Possibility of microscopic liquid water formation at landing sites on Mars and their observational potential

•We predict the appearance of microscopic liquid water on Mars on hygroscopic mineral surfaces.•The ideal periods are mostly during nighttime between 2–7 am.•At most of the former landing sites such microscopic liquid could have appeared.•We predict these ideal periods for the ExoMars rover’s candid...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Icarus (New York, N.Y. 1962) N.Y. 1962), 2017-01, Vol.282, p.84-92
Hauptverfasser: Pal, B, Kereszturi, A
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 92
container_issue
container_start_page 84
container_title Icarus (New York, N.Y. 1962)
container_volume 282
creator Pal, B
Kereszturi, A
description •We predict the appearance of microscopic liquid water on Mars on hygroscopic mineral surfaces.•The ideal periods are mostly during nighttime between 2–7 am.•At most of the former landing sites such microscopic liquid could have appeared.•We predict these ideal periods for the ExoMars rover’s candidate landing sites.•This period at the primary landing site (Oxia Planum) is LS = 115–225 and in Local Time = 2–5. Microscopic liquid brines, especially calcium-perchlorate could emerge by deliquescence on Mars during night time hours. Using climate model computations and orbital humidity observations, the ideal periods and their annual plus daily characteristics at various past, current and future landing sites were compared. Such results provide context for future analysis and targeting the related observations by the next missions for Mars. Based on the analysis, at most (but not all) past missions’ landing sites, microscopic brine could emerge during night time for different durations. Analysing the conditions at ExoMars rover’s primary landing site at Oxia Planum, the best annual period was found to be between Ls 115–225, and in LocalTime 2–5, after midnight. In an ideal case, 4 h of continuous liquid phase can emerge there. Local conditions might cause values to differ from those estimated by the model. Thermal inertia could especially make such differences (low TI values favour fast cooling and H2O cold trapping at loose surfaces) and the concentration of calcium-perchlorate salt in the regolith also influences the process (it might occur preferentially at long-term exposed surfaces without recent loose dust coverage). These factors should be taken into account while targeting future liquid water observations on Mars.
doi_str_mv 10.1016/j.icarus.2016.09.006
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1864534464</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0019103516305681</els_id><sourcerecordid>1846392575</sourcerecordid><originalsourceid>FETCH-LOGICAL-a395t-4523610ad2254be90b73ef1167ae959df0bbaf3c70b47929abe43e5cd274d4f3</originalsourceid><addsrcrecordid>eNqFUcFOGzEQtRBIDZQ_6MHHXnYZr-1dfEGqIgpIqdoDd8vrnYWJNutgO6ny9ziEc3sazdN7TzPvMfZNQC1AtDfrmryLu1Q3ZavB1ADtGVsIMFA1rZLnbAEgTCVA6i_sMqU1AOhbIxds-hNSop4mygceRr4hH0PyYUueT_S2o4H_dRkjH0PcuExh5i7zyc0DzS88UcbEC_bLxcQLyPMrUuShTxj3H3Q38W3IOGdy01d2Mbop4fXnvGLPP--fl4_V6vfD0_LHqnLS6Fwp3chWgBuaRqseDfSdxFGItnNotBlG6Hs3St9BrzrTGNejkqj90HRqUKO8Yt9PttsY3naYst1Q8jiVqzHskhW3rdJSqZLM_6mqlabRnS5UdaIeA0oRR7uNtHHxYAXYYw12bU812GMNFowtNRTZ3UmG5eE9YbTJE84eB4rosx0C_dvgHZMmlMs</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1846392575</pqid></control><display><type>article</type><title>Possibility of microscopic liquid water formation at landing sites on Mars and their observational potential</title><source>ScienceDirect Journals (5 years ago - present)</source><creator>Pal, B ; Kereszturi, A</creator><creatorcontrib>Pal, B ; Kereszturi, A</creatorcontrib><description>•We predict the appearance of microscopic liquid water on Mars on hygroscopic mineral surfaces.•The ideal periods are mostly during nighttime between 2–7 am.•At most of the former landing sites such microscopic liquid could have appeared.•We predict these ideal periods for the ExoMars rover’s candidate landing sites.