Three Years of ACB Phase Function Observations from the Mars Science Laboratory: Interannual and Diurnal Variability and Constraints on Ice Crystal Habit

We examine 3 yr of phase-function observations of water-ice clouds taken during the Aphelion Cloud Belt season by the Mars Science Laboratory (MSL). We derive lower-bound single-scattering phase functions for Mars years (MYs) 34, 35, and 36, over a range of scattering angles from 45° to 155°, expand...

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Published in:The Planetary Science Journal
Main Authors: Alex C. Innanen, Brittney A. Cooper, Conor W. Hayes, Charissa L. Campbell, Jacob L. Kloos, Scott D. Guzewich, John E. Moores
Format: Article
Language:English
Published: IOP Publishing 2024-01-01
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Online Access:https://doi.org/10.3847/PSJ/ad2990
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author Alex C. Innanen
Brittney A. Cooper
Conor W. Hayes
Charissa L. Campbell
Jacob L. Kloos
Scott D. Guzewich
John E. Moores
author_facet Alex C. Innanen
Brittney A. Cooper
Conor W. Hayes
Charissa L. Campbell
Jacob L. Kloos
Scott D. Guzewich
John E. Moores
author_sort Alex C. Innanen
collection DOAJ
container_title The Planetary Science Journal
description We examine 3 yr of phase-function observations of water-ice clouds taken during the Aphelion Cloud Belt season by the Mars Science Laboratory (MSL). We derive lower-bound single-scattering phase functions for Mars years (MYs) 34, 35, and 36, over a range of scattering angles from 45° to 155°, expanding on the MY 34 phase function previously derived from MSL observations using the same method. We also modify the procedure used for MY 34 to make use of cloud opacity values derived from other MSL observations, often taken in conjunction with the phase-function observations. From these, we see little variability, both interannually and diurnally in the phase function at Gale Crater. We use our derived phase functions to attempt to constrain a dominant ice-crystal geometry by fitting a two-term Henyey–Greenstein function. In comparing to HG functions of Martian dust and modeled water-ice crystals, we see agreement especially with droxtal water-ice crystals, dust at Gale crater, and irregular volcanic glasses. This could be indicative of crystals composed of some irregular shape.
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spelling doaj-art-e0d645bdcd6b4cfbb582565cdcb0c39d2025-08-19T23:02:19ZengIOP PublishingThe Planetary Science Journal2632-33382024-01-01537210.3847/PSJ/ad2990Three Years of ACB Phase Function Observations from the Mars Science Laboratory: Interannual and Diurnal Variability and Constraints on Ice Crystal HabitAlex C. Innanen0https://orcid.org/0000-0002-4059-2296Brittney A. Cooper1https://orcid.org/0000-0002-7842-6496Conor W. Hayes2https://orcid.org/0000-0003-4439-0461Charissa L. Campbell3https://orcid.org/0000-0002-8395-4103Jacob L. Kloos4https://orcid.org/0000-0001-8981-0197Scott D. Guzewich5https://orcid.org/0000-0003-1149-7385John E. Moores6https://orcid.org/0000-0001-9435-1095Centre for Research in Earth and Space Science York University Toronto, Ontario, Canada ; ainnanen@yorku.caNOIRLab Gemini North Observatory Hilo , HI, USA; Sierra Space Broomfield , CO, USACentre for Research in Earth and Space Science York University Toronto, Ontario, Canada ; ainnanen@yorku.caCentre for Research in Earth and Space Science York University Toronto, Ontario, Canada ; ainnanen@yorku.ca; NASA Goddard Space Flight Center Greenbelt , MD, USADepartment of Astronomy University of Maryland College Park, MD, USANASA Goddard Space Flight Center Greenbelt , MD, USACentre for Research in Earth and Space Science York University Toronto, Ontario, Canada ; ainnanen@yorku.caWe examine 3 yr of phase-function observations of water-ice clouds taken during the Aphelion Cloud Belt season by the Mars Science Laboratory (MSL). We derive lower-bound single-scattering phase functions for Mars years (MYs) 34, 35, and 36, over a range of scattering angles from 45° to 155°, expanding on the MY 34 phase function previously derived from MSL observations using the same method. We also modify the procedure used for MY 34 to make use of cloud opacity values derived from other MSL observations, often taken in conjunction with the phase-function observations. From these, we see little variability, both interannually and diurnally in the phase function at Gale Crater. We use our derived phase functions to attempt to constrain a dominant ice-crystal geometry by fitting a two-term Henyey–Greenstein function. In comparing to HG functions of Martian dust and modeled water-ice crystals, we see agreement especially with droxtal water-ice crystals, dust at Gale crater, and irregular volcanic glasses. This could be indicative of crystals composed of some irregular shape.https://doi.org/10.3847/PSJ/ad2990MarsWater vaporPlanetary atmospheresAtmospheric clouds
spellingShingle Alex C. Innanen
Brittney A. Cooper
Conor W. Hayes
Charissa L. Campbell
Jacob L. Kloos
Scott D. Guzewich
John E. Moores
Three Years of ACB Phase Function Observations from the Mars Science Laboratory: Interannual and Diurnal Variability and Constraints on Ice Crystal Habit
Mars
Water vapor
Planetary atmospheres
Atmospheric clouds
title Three Years of ACB Phase Function Observations from the Mars Science Laboratory: Interannual and Diurnal Variability and Constraints on Ice Crystal Habit
title_full Three Years of ACB Phase Function Observations from the Mars Science Laboratory: Interannual and Diurnal Variability and Constraints on Ice Crystal Habit
title_fullStr Three Years of ACB Phase Function Observations from the Mars Science Laboratory: Interannual and Diurnal Variability and Constraints on Ice Crystal Habit
title_full_unstemmed Three Years of ACB Phase Function Observations from the Mars Science Laboratory: Interannual and Diurnal Variability and Constraints on Ice Crystal Habit
title_short Three Years of ACB Phase Function Observations from the Mars Science Laboratory: Interannual and Diurnal Variability and Constraints on Ice Crystal Habit
title_sort three years of acb phase function observations from the mars science laboratory interannual and diurnal variability and constraints on ice crystal habit
topic Mars
Water vapor
Planetary atmospheres
Atmospheric clouds
url https://doi.org/10.3847/PSJ/ad2990
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