Latitudinal and Longitudinal Oscillations of Cloud Features on Neptune
Voyager observations suggest that three of Neptune's major cloud features oscillate in latitude by 2° to 4° and that two of them simultaneously oscillate in longitude by 7.8° and 98° about their mean drift longitudes. The observations define most convincingly the two orthogonal oscillations of...
Gespeichert in:
Veröffentlicht in: | Science (American Association for the Advancement of Science) 1991-11, Vol.254 (5032), p.684-686 |
---|---|
1. Verfasser: | |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 686 |
---|---|
container_issue | 5032 |
container_start_page | 684 |
container_title | Science (American Association for the Advancement of Science) |
container_volume | 254 |
creator | Sromovsky, Lawrence A. |
description | Voyager observations suggest that three of Neptune's major cloud features oscillate in latitude by 2° to 4° and that two of them simultaneously oscillate in longitude by 7.8° and 98° about their mean drift longitudes. The observations define most convincingly the two orthogonal oscillations of the second dark spot (near 53° south). These oscillations have similar periods near 800 hours and approximately satisfy a simple advective model in which a latitudinal oscillation produces a phase-shifted longitudinal oscillation proportional to the local wind shear. The latitudinal motion of the Great Dark Spot can be fit with an oscillation period of about 2550 hours, whereas its dominant longitudinal motion, if oscillatory at all, has such a long period that it is not well constrained by the Voyager data. |
doi_str_mv | 10.1126/science.254.5032.684 |
format | Article |
fullrecord | <record><control><sourceid>gale_proqu</sourceid><recordid>TN_cdi_proquest_miscellaneous_743282789</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A11518274</galeid><jstor_id>2879275</jstor_id><sourcerecordid>A11518274</sourcerecordid><originalsourceid>FETCH-LOGICAL-c772t-401f134abca5e250a6bf776d0c1fdd6703263092b4f3675b9f23f85c1061cd823</originalsourceid><addsrcrecordid>eNqN00uP0zAQAGALgdhS-AcrFHFYOGyKn7F9XCpaVqq2Bx5Xy3HsKlVqFzuR4N_j0mpXRRWtcog0_sb2ZDIAXCM4QQhXH5NprTd2ghmdMEjwpBL0GRghKFkpMSTPwQhCUpUCcnYFXqW0hjCvSfISXCHOOeWSjMBsofu2H5rW667QvikWwa8eA8t8SNdlEXwqgiumXRiaYmZ1P0SbI754sNt-8PY1eOF0l-ybw3sMvs8-f5t-KRfL-f30blEaznFfUogcIlTXRjOLGdRV7TivGmiQa5qK5zIqAiWuqSMVZ7V0mDjBDIIVMo3AZAze7_fdxvBzsKlXmzYZm-_obRiS4pRggbmQ5yUhGGLxV978V2KGGceCnIeIUsYgPgtRrgRLyTJ89w9chyHmL7_bjDCGRbU79naPVrqzqvUu9FGblfU26i5469ocvkOI5W1z_WNQnuD5aeymNaf8hyOfSW9_9Ss9pKTuvz5cTJc_Lqaf5pdSMV8c0dtT1ISusyur8q82XR5xuucmhpSidWob242OvxWCajdE6jBEucdU7YZI5SHKaW8PXRnqjW2ekg5Tk8H1HnidtPJ9zC2VeeYggYyKp-V16kN8TMeCS8wZ-QPYhSOq</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>213552863</pqid></control><display><type>article</type><title>Latitudinal and Longitudinal Oscillations of Cloud Features on Neptune</title><source>American Association for the Advancement of Science</source><source>Jstor Complete Legacy</source><source>NASA Technical Reports Server</source><creator>Sromovsky, Lawrence A.</creator><creatorcontrib>Sromovsky, Lawrence A.</creatorcontrib><description>Voyager observations suggest that three of Neptune's major cloud features oscillate in latitude by 2° to 4° and that two of them simultaneously oscillate in longitude by 7.8° and 98° about their mean drift longitudes. The observations define most convincingly the two orthogonal oscillations of the second dark spot (near 53° south). These oscillations have similar periods near 800 hours and approximately satisfy a simple advective model in which a latitudinal oscillation produces a phase-shifted longitudinal oscillation proportional to the local wind shear. The latitudinal motion of the Great Dark Spot can be fit with an oscillation period of about 2550 hours, whereas its dominant longitudinal motion, if oscillatory at all, has such a long period that it is not well constrained by the Voyager data.