PMID- 33294305 OWN - NLM STAT- PubMed-not-MEDLINE LR - 20210110 IS - 2169-9097 (Print) IS - 2169-9100 (Electronic) IS - 2169-9097 (Linking) VI - 123 IP - 5 DP - 2018 May TI - Constraining the Potential Liquid Water Environment at Gale Crater, Mars. PG - 1156-1167 LID - 10.1002/2018je005558 [doi] AB - The Mars Science Laboratory (MSL) Rover Environmental Monitoring Station (REMS) has now made continuous in situ meteorological measurements for several Martian years at Gale crater, Mars. Of importance in the search for liquid formation are REMS' measurements of ground temperature and in-air measurements of temperature and relative humidity, which is with respect to ice. Such data can constrain the surface and subsurface stability of brines. Here we use updated calibrations to REMS data and consistent relative humidity comparisons (i.e., with respect to liquid versus with respect to ice) to investigate the potential formation of surface and subsurface liquids throughout MSL's traverse. We specifically study the potential for the deliquescence of calcium perchlorate. Our data analysis suggests that surface brine formation is not favored within the first 1648 sols as there are only two times (sols 1232 and 1311) when humidity-temperature conditions were within error consistent with a liquid phase. On the other hand, modeling of the subsurface environment would support brine production in the shallow subsurface. Indeed, we find that the shallow subsurface for terrains with low thermal inertia (Gamma less, similar 300 J m(-2) K(-1) s(-1/2)) may be occasionally favorable to brine formation through deliquescence. Terrains with Gamma less, similar 175 J m(-2) K(-1) s(-1/2) and albedos of greater, similar0.25 are the most apt to subsurface brine formation. Should brines form, they would occur around Ls 100 degrees . Their predicted properties would not meet the Special nor Uncertain Region requirements, as such they would not be potential habitable environments to life as we know it. FAU - Rivera-Valentin, Edgard G AU - Rivera-Valentin EG AUID- ORCID: 0000-0002-4042-003X AD - Arecibo Observatory, Universities Space Research Association, Arecibo, PR, USA. AD - Lunar and Planetary Institute, Universities Space Research Association, Houston, TX, USA. FAU - Gough, Raina V AU - Gough RV AUID- ORCID: 0000-0003-2755-7282 AD - Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA. AD - Department of Chemistry and Biochemistry, University of Colorado Boulder, Boulder, CO, USA. FAU - Chevrier, Vincent F AU - Chevrier VF AUID- ORCID: 0000-0002-1111-587X AD - Arkansas Center for Space and Planetary Sciences, University of Arkansas, Fayetteville, AR, USA. FAU - Primm, Katherine M AU - Primm KM AUID- ORCID: 0000-0002-9047-5370 AD - Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA. AD - Department of Chemistry and Biochemistry, University of Colorado Boulder, Boulder, CO, USA. FAU - Martinez, German M AU - Martinez GM AUID- ORCID: 0000-0001-5885-236X AD - Department of Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, MI, USA. FAU - Tolbert, Margaret AU - Tolbert M AUID- ORCID: 0000-0001-5730-6412 AD - Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA. AD - Department of Chemistry and Biochemistry, University of Colorado Boulder, Boulder, CO, USA. LA - eng GR - NNX15AM42G/NASA/NASA/United States PT - Journal Article DEP - 20180331 PL - United States TA - J Geophys Res Planets JT - Journal of geophysical research. Planets JID - 101661797 PMC - PMC7720553 MID - NIHMS995954 EDAT- 2018/05/01 00:00 MHDA- 2018/05/01 00:01 PMCR- 2020/12/07 CRDT- 2020/12/09 06:15 PHST- 2020/12/09 06:15 [entrez] PHST- 2018/05/01 00:00 [pubmed] PHST- 2018/05/01 00:01 [medline] PHST- 2020/12/07 00:00 [pmc-release] AID - 10.1002/2018je005558 [doi] PST - ppublish SO - J Geophys Res Planets. 2018 May;123(5):1156-1167. doi: 10.1002/2018je005558. Epub 2018 Mar 31.