Loading…

Arbitrarily high order Convected Scheme solution of the Vlasov-Poisson system

The Convected Scheme (CS) is a `forward-trajectory' semi-Lagrangian method for solution of transport equations, which has been most often applied to the kinetic description of plasmas and rarefied neutral gases. In its simplest form, the CS propagates the solution by advecting the `moving cells...

Full description

Saved in:
Bibliographic Details
Published in:arXiv.org 2014-03
Main Authors: Güçlü, Yaman, Christlieb, Andrew J, Hitchon, William N G
Format: Article
Language:English
Subjects:
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by
cites
container_end_page
container_issue
container_start_page
container_title arXiv.org
container_volume
creator Güçlü, Yaman
Christlieb, Andrew J
Hitchon, William N G
description The Convected Scheme (CS) is a `forward-trajectory' semi-Lagrangian method for solution of transport equations, which has been most often applied to the kinetic description of plasmas and rarefied neutral gases. In its simplest form, the CS propagates the solution by advecting the `moving cells' along their characteristic trajectories, and by remapping them on the mesh at the end of the time step. The CS is conservative, positivity preserving, simple to implement, and not subject to time step restriction to maintain stability. Recently [Y. G\"uçl\"u and W.N.G. Hitchon, 2012] a new methodology was introduced for reducing numerical diffusion, based on a modified equation analysis: the remapping error was compensated by applying small corrections to the final position of the moving cells prior to remapping. While the spatial accuracy was increased from 2nd to 4th order, the new scheme retained the important properties of the original method, and was shown to be simple and efficient for constant advection problems. Here the CS is applied to the solution of the Vlasov-Poisson system: the Vlasov equation is split into two constant advection equations, one in configuration space and one in velocity space, and high order time accuracy is achieved by proper composition of the operators. The splitting procedure enables us to use the constant advection solver, which we extend to arbitrarily high order of accuracy: a new improved procedure is given, which makes the calculation of the corrections straightforward. Focusing on periodic domains, we describe a spectrally accurate scheme based on the fast Fourier transform; the proposed implementation is strictly conservative and positivity preserving. The ability to correctly reproduce the system dynamics, as well as resolving small-scale features in the solution, is shown in classical 1D-1V test cases, both in the linear and the non-linear regimes.
doi_str_mv 10.48550/arxiv.1311.5310
format article
fullrecord <record><control><sourceid>proquest</sourceid><recordid>TN_cdi_proquest_journals_2082931261</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2082931261</sourcerecordid><originalsourceid>FETCH-LOGICAL-a511-10f67da5ed3f61eb7dcbdb8c76fff570942990eaf00dae1e5355cd6577e8f7fd3</originalsourceid><addsrcrecordid>eNotjc9LwzAYQIMgOObuHgOeW_MlTdIeR_EXTBQcXkfafLEZXaNJOtx_70BPD97hPUJugJVVLSW7M_HHH0sQAKUUwC7IggsBRV1xfkVWKe0ZY1xpLqVYkJd17HyOJvrxRAf_OdAQLUbahumIfUZL3_sBD0hTGOfsw0SDo3lA-jGaFI7FW_ApnW06pYyHa3LpzJhw9c8l2T7cb9unYvP6-NyuN4WRAAUwp7Q1Eq1wCrDTtu9sV_daOeekZk3Fm4ahcYxZg4BSSNlbJbXG2mlnxZLc_mW_YvieMeXdPsxxOh93nNW8EcAViF9HE1Ct</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2082931261</pqid></control><display><type>article</type><title>Arbitrarily high order Convected Scheme solution of the Vlasov-Poisson system</title><source>Publicly Available Content (ProQuest)</source><creator>Güçlü, Yaman ; Christlieb, Andrew J ; Hitchon, William N G</creator><creatorcontrib>Güçlü, Yaman ; Christlieb, Andrew J ; Hitchon, William N G</creatorcontrib><description>The Convected Scheme (CS) is a `forward-trajectory' semi-Lagrangian method for solution of transport equations, which has been most often applied to the kinetic description of plasmas and rarefied neutral gases. In its simplest form, the CS propagates the solution by advecting the `moving cells' along their characteristic trajectories, and by remapping them on the mesh at the end of the time step. The CS is conservative, positivity preserving, simple to implement, and not subject to time step restriction to maintain stability. Recently [Y. G\"uçl\"u and W.N.G. Hitchon, 2012] a new methodology was introduced for reducing numerical diffusion, based on a modified equation analysis: the remapping error was compensated by applying small corrections to the final position of the moving cells prior to remapping. While the spatial accuracy was increased from 2nd to 4th order, the new scheme retained the important properties of the original method, and was shown to be simple and efficient for constant advection problems. Here the CS is applied to the solution of the Vlasov-Poisson system: the Vlasov equation is split into two constant advection equations, one in configuration space and one in velocity space, and high order time accuracy is achieved by proper composition of the operators. The splitting procedure enables us to use the constant advection solver, which we extend to arbitrarily high order of accuracy: a new improved procedure is given, which makes the calculation of the corrections straightforward. Focusing on periodic domains, we describe a spectrally accurate scheme based on the fast Fourier transform; the proposed implementation is strictly conservative and positivity preserving. The ability to correctly reproduce the system dynamics, as well as resolving small-scale features in the solution, is shown in classical 1D-1V test cases, both in the linear and the non-linear regimes.