</description><identifier>ISSN: 0036-8075</identifier><identifier>EISSN: 1095-9203</identifier><identifier>DOI: 10.1126/science.254.5032.684</identifier><identifier>PMID: 17774793</identifier><identifier>CODEN: SCIEAS</identifier><language>eng</language><publisher>Legacy CDMS: American Society for the Advancement of Science</publisher><subject>Atmosphere ; Axes of rotation ; Clouds ; Clouds (Meteorology) ; Empirical modeling ; Lunar And Planetary Exploration ; Neptune ; Neptune (Planet) ; Oscillation ; Phase shift ; Planetary atmospheres ; Planets ; Rotation ; Scooters ; Wind shear</subject><ispartof>Science (American Association for the Advancement of Science), 1991-11, Vol.254 (5032), p.684-686</ispartof><rights>Copyright 1991 American Association for the Advancement of Science</rights><rights>COPYRIGHT 1991 American Association for the Advancement of Science</rights><rights>COPYRIGHT 1991 American Association for the Advancement of Science</rights><rights>Copyright American Association for the Advancement of Science Nov 1, 1991</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c772t-401f134abca5e250a6bf776d0c1fdd6703263092b4f3675b9f23f85c1061cd823</citedby><cites>FETCH-LOGICAL-c772t-401f134abca5e250a6bf776d0c1fdd6703263092b4f3675b9f23f85c1061cd823</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/2879275$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/2879275$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,778,782,801,2873,2874,27911,27912,58004,58237</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/17774793$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Sromovsky, Lawrence A.</creatorcontrib><title>Latitudinal and Longitudinal Oscillations of Cloud Features on Neptune</title><title>Science (American Association for the Advancement of Science)</title><addtitle>Science</addtitle><description>Voyager observations suggest that three of Neptune's major cloud features oscillate in latitude by 2° to 4° and that two of them simultaneously oscillate in longitude by 7.8° and 98° about their mean drift longitudes. The observations define most convincingly the two orthogonal oscillations of the second dark spot (near 53° south). These oscillations have similar periods near 800 hours and approximately satisfy a simple advective model in which a latitudinal oscillation produces a phase-shifted longitudinal oscillation proportional to the local wind shear. The latitudinal motion of the Great Dark Spot can be fit with an oscillation period of about 2550 hours, whereas its dominant longitudinal motion, if oscillatory at all, has such a long period that it is not well constrained by the Voyager data.</description><subject>Atmosphere</subject><subject>Axes of rotation</subject><subject>Clouds</subject><subject>Clouds (Meteorology)</subject><subject>Empirical modeling</subject><subject>Lunar And Planetary Exploration</subject><subject>Neptune</subject><subject>Neptune (Planet)</subject><subject>Oscillation</subject><subject>Phase shift</subject><subject>Planetary atmospheres</subject><subject>Planets</subject><subject>Rotation</subject><subject>Scooters</subject><subject>Wind shear</subject><issn>0036-8075</issn><issn>1095-9203</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1991</creationdate><recordtype>article</recordtype><sourceid>CYI</sourceid><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqN00uP0zAQAGALgdhS-AcrFHFYOGyKn7F9XCpaVqq2Bx5Xy3HsKlVqFzuR4N_j0mpXRRWtcog0_sb2ZDIAXCM4QQhXH5NprTd2ghmdMEjwpBL0GRghKFkpMSTPwQhCUpUCcnYFXqW0hjCvSfISXCHOOeWSjMBsofu2H5rW667QvikWwa8eA8t8SNdlEXwqgiumXRiaYmZ1P0SbI754sNt-8PY1eOF0l-ybw3sMvs8-f5t-KRfL-f30blEaznFfUogcIlTXRjOLGdRV7TivGmiQa5qK5zIqAiWuqSMVZ7V0mDjBDIIVMo3AZAze7_fdxvBzsKlXmzYZm-_obRiS4pRggbmQ5yUhGGLxV978V2KGGceCnIeIUsYgPgtRrgRLyTJ89w9chyHmL7_bjDCGRbU79naPVrqzqvUu9FGblfU26i5469ocvkOI5W1z_WNQnuD5aeymNaf8hyOfSW9_9Ss9pKTuvz5cTJc_Lqaf5pdSMV8c0dtT1ISusyur8q82XR5xuucmhpSidWob242OvxWCajdE6jBEucdU7YZI5SHKaW8PXRnqjW2ekg5Tk8H1HnidtPJ9zC2VeeYggYyKp-V16kN8TMeCS8wZ-QPYhSOq</recordid><startdate>19911101</startdate><enddate>19911101</enddate><creator>Sromovsky, Lawrence A.</creator><general>American Society for the Advancement of Science</general><general>American Association for the Advancement of Science</general><general>The American Association for the Advancement of Science</general><scope>CYE</scope><scope>CYI</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8GL</scope><scope>IBG</scope><scope>IOV</scope><scope>ISN</scope><scope>0-V</scope><scope>3V.</scope><scope>7QF</scope><scope>7QG</scope><scope>7QL</scope><scope>7QP</scope><scope>7QQ</scope><scope>7QR</scope><scope>7SC</scope><scope>7SE</scope><scope>7SN</scope><scope>7SP</scope><scope>7SR</scope><scope>7SS</scope><scope>7T7</scope><scope>7TA</scope><scope>7TB</scope><scope>7TK</scope><scope>7TM</scope><scope>7U5</scope><scope>7U9</scope><scope>7X2</scope><scope>7X7</scope><scope>7XB</scope><scope>88A</scope><scope>88B</scope><scope>88E</scope><scope>88I</scope><scope>8AF</scope><scope>8BQ</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FH</scope><scope>8FI</scope><scope>8FJ</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ALSLI</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>CJNVE</scope><scope>D1I</scope><scope>DWQXO</scope><scope>F28</scope><scope>FR3</scope><scope>FYUFA</scope><scope>GHDGH</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H8G</scope><scope>H94</scope><scope>HCIFZ</scope><scope>JG9</scope><scope>JQ2</scope><scope>K9-</scope><scope>K9.