Relationship between Ulysses plasma observations and solar observations during the Whole Sun Month campaign

In this report, we summarize measurements made by the plasma experiment on the Ulysses spacecraft during the period designated as “Whole Sun Month” (WSM, August 10 to September 8, 1996). This interval coincided with the return of solar wind variability at Ulysses. Ulysses was located at ∼ 28°N helio...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of Geophysical Research 1999-05, Vol.104 (A5), p.9871-9879
Hauptverfasser: Riley, Pete, Gosling, J. T., McComas, D. J., Pizzo, V. J., Luhmann, J. G., Biesecker, D., Forsyth, R. J., Hoeksema, J. T., Lecinski, A., Thompson, B. J.
Format: Artikel
Sprache:eng
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 9879
container_issue A5
container_start_page 9871
container_title Journal of Geophysical Research
container_volume 104
creator Riley, Pete
Gosling, J. T.
McComas, D. J.
Pizzo, V. J.
Luhmann, J. G.
Biesecker, D.
Forsyth, R. J.
Hoeksema, J. T.
Lecinski, A.
Thompson, B. J.
description In this report, we summarize measurements made by the plasma experiment on the Ulysses spacecraft during the period designated as “Whole Sun Month” (WSM, August 10 to September 8, 1996). This interval coincided with the return of solar wind variability at Ulysses. Ulysses was located at ∼ 28°N heliographic latitude, at a heliocentric distance of 4.25 AU, and on the opposite side of the Sun from Earth. In particular, we explore the evolution of the solar wind between the Sun and Ulysses for several rotations surrounding WSM. Specifically, we map Ulysses measurements back toward the Sun by applying a two‐dimensional inverse MHD algorithm. This approach is compared with the commonly used constant speed (or ballistic) approximation. We find that the MHD mapping technique produces substantially better results when compared with solar observations. Both the Ulysses MHD‐mapped results and the solar observations are consistent with a picture of a modestly tilted streamer belt (< 10°) that was deformed northward by an active region at 240° –; 270° longitude.
doi_str_mv 10.1029/1998JA900078
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_27102121</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>27102121</sourcerecordid><originalsourceid>FETCH-LOGICAL-c3777-333927ca197e1d6aa3eb82558f439692a4d1fbbb07b533b1542683319e6c60db3</originalsourceid><addsrcrecordid>eNqF0L1OwzAUhmELgUQFbFyAJyYCPnYSx2OFoFD-pBbEaNnJKQ24SbBTSu-eVEEIFpgsWc93hpeQQ2AnwLg6BaWy8VAxxmS2RQYckjTinPFtMmAQZxHjXO6SgxBeOsLiJI0ZDMjrBJ1py7oK87KhFtsVYkUf3ToEDLRxJiwMrW1A_94zaqqChtoZ__u7WPqyeqbtHOnTvHZIp8uK3tZVO6e5WTSmfK72yc7MuIAHX-8eebw4fzi7jG7uR1dnw5soF1LKSAihuMwNKIlQpMYItBlPkmwWC5UqbuICZtZaJm0ihIUk5mkmBChM85QVVuyRo_5u4-u3JYZWL8qQo3OmwnoZNJddMODwL4QM2KZdB497mPs6BI8z3fhyYfxaA9Ob-vpn_Y6Lnq9Kh-s_rR6PJkOIRSa7VdSvytDix_fK-FedSiET_XQ30g_qGibX07EW4hPk55Wt</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>18100148</pqid></control><display><type>article</type><title>Relationship between Ulysses plasma observations and solar observations during the Whole Sun Month campaign</title><source>Wiley Online Library Free Content</source><source>Access via Wiley Online Library</source><source>Wiley-Blackwell AGU Digital Library</source><source>Alma/SFX Local Collection</source><creator>Riley, Pete ; Gosling, J. T. ; McComas, D. J. ; Pizzo, V. J. ; Luhmann, J. G. ; Biesecker, D. ; Forsyth, R. J. ; Hoeksema, J. T. ; Lecinski, A. ; Thompson, B. J.</creator><creatorcontrib>Riley, Pete ; Gosling, J. T. ; McComas, D. J. ; Pizzo, V. J. ; Luhmann, J. G. ; Biesecker, D. ; Forsyth, R. J. ; Hoeksema, J. T. ; Lecinski, A. ; Thompson, B. J.