•This period at the primary landing site (Oxia Planum) is LS = 115–225 and in Local Time = 2–5. Microscopic liquid brines, especially calcium-perchlorate could emerge by deliquescence on Mars during night time hours. Using climate model computations and orbital humidity observations, the ideal periods and their annual plus daily characteristics at various past, current and future landing sites were compared. Such results provide context for future analysis and targeting the related observations by the next missions for Mars. Based on the analysis, at most (but not all) past missions’ landing sites, microscopic brine could emerge during night time for different durations. Analysing the conditions at ExoMars rover’s primary landing site at Oxia Planum, the best annual period was found to be between Ls 115–225, and in LocalTime 2–5, after midnight. In an ideal case, 4 h of continuous liquid phase can emerge there. Local conditions might cause values to differ from those estimated by the model. Thermal inertia could especially make such differences (low TI values favour fast cooling and H2O cold trapping at loose surfaces) and the concentration of calcium-perchlorate salt in the regolith also influences the process (it might occur preferentially at long-term exposed surfaces without recent loose dust coverage). These factors should be taken into account while targeting future liquid water observations on Mars.</description><identifier>ISSN: 0019-1035</identifier><identifier>EISSN: 1090-2643</identifier><identifier>DOI: 10.1016/j.icarus.2016.09.006</identifier><language>eng</language><publisher>Elsevier Inc</publisher><subject>Brines ; Cold traps ; Cooling ; Deliquescence ; ExoMars ; Landing sites ; Liquid water ; Mars ; Mars missions ; Mission planning ; Night ; Trapping ; Water</subject><ispartof>Icarus (New York, N.Y. 1962), 2017-01, Vol.282, p.84-92</ispartof><rights>2016 Elsevier Inc.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a395t-4523610ad2254be90b73ef1167ae959df0bbaf3c70b47929abe43e5cd274d4f3</citedby><cites>FETCH-LOGICAL-a395t-4523610ad2254be90b73ef1167ae959df0bbaf3c70b47929abe43e5cd274d4f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.icarus.2016.09.006$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3548,27922,27923,45993</link.rule.ids></links><search><creatorcontrib>Pal, B</creatorcontrib><creatorcontrib>Kereszturi, A</creatorcontrib><title>Possibility of microscopic liquid water formation at landing sites on Mars and their observational potential</title><title>Icarus (New York, N.Y. 1962)</title><description>•We predict the appearance of microscopic liquid water on Mars on hygroscopic mineral surfaces.•The ideal periods are mostly during nighttime between 2–7 am.•At most of the former landing sites such microscopic liquid could have appeared.•We predict these ideal periods for the ExoMars rover’s candidate landing sites.•This period at the primary landing site (Oxia Planum) is LS = 115–225 and in Local Time = 2–5. Microscopic liquid brines, especially calcium-perchlorate could emerge by deliquescence on Mars during night time hours. Using climate model computations and orbital humidity observations, the ideal periods and their annual plus daily characteristics at various past, current and future landing sites were compared. Such results provide context for future analysis and targeting the related observations by the next missions for Mars. Based on the analysis, at most (but not all) past missions’ landing sites, microscopic brine could emerge during night time for different durations. Analysing the conditions at ExoMars rover’s primary landing site at Oxia Planum, the best annual period was found to be between Ls 115–225, and in LocalTime 2–5, after midnight. In an ideal case, 4 h of continuous liquid phase can emerge there. Local conditions might cause values to differ from those estimated by the model. Thermal inertia could especially make such differences (low TI values favour fast cooling and H2O cold trapping at loose surfaces) and the concentration of calcium-perchlorate salt in the regolith also influences the process (it might occur preferentially at long-term exposed surfaces without recent loose dust coverage). These factors should be taken into account while targeting future liquid water observations on Mars.</description><subject>Brines</subject><subject>Cold traps</subject><subject>Cooling</subject><subject>Deliquescence</subject><subject>ExoMars</subject><subject>Landing sites</subject><subject>Liquid water</subject><subject>Mars</subject><subject>Mars missions</subject><subject>Mission planning</subject><subject>Night</subject><subject>Trapping</subject><subject>Water</subject><issn>0019-1035</issn><issn>1090-2643</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNqFUcFOGzEQtRBIDZQ_6MHHXnYZr-1dfEGqIgpIqdoDd8vrnYWJNutgO6ny9ziEc3sazdN7TzPvMfZNQC1AtDfrmryLu1Q3ZavB1ADtGVsIMFA1rZLnbAEgTCVA6i_sMqU1AOhbIxds-hNSop4mygceRr4hH0PyYUueT_S2o4H_dRkjH0PcuExh5i7zyc0DzS88UcbEC_bLxcQLyPMrUuShTxj3H3Q38W3IOGdy01d2Mbop4fXnvGLPP--fl4_V6vfD0_LHqnLS6Fwp3chWgBuaRqseDfSdxFGItnNotBlG6Hs3St9BrzrTGNejkqj90HRqUKO8Yt9PttsY3naYst1Q8jiVqzHskhW3rdJSqZLM_6mqlabRnS5UdaIeA0oRR7uNtHHxYAXYYw12bU812GMNFowtNRTZ3UmG5eE9YbTJE84eB4rosx0C_dvgHZMmlMs</recordid><startdate>20170115</startdate><enddate>20170115</enddate><creator>Pal, B</creator><creator>Kereszturi, A</creator><general>Elsevier Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>20170115</creationdate><title>Possibility