</description><identifier>EISSN: 2331-8422</identifier><identifier>DOI: 10.48550/arxiv.1311.5310</identifier><language>eng</language><publisher>Ithaca: Cornell University Library, arXiv.org</publisher><subject>Accuracy ; Advection ; Domains ; Error analysis ; Error compensation ; Error correction ; Fast Fourier transformations ; Fourier transforms ; Mathematical analysis ; Neutral gases ; Plasmas ; System dynamics ; Trajectories ; Vlasov equations</subject><ispartof>arXiv.org, 2014-03</ispartof><rights>2014. This work is published under http://arxiv.org/licenses/nonexclusive-distrib/1.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.proquest.com/docview/2082931261?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>780,784,25753,27925,37012,44590</link.rule.ids></links><search><creatorcontrib>Güçlü, Yaman</creatorcontrib><creatorcontrib>Christlieb, Andrew J</creatorcontrib><creatorcontrib>Hitchon, William N G</creatorcontrib><title>Arbitrarily high order Convected Scheme solution of the Vlasov-Poisson system</title><title>arXiv.org</title><description>The Convected Scheme (CS) is a `forward-trajectory' semi-Lagrangian method for solution of transport equations, which has been most often applied to the kinetic description of plasmas and rarefied neutral gases. In its simplest form, the CS propagates the solution by advecting the `moving cells' along their characteristic trajectories, and by remapping them on the mesh at the end of the time step. The CS is conservative, positivity preserving, simple to implement, and not subject to time step restriction to maintain stability. Recently [Y. G\"uçl\"u and W.N.G. Hitchon, 2012] a new methodology was introduced for reducing numerical diffusion, based on a modified equation analysis: the remapping error was compensated by applying small corrections to the final position of the moving cells prior to remapping. While the spatial accuracy was increased from 2nd to 4th order, the new scheme retained the important properties of the original method, and was shown to be simple and efficient for constant advection problems. Here the CS is applied to the solution of the Vlasov-Poisson system: the Vlasov equation is split into two constant advection equations, one in configuration space and one in velocity space, and high order time accuracy is achieved by proper composition of the operators. The splitting procedure enables us to use the constant advection solver, which we extend to arbitrarily high order of accuracy: a new improved procedure is given, which makes the calculation of the corrections straightforward. Focusing on periodic domains, we describe a spectrally accurate scheme based on the fast Fourier transform; the proposed implementation is strictly conservative and positivity preserving. The ability to correctly reproduce the system dynamics, as well as resolving small-scale features in the solution, is shown in classical 1D-1V test cases, both in the linear and the non-linear regimes.</description><subject>Accuracy</subject><subject>Advection</subject><subject>Domains</subject><subject>Error analysis</subject><subject>Error compensation</subject><subject>Error correction</subject><subject>Fast Fourier transformations</subject><subject>Fourier transforms</subject><subject>Mathematical analysis</subject><subject>Neutral gases</subject><subject>Plasmas</subject><subject>System dynamics</subject><subject>Trajectories</subject><subject>Vlasov equations</subject><issn>2331-8422</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><recordid>eNotjc9LwzAYQIMgOObuHgOeW_MlTdIeR_EXTBQcXkfafLEZXaNJOtx_70BPD97hPUJugJVVLSW7M_HHH0sQAKUUwC7IggsBRV1xfkVWKe0ZY1xpLqVYkJd17HyOJvrxRAf_OdAQLUbahumIfUZL3_sBD0hTGOfsw0SDo3lA-jGaFI7FW_ApnW06pYyHa3LpzJhw9c8l2T7cb9unYvP6-NyuN4WRAAUwp7Q1Eq1wCrDTtu9sV_daOeekZk3Fm4ahcYxZg4BSSNlbJbXG2mlnxZLc_mW_YvieMeXdPsxxOh93nNW8EcAViF9HE1Ct</recordid><startdate>20140331</startdate><enddate>20140331</enddate><creator>Güçlü, Yaman</creator><creator>Christlieb, Andrew J</creator><creator>Hitchon, William N G</creator><general>Cornell University Library, arXiv.org</general><scope>8FE</scope><scope>8FG</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>HCIFZ</scope><scope>L6V</scope><scope>M7S</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope></search><sort><creationdate>20140331</creationdate><title>Arbitrarily