</creatorcontrib><description>In this report, we summarize measurements made by the plasma experiment on the Ulysses spacecraft during the period designated as “Whole Sun Month” (WSM, August 10 to September 8, 1996). This interval coincided with the return of solar wind variability at Ulysses. Ulysses was located at ∼ 28°N heliographic latitude, at a heliocentric distance of 4.25 AU, and on the opposite side of the Sun from Earth. In particular, we explore the evolution of the solar wind between the Sun and Ulysses for several rotations surrounding WSM. Specifically, we map Ulysses measurements back toward the Sun by applying a two‐dimensional inverse MHD algorithm. This approach is compared with the commonly used constant speed (or ballistic) approximation. We find that the MHD mapping technique produces substantially better results when compared with solar observations. Both the Ulysses MHD‐mapped results and the solar observations are consistent with a picture of a modestly tilted streamer belt (&lt; 10°) that was deformed northward by an active region at 240° –; 270° longitude.</description><identifier>ISSN: 0148-0227</identifier><identifier>EISSN: 2156-2202</identifier><identifier>DOI: 10.1029/1998JA900078</identifier><language>eng</language><publisher>Blackwell Publishing Ltd</publisher><ispartof>Journal of Geophysical Research, 1999-05, Vol.104 (A5), p.9871-9879</ispartof><rights>Copyright 1999 by the American Geophysical Union.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3777-333927ca197e1d6aa3eb82558f439692a4d1fbbb07b533b1542683319e6c60db3</citedby><cites>FETCH-LOGICAL-c3777-333927ca197e1d6aa3eb82558f439692a4d1fbbb07b533b1542683319e6c60db3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F1998JA900078$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F1998JA900078$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,1433,11514,27924,27925,45574,45575,46409,46468,46833,46892</link.rule.ids></links><search><creatorcontrib>Riley, Pete</creatorcontrib><creatorcontrib>Gosling, J. T.</creatorcontrib><creatorcontrib>McComas, D. J.</creatorcontrib><creatorcontrib>Pizzo, V. J.</creatorcontrib><creatorcontrib>Luhmann, J. G.</creatorcontrib><creatorcontrib>Biesecker, D.</creatorcontrib><creatorcontrib>Forsyth, R. J.</creatorcontrib><creatorcontrib>Hoeksema, J. T.</creatorcontrib><creatorcontrib>Lecinski, A.</creatorcontrib><creatorcontrib>Thompson, B. J.</creatorcontrib><title>Relationship between Ulysses plasma observations and solar observations during the Whole Sun Month campaign</title><title>Journal of Geophysical Research</title><addtitle>J. Geophys. Res</addtitle><description>In this report, we summarize measurements made by the plasma experiment on the Ulysses spacecraft during the period designated as “Whole Sun Month” (WSM, August 10 to September 8, 1996). This interval coincided with the return of solar wind variability at Ulysses. Ulysses was located at ∼ 28°N heliographic latitude, at a heliocentric distance of 4.25 AU, and on the opposite side of the Sun from Earth. In particular, we explore the evolution of the solar wind between the Sun and Ulysses for several rotations surrounding WSM. Specifically, we map Ulysses measurements back toward the Sun by applying a two‐dimensional inverse MHD algorithm. This approach is compared with the commonly used constant speed (or ballistic) approximation. We find that the MHD mapping technique produces substantially better results when compared with solar observations. Both the Ulysses MHD‐mapped results and the solar observations are consistent with a picture of a modestly tilted streamer belt (&lt; 10°) that was deformed northward by an active region at 240° –; 270° longitude.</description><issn>0148-0227</issn><issn>2156-2202</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1999</creationdate><recordtype>article</recordtype><recordid>eNqF0L1OwzAUhmELgUQFbFyAJyYCPnYSx2OFoFD-pBbEaNnJKQ24SbBTSu-eVEEIFpgsWc93hpeQQ2AnwLg6BaWy8VAxxmS2RQYckjTinPFtMmAQZxHjXO6SgxBeOsLiJI0ZDMjrBJ1py7oK87KhFtsVYkUf3ToEDLRxJiwMrW1A_94zaqqChtoZ__u7WPqyeqbtHOnTvHZIp8uK3tZVO6e5WTSmfK72yc7MuIAHX-8eebw4fzi7jG7uR1dnw5soF1LKSAihuMwNKIlQpMYItBlPkmwWC5UqbuICZtZaJm0ihIUk5mkmBChM85QVVuyRo_5u4-u3JYZWL8qQo3OmwnoZNJddMODwL4QM2KZdB497mPs6BI8z3fhyYfxaA9Ob-vpn_Y6Lnq9Kh-s_rR6PJkOIRSa7VdSvytDix_fK-FedSiET_XQ30g_qGibX07EW4hPk55Wt</recordid><startdate>19990501</startdate><enddate>19990501</enddate><creator>Riley, Pete</creator><creator>Gosling, J. T.</creator><creator>McComas, D. J.</creator><creator>Pizzo, V. J.</creator><creator>Luhmann, J. G.</creator><creator>Biesecker, D.</creator><creator>Forsyth, R. J.</creator><creator>Hoeksema, J. T.</creator><creator>Lecinski, A.