ coordinate system for representing finite difference grids in ocean models is presented and compared with the traditional Cartesian method. The alternative method represents any arbitrary three-dimensional domain as a one-dimensional vector. Advantages of using this method include the exclusion of all land ‘dry’ points from the computational grid, leading to savings in the memory used and increased execution speed where domains have a low ratio of wet to total computational cells. The Cartesian and compressed models are applied to a variety of domains to assess the performance of each in terms of memory use and computational speed.
doi_str_mv 10.1016/j.ocemod.2006.04.002
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_20557059</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S1463500306000436</els_id><sourcerecordid>20557059</sourcerecordid><originalsourceid>FETCH-LOGICAL-c337t-c60dcdef88ea5c192ae0b152603363279dbe76bdc12b3c23ff25a479aea743ee3</originalsourceid><addsrcrecordid>eNp9UE1LAzEQDaJgrf4DDzl523WSbHa7F6EUv7DgRc8hm0wkZXdTk22h_96UikdPM8O8D94j5JZByYDV95syGByCLTlAXUJVAvAzMmNVLQoJjJ3_7SAuyVVKGwDWMCFn5G05Ut1PGEc9-T1SE0K0Ph9I0yFNOFAXIk2h3_vxizo_-vyx3jmMOBqk2ViPNHtjn67JhdN9wpvfOSefT48fq5di_f78ulquCyNEMxWmBmssusUCtTSs5RqhY5LXIEQteNPaDpu6s4bxThgunONSV02rUTeVQBRzcnfS3cbwvcM0qcEng32vRwy7pDhI2YBsM7A6AU0MKUV0ahv9oONBMVDH5tRGnZpTx-YUVCo3l2kPJ1rOhHuPUSXjj2mtj2gmZYP_X-AH-Tx6UQ</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>20557059</pqid></control><display><type>article</type><title>An alternative coordinate system for solving finite difference ocean models</title><source>Elsevier</source><creator>Herzfeld, M.</creator><creatorcontrib>Herzfeld, M.</creatorcontrib><description>An alternative ‘compressed’ coordinate system for representing finite difference grids in ocean models is presented and compared with the traditional Cartesian method. The alternative method represents any arbitrary three-dimensional domain as a one-dimensional vector. Advantages of using this method include the exclusion of all land ‘dry’ points from the computational grid, leading to savings in the memory used and increased execution speed where domains have a low ratio of wet to total computational cells. The Cartesian and compressed models are applied to a variety of domains to assess the performance of each in terms of memory use and computational speed.</description><identifier>ISSN: 1463-5003</identifier><identifier>EISSN: 1463-5011</identifier><identifier>DOI: 10.1016/j.ocemod.2006.04.002</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Coordinate systems ; Finite difference method ; Marine ; Modelling</subject><ispartof>Ocean modelling (Oxford), 2006, Vol.14 (3), p.174-196</ispartof><rights>2006</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c337t-c60dcdef88ea5c192ae0b152603363279dbe76bdc12b3c23ff25a479aea743ee3</citedby><cites>FETCH-LOGICAL-c337t-c60dcdef88ea5c192ae0b152603363279dbe76bdc12b3c23ff25a479aea743ee3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,4010,27900,27901,27902</link.rule.ids></links><search><creatorcontrib>Herzfeld, M.</creatorcontrib><title>An alternative coordinate system for solving finite difference ocean models</title><title>Ocean modelling (Oxford)</title><description>An alternative ‘compressed’ coordinate system for representing finite difference grids in ocean models is presented and compared with the traditional Cartesian method. The alternative method represents any arbitrary three-dimensional domain as a one-dimensional vector. Advantages of using this method include the exclusion of all land ‘dry’ points from the computational grid, leading to savings in the memory used and increased execution speed where domains have a low ratio of wet to total computational cells. The Cartesian and compressed models are applied to a variety of domains to assess the performance of each in terms of memory use and computational speed.</description><subject>Coordinate systems</subject><subject>Finite difference method</subject><subject>Marine</subject><subject>Modelling</subject><issn>1463-5003</issn><issn>1463-5011</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNp9UE1LAzEQDaJgrf4DDzl523WSbHa7F6EUv7DgRc8hm0wkZXdTk22h_96UikdPM8O8D94j5JZByYDV95syGByCLTlAXUJVAvAzMmNVLQoJjJ3_7SAuyVVKGwDWMCFn5G05Ut1PGEc9-T1SE0K0Ph9I0yFNOFAXIk2h3_vxizo_-vyx3jmMOBqk2ViPNHtjn67JhdN9wpvfOSefT48fq5di_f78ulquCyNEMxWmBmssusUCtTSs5RqhY5LXIEQteNPaDpu6s4bxThgunONSV02rUTeVQBRzcnfS3cbwvcM0qcEng32vRwy7pDhI2YBsM7A6AU0MKUV0ahv9oONBMVDH5tRGnZpTx-YUVCo3l2kPJ1rOhHuPUSXjj2mtj2gmZYP_X-AH-Tx6UQ</recordid><startdate>2006</startdate><enddate>2006</enddate><creator>Herzfeld, M.</creator><general>Elsevier Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>2006</creationdate><title>An alternative coordinate system for solving finite difference ocean models</title><author>Herzfeld, M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c337t-c60dcdef88ea5c192ae0b152603363279dbe76bdc12b3c23ff25a479aea743ee3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Coordinate systems</topic><topic>Finite difference method</topic><topic>Marine</topic><topic>Modelling</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Herzfeld, M.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><jtitle>Ocean modelling (Oxford)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Herzfeld, M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>An alternative coordinate system for solving finite difference ocean models</atitle><jtitle>Ocean modelling (Oxford)</jtitle><date>2006</date><risdate>2006</risdate><volume>14</volume><issue>3</issue><spage>174</spage><epage>196</epage><pages>174-196</pages><issn>1463-5003</issn><eissn>1463-5011</eissn><abstract>An alternative ‘compressed’ coordinate system for representing finite difference grids in ocean models is presented and compared with the traditional Cartesian method. The alternative method represents any arbitrary three-dimensional domain as a one-dimensional vector. Advantages of using this method include the exclusion of all land ‘dry’ points from the computational grid, leading to savings in the memory used and increased execution speed where domains have a low ratio of wet to total computational cells. The Cartesian and compressed models are applied to a variety of domains to assess the performance of each in terms of memory use and computational speed.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.ocemod.2006.04.002</doi><tpages>23</tpages></addata></record>
fulltext fulltext
identifier ISSN: 1463-5003
ispartof Ocean modelling (Oxford), 2006, Vol.14 (3), p.174-196
issn 1463-5003
1463-5011
language eng
recordid cdi_proquest_miscellaneous_20557059
source Elsevier
subjects Coordinate systems
Finite difference method
Marine
Modelling
title An alternative coordinate system for solving finite difference ocean models
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-06T10%3A25%3A13IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=An%20alternative%20coordinate%20system%20for%20solving%20finite%20difference%20ocean%20models&rft.jtitle=Ocean%20modelling%20(Oxford)&rft.au=Herzfeld,%20M.&rft.date=2006&rft.volume=14&rft.issue=3&rft.spage=174&rft.epage=196&rft.pages=174-196&rft.issn=1463-5003&rft.eissn=1463-5011&rft_id=info:doi/10.1016/j.ocemod.2006.04.002&rft_dat=%3Cproquest_cross%3E20557059%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c337t-c60dcdef88ea5c192ae0b152603363279dbe76bdc12b3c23ff25a479aea743ee3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=20557059&rft_id=info:pmid/&rfr_iscdi=true