high order Convected Scheme solution of the Vlasov-Poisson system</title><author>Güçlü, Yaman ; Christlieb, Andrew J ; Hitchon, William N G</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a511-10f67da5ed3f61eb7dcbdb8c76fff570942990eaf00dae1e5355cd6577e8f7fd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Accuracy</topic><topic>Advection</topic><topic>Domains</topic><topic>Error analysis</topic><topic>Error compensation</topic><topic>Error correction</topic><topic>Fast Fourier transformations</topic><topic>Fourier transforms</topic><topic>Mathematical analysis</topic><topic>Neutral gases</topic><topic>Plasmas</topic><topic>System dynamics</topic><topic>Trajectories</topic><topic>Vlasov equations</topic><toplevel>online_resources</toplevel><creatorcontrib>Güçlü, Yaman</creatorcontrib><creatorcontrib>Christlieb, Andrew J</creatorcontrib><creatorcontrib>Hitchon, William N G</creatorcontrib><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>Materials Science &amp; Engineering Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central</collection><collection>ProQuest Central Essentials</collection><collection>AUTh Library subscriptions: ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Engineering Collection</collection><collection>Engineering Database</collection><collection>Publicly Available Content (ProQuest)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Engineering collection</collection><jtitle>arXiv.org</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Güçlü, Yaman</au><au>Christlieb, Andrew J</au><au>Hitchon, William N G</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Arbitrarily high order Convected Scheme solution of the Vlasov-Poisson system</atitle><jtitle>arXiv.org</jtitle><date>2014-03-31</date><risdate>2014</risdate><eissn>2331-8422</eissn><abstract>The Convected Scheme (CS) is a `forward-trajectory' semi-Lagrangian method for solution of transport equations, which has been most often applied to the kinetic description of plasmas and rarefied neutral gases. In its simplest form, the CS propagates the solution by advecting the `moving cells' along their characteristic trajectories, and by remapping them on the mesh at the end of the time step. The CS is conservative, positivity preserving, simple to implement, and not subject to time step restriction to maintain stability. Recently [Y. G\"uçl\"u and W.N.G. Hitchon, 2012] a new methodology was introduced for reducing numerical diffusion, based on a modified equation analysis: the remapping error was compensated by applying small corrections to the final position of the moving cells prior to remapping. While the spatial accuracy was increased from 2nd to 4th order, the new scheme retained the important properties of the original method, and was shown to be simple and efficient for constant advection problems. Here the CS is applied to the solution of the Vlasov-Poisson system: the Vlasov equation is split into two constant advection equations, one in configuration space and one in velocity space, and high order time accuracy is achieved by proper composition of the operators. The splitting procedure enables us to use the constant advection solver, which we extend to arbitrarily high order of accuracy: a new improved procedure is given, which makes the calculation of the corrections straightforward. Focusing on periodic domains, we describe a spectrally accurate scheme based on the fast Fourier transform; the proposed implementation is strictly conservative and positivity preserving. The ability to correctly reproduce the system dynamics, as well as resolving small-scale features in the solution, is shown in classical 1D-1V test cases, both in the linear and the non-linear regimes.</abstract><cop>Ithaca</cop><pub>Cornell University Library, arXiv.org</pub><doi>10.48550/arxiv.1311.5310</doi><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier EISSN: 2331-8422
ispartof arXiv.org, 2014-03
issn 2331-8422
language eng
recordid cdi_proquest_journals_2082931261
source Publicly Available Content (ProQuest)
subjects Accuracy
Advection
Domains
Error analysis
Error compensation
Error correction
Fast Fourier transformations
Fourier transforms
Mathematical analysis
Neutral gases
Plasmas
System dynamics
Trajectories
Vlasov equations
title Arbitrarily high order Convected Scheme solution of the Vlasov-Poisson system
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-28T23%3A29%3A27IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Arbitrarily%20high%20order%20Convected%20Scheme%20solution%20of%20the%20Vlasov-Poisson%20system&rft.jtitle=arXiv.org&rft.au=G%C3%BC%C3%A7l%C3%BC,%20Yaman&rft.date=2014-03-31&rft.eissn=2331-8422&rft_id=info:doi/10.48550/arxiv.1311.5310&rft_dat=%3Cproquest%3E2082931261%3C/proquest%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a511-10f67da5ed3f61eb7dcbdb8c76fff570942990eaf00dae1e5355cd6577e8f7fd3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=2082931261&rft_id=info:pmid/&rfr_iscdi=true