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Richardson, Mark I., Newman, Claire E. (2018) On the relationship between surface pressure, terrain elevation, and air temperature. Part I: The large diurnal surface pressure range at Gale Crater, Mars and its origin due to lateral hydrostatic adjustment. Planetary and Space Science, 164. 132-157 doi:10.1016/j.pss.2018.07.003

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Reference TypeJournal (article/letter/editorial)
TitleOn the relationship between surface pressure, terrain elevation, and air temperature. Part I: The large diurnal surface pressure range at Gale Crater, Mars and its origin due to lateral hydrostatic adjustment
JournalPlanetary and Space Science
AuthorsRichardson, Mark I.Author
Newman, Claire E.Author
Year2018 (December)Volume164
PublisherElsevier BV
DOIdoi:10.1016/j.pss.2018.07.003Search in ResearchGate
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Mindat Ref. ID388122Long-form Identifiermindat:1:5:388122:8
GUID0
Full ReferenceRichardson, Mark I., Newman, Claire E. (2018) On the relationship between surface pressure, terrain elevation, and air temperature. Part I: The large diurnal surface pressure range at Gale Crater, Mars and its origin due to lateral hydrostatic adjustment. Planetary and Space Science, 164. 132-157 doi:10.1016/j.pss.2018.07.003
Plain TextRichardson, Mark I., Newman, Claire E. (2018) On the relationship between surface pressure, terrain elevation, and air temperature. Part I: The large diurnal surface pressure range at Gale Crater, Mars and its origin due to lateral hydrostatic adjustment. Planetary and Space Science, 164. 132-157 doi:10.1016/j.pss.2018.07.003
In(2018) Planetary and Space Science Vol. 164. Elsevier BV

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