</creator><creator>Thompson, B. J.</creator><general>Blackwell Publishing Ltd</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>19990501</creationdate><title>Relationship between Ulysses plasma observations and solar observations during the Whole Sun Month campaign</title><author>Riley, Pete ; Gosling, J. T. ; McComas, D. J. ; Pizzo, V. J. ; Luhmann, J. G. ; Biesecker, D. ; Forsyth, R. J. ; Hoeksema, J. T. ; Lecinski, A. ; Thompson, B. J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3777-333927ca197e1d6aa3eb82558f439692a4d1fbbb07b533b1542683319e6c60db3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1999</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Riley, Pete</creatorcontrib><creatorcontrib>Gosling, J. T.</creatorcontrib><creatorcontrib>McComas, D. J.</creatorcontrib><creatorcontrib>Pizzo, V. J.</creatorcontrib><creatorcontrib>Luhmann, J. G.</creatorcontrib><creatorcontrib>Biesecker, D.</creatorcontrib><creatorcontrib>Forsyth, R. J.</creatorcontrib><creatorcontrib>Hoeksema, J. T.</creatorcontrib><creatorcontrib>Lecinski, A.</creatorcontrib><creatorcontrib>Thompson, B. J.</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of Geophysical Research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Riley, Pete</au><au>Gosling, J. T.</au><au>McComas, D. J.</au><au>Pizzo, V. J.</au><au>Luhmann, J. G.</au><au>Biesecker, D.</au><au>Forsyth, R. J.</au><au>Hoeksema, J. T.</au><au>Lecinski, A.</au><au>Thompson, B. J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Relationship between Ulysses plasma observations and solar observations during the Whole Sun Month campaign</atitle><jtitle>Journal of Geophysical Research</jtitle><addtitle>J. Geophys. Res</addtitle><date>1999-05-01</date><risdate>1999</risdate><volume>104</volume><issue>A5</issue><spage>9871</spage><epage>9879</epage><pages>9871-9879</pages><issn>0148-0227</issn><eissn>2156-2202</eissn><abstract>In this report, we summarize measurements made by the plasma experiment on the Ulysses spacecraft during the period designated as “Whole Sun Month” (WSM, August 10 to September 8, 1996). This interval coincided with the return of solar wind variability at Ulysses. Ulysses was located at ∼ 28°N heliographic latitude, at a heliocentric distance of 4.25 AU, and on the opposite side of the Sun from Earth. In particular, we explore the evolution of the solar wind between the Sun and Ulysses for several rotations surrounding WSM. Specifically, we map Ulysses measurements back toward the Sun by applying a two‐dimensional inverse MHD algorithm. This approach is compared with the commonly used constant speed (or ballistic) approximation. We find that the MHD mapping technique produces substantially better results when compared with solar observations. Both the Ulysses MHD‐mapped results and the solar observations are consistent with a picture of a modestly tilted streamer belt (&lt; 10°) that was deformed northward by an active region at 240° –; 270° longitude.</abstract><pub>Blackwell Publishing Ltd</pub><doi>10.1029/1998JA900078</doi><tpages>9</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0148-0227
ispartof Journal of Geophysical Research, 1999-05, Vol.104 (A5), p.9871-9879
issn 0148-0227
2156-2202
language eng
recordid cdi_proquest_miscellaneous_27102121
source Wiley Online Library Free Content; Access via Wiley Online Library; Wiley-Blackwell AGU Digital Library; Alma/SFX Local Collection
title Relationship between Ulysses plasma observations and solar observations during the Whole Sun Month campaign
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-29T17%3A03%3A48IST&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=Relationship%20between%20Ulysses%20plasma%20observations%20and%20solar%20observations%20during%20the%20Whole%20Sun%20Month%20campaign&rft.jtitle=Journal%20of%20Geophysical%20Research&rft.au=Riley,%20Pete&rft.date=1999-05-01&rft.volume=104&rft.issue=A5&rft.spage=9871&rft.epage=9879&rft.pages=9871-9879&rft.issn=0148-0227&rft.eissn=2156-2202&rft_id=info:doi/10.1029/1998JA900078&rft_dat=%3Cproquest_cross%3E27102121%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=18100148&rft_id=info:pmid/&rfr_iscdi=true