</scope><scope>KB.</scope><scope>KR7</scope><scope>L6V</scope><scope>L7M</scope><scope>LK8</scope><scope>L~C</scope><scope>L~D</scope><scope>M0K</scope><scope>M0P</scope><scope>M0R</scope><scope>M0S</scope><scope>M1P</scope><scope>M2O</scope><scope>M2P</scope><scope>M7N</scope><scope>M7P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>P64</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PDBOC</scope><scope>PQEDU</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>R05</scope><scope>RC3</scope><scope>7TG</scope><scope>KL.</scope><scope>7X8</scope></search><sort><creationdate>19911101</creationdate><title>Latitudinal and Longitudinal Oscillations of Cloud Features on Neptune</title><author>Sromovsky, Lawrence A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c772t-401f134abca5e250a6bf776d0c1fdd6703263092b4f3675b9f23f85c1061cd823</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1991</creationdate><topic>Atmosphere</topic><topic>Axes of rotation</topic><topic>Clouds</topic><topic>Clouds (Meteorology)</topic><topic>Empirical modeling</topic><topic>Lunar And Planetary Exploration</topic><topic>Neptune</topic><topic>Neptune (Planet)</topic><topic>Oscillation</topic><topic>Phase shift</topic><topic>Planetary atmospheres</topic><topic>Planets</topic><topic>Rotation</topic><topic>Scooters</topic><topic>Wind shear</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sromovsky, Lawrence A.</creatorcontrib><collection>NASA Scientific and Technical Information</collection><collection>NASA Technical Reports Server</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>Gale In Context: High School</collection><collection>Gale In Context: Biography</collection><collection>Gale In Context: Opposing Viewpoints</collection><collection>Gale In Context: Canada</collection><collection>ProQuest Social Sciences Premium Collection</collection><collection>ProQuest Central (Corporate)</collection><collection>Aluminium Industry Abstracts</collection><collection>Animal Behavior Abstracts</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Calcium & Calcified Tissue Abstracts</collection><collection>Ceramic Abstracts</collection><collection>Chemoreception Abstracts</collection><collection>Computer and Information Systems Abstracts</collection><collection>Corrosion Abstracts</collection><collection>Ecology Abstracts</collection><collection>Electronics & Communications Abstracts</collection><collection>Engineered Materials Abstracts</collection><collection>Entomology Abstracts (Full archive)</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Materials Business File</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Neurosciences Abstracts</collection><collection>Nucleic Acids Abstracts</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Virology and AIDS Abstracts</collection><collection>Agricultural Science Collection</collection><collection>Health & Medical Collection</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Biology Database (Alumni Edition)</collection><collection>Education Database (Alumni Edition)</collection><collection>Medical Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>STEM Database</collection><collection>METADEX</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>Hospital Premium Collection</collection><collection>Hospital Premium Collection (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Social Science Premium Collection</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>eLibrary</collection><collection>ProQuest Central</collection><collection>Technology Collection (ProQuest)</collection><collection>Natural Science Collection (ProQuest)</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>Education Collection</collection><collection>ProQuest Materials Science Collection</collection><collection>ProQuest Central Korea</collection><collection>ANTE: Abstracts in New Technology & Engineering</collection><collection>Engineering Research Database</collection><collection>Health Research Premium Collection</collection><collection>Health Research Premium Collection (Alumni)</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aerospace Database</collection><collection>Copper Technical Reference Library</collection><collection>AIDS