of microscopic liquid water formation at landing sites on Mars and their observational potential</title><author>Pal, B ; Kereszturi, A</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a395t-4523610ad2254be90b73ef1167ae959df0bbaf3c70b47929abe43e5cd274d4f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Brines</topic><topic>Cold traps</topic><topic>Cooling</topic><topic>Deliquescence</topic><topic>ExoMars</topic><topic>Landing sites</topic><topic>Liquid water</topic><topic>Mars</topic><topic>Mars missions</topic><topic>Mission planning</topic><topic>Night</topic><topic>Trapping</topic><topic>Water</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Pal, B</creatorcontrib><creatorcontrib>Kereszturi, A</creatorcontrib><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>Icarus (New York, N.Y. 1962)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Pal, B</au><au>Kereszturi, A</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Possibility of microscopic liquid water formation at landing sites on Mars and their observational potential</atitle><jtitle>Icarus (New York, N.Y. 1962)</jtitle><date>2017-01-15</date><risdate>2017</risdate><volume>282</volume><spage>84</spage><epage>92</epage><pages>84-92</pages><issn>0019-1035</issn><eissn>1090-2643</eissn><abstract>•We predict the appearance of microscopic liquid water on Mars on hygroscopic mineral surfaces.•The ideal periods are mostly during nighttime between 2–7 am.•At most of the former landing sites such microscopic liquid could have appeared.•We predict these ideal periods for the ExoMars rover’s candidate landing sites.•This period at the primary landing site (Oxia Planum) is LS = 115–225 and in Local Time = 2–5. Microscopic liquid brines, especially calcium-perchlorate could emerge by deliquescence on Mars during night time hours. Using climate model computations and orbital humidity observations, the ideal periods and their annual plus daily characteristics at various past, current and future landing sites were compared. Such results provide context for future analysis and targeting the related observations by the next missions for Mars. Based on the analysis, at most (but not all) past missions’ landing sites, microscopic brine could emerge during night time for different durations. Analysing the conditions at ExoMars rover’s primary landing site at Oxia Planum, the best annual period was found to be between Ls 115–225, and in LocalTime 2–5, after midnight. In an ideal case, 4 h of continuous liquid phase can emerge there. Local conditions might cause values to differ from those estimated by the model. Thermal inertia could especially make such differences (low TI values favour fast cooling and H2O cold trapping at loose surfaces) and the concentration of calcium-perchlorate salt in the regolith also influences the process (it might occur preferentially at long-term exposed surfaces without recent loose dust coverage). These factors should be taken into account while targeting future liquid water observations on Mars.</abstract><pub>Elsevier Inc</pub><doi>10.1016/j.icarus.2016.09.006</doi><tpages>9</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0019-1035
ispartof Icarus (New York, N.Y. 1962), 2017-01, Vol.282, p.84-92
issn 0019-1035
1090-2643
language eng
recordid cdi_proquest_miscellaneous_1864534464
source ScienceDirect Journals (5 years ago - present)
subjects Brines
Cold traps
Cooling
Deliquescence
ExoMars
Landing sites
Liquid water
Mars
Mars missions
Mission planning
Night
Trapping
Water
title Possibility of microscopic liquid water formation at landing sites on Mars and their observational potential
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-13T20%3A59%3A21IST&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=Possibility%20of%20microscopic%20liquid%20water%20formation%20at%20landing%20sites%20on%20Mars%20and%20their%20observational%20potential&rft.jtitle=Icarus%20(New%20York,%20N.Y.%201962)&rft.au=Pal,%20B&rft.date=2017-01-15&rft.volume=282&rft.spage=84&rft.epage=92&rft.pages=84-92&rft.issn=0019-1035&rft.eissn=1090-2643&rft_id=info:doi/10.1016/j.icarus.2016.09.006&rft_dat=%3Cproquest_cross%3E1846392575%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=1846392575&rft_id=info:pmid/&rft_els_id=S0019103516305681&rfr_iscdi=true