and Cancer Research Abstracts</collection><collection>SciTech Premium Collection</collection><collection>Materials Research Database</collection><collection>ProQuest Computer Science Collection</collection><collection>Consumer Health Database (Alumni Edition)</collection><collection>ProQuest Health & Medical Complete (Alumni)</collection><collection>Materials Science Database</collection><collection>Civil Engineering Abstracts</collection><collection>ProQuest Engineering Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>ProQuest Biological Science Collection</collection><collection>Computer and Information Systems Abstracts Academic</collection><collection>Computer and Information Systems Abstracts Professional</collection><collection>Agricultural Science Database</collection><collection>Education Database</collection><collection>Consumer Health Database</collection><collection>Health & Medical Collection (Alumni Edition)</collection><collection>Medical Database</collection><collection>Research Library</collection><collection>Science Database (ProQuest)</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Biological Science Database</collection><collection>Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>Materials Science Collection</collection><collection>ProQuest One Education</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><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>University of Michigan</collection><collection>Genetics Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>MEDLINE - Academic</collection><jtitle>Science (American Association for the Advancement of Science)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sromovsky, Lawrence A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Latitudinal and Longitudinal Oscillations of Cloud Features on Neptune</atitle><jtitle>Science (American Association for the Advancement of Science)</jtitle><addtitle>Science</addtitle><date>1991-11-01</date><risdate>1991</risdate><volume>254</volume><issue>5032</issue><spage>684</spage><epage>686</epage><pages>684-686</pages><issn>0036-8075</issn><eissn>1095-9203</eissn><coden>SCIEAS</coden><abstract>Voyager observations suggest that three of Neptune's major cloud features oscillate in latitude by 2° to 4° and that two of them simultaneously oscillate in longitude by 7.8° and 98° about their mean drift longitudes. The observations define most convincingly the two orthogonal oscillations of the second dark spot (near 53° south). These oscillations have similar periods near 800 hours and approximately satisfy a simple advective model in which a latitudinal oscillation produces a phase-shifted longitudinal oscillation proportional to the local wind shear. The latitudinal motion of the Great Dark Spot can be fit with an oscillation period of about 2550 hours, whereas its dominant longitudinal motion, if oscillatory at all, has such a long period that it is not well constrained by the Voyager data.</abstract><cop>Legacy CDMS</cop><pub>American Society for the Advancement of Science</pub><pmid>17774793</pmid><doi>10.1126/science.254.5032.684</doi><tpages>3</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0036-8075 |
ispartof | Science (American Association for the Advancement of Science), 1991-11, Vol.254 (5032), p.684-686 |
issn | 0036-8075 1095-9203 |
language | eng |
recordid | cdi_proquest_miscellaneous_743282789 |
source | American Association for the Advancement of Science; Jstor Complete Legacy; NASA Technical Reports Server |
subjects | Atmosphere Axes of rotation Clouds Clouds (Meteorology) Empirical modeling Lunar And Planetary Exploration Neptune Neptune (Planet) Oscillation Phase shift Planetary atmospheres Planets Rotation Scooters Wind shear |
title | Latitudinal and Longitudinal Oscillations of Cloud Features on Neptune |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-15T14%3A51%3A35IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Latitudinal%20and%20Longitudinal%20Oscillations%20of%20Cloud%20Features%20on%20Neptune&rft.jtitle=Science%20(American%20Association%20for%20the%20Advancement%20of%20Science)&rft.au=Sromovsky,%20Lawrence%20A.&rft.date=1991-11-01&rft.volume=254&rft.issue=5032&rft.spage=684&rft.epage=686&rft.pages=684-686&rft.issn=0036-8075&rft.eissn=1095-9203&rft.coden=SCIEAS&rft_id=info:doi/10.1126/science.254.5032.684&rft_dat=%3Cgale_proqu%3EA11518274%3C/gale_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=213552863&rft_id=info:pmid/17774793&rft_galeid=A11518274&rft_jstor_id=2879275&rfr_iscdi=true |