Seasonal Variations over the Zhurong Plume-disturbed Zone Indicate Modern Dust Transport in Utopia Planitia, Mars

Abstract Dust activity is critical to the modern Martian climate system and drives episodic material exchange between the surface and atmosphere. Characterizing this exchange requires numerical modeling and coordinated in situ and orbital observations, which improve constraints on atmospheric processes and support robotic mission safety. We performed reflectance cross calibration between the Tianwen-1 HiRIC and Mars Reconnaissance Orbiter (MRO) HiRISE datasets to track surface changes disturbed by landing plume effects across 2 Martian yr after the Zhurong rover’s arrival. Observations show surface reflectance rapidly recovered to prelanding conditions within the first Martian year, followed by a moderate dust-cleaning event in the subsequent spring. We conclude that the site undergoes significant dust accumulation starting in late northern summer, paired with springtime dust removal driven by convective vortices. This combined pattern of dust exchange differs from records at earlier landing sites, demonstrating substantial spatial variability in modern local dust activity across Mars.

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Publication Details

Journal
The Astronomical Journal
Published
2026-11-03
DOI
https://doi.org/10.3847/1538-3881/aeb125
Primary Topic
Planetary Science and Exploration
Type
article
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article

Seasonal Variations over the Zhurong Plume-disturbed Zone Indicate Modern Dust Transport in Utopia Planitia, Mars

Zhaopeng Chen, Jie Dong, Qiang Fu, Dafei Li et al.
The Astronomical Journal
Planetary Science and Exploration
article

Seasonal Variations over the Zhurong Plume-disturbed Zone Indicate Modern Dust Transport in Utopia Planitia, Mars

Zhaopeng Chen, Jie Dong, Qiang Fu, Dafei Li, Qing Zhang, Xinbo Zhu, Zhibin Li, GAO Mengjia, Jingjing Zhang, Wangli Chen, Renhao Tian, Jiawei Li, Chunlai Li, Jianjun Liu, Rongwei He, Yuhang Liu, Wei Yan, Pan Xie, Jia Wang
article en

Abstract

Abstract Dust activity is critical to the modern Martian climate system and drives episodic material exchange between the surface and atmosphere. Characterizing this exchange requires numerical modeling and coordinated in situ and orbital observations, which improve constraints on atmospheric processes and support robotic mission safety. We performed reflectance cross calibration between the Tianwen-1 HiRIC and Mars Reconnaissance Orbiter (MRO) HiRISE datasets to track surface changes disturbed by landing plume effects across 2 Martian yr after the Zhurong rover’s arrival. Observations show surface reflectance rapidly recovered to prelanding conditions within the first Martian year, followed by a moderate dust-cleaning event in the subsequent spring. We conclude that the site undergoes significant dust accumulation starting in late northern summer, paired with springtime dust removal driven by convective vortices. This combined pattern of dust exchange differs from records at earlier landing sites, demonstrating substantial spatial variability in modern local dust activity across Mars.

The Astronomical JournalVol. 172(6)
Sun Yat-sen University (CN), China Academy of Space Technology (CN), Chinese Academy of Sciences (CN), University of Chinese Academy of Sciences (CN), Beijing Aerospace Flight Control Center (CN), Institute of Spacecraft System Engineering (CN), University of Hong Kong (HK)
Openalex Percentile: Top 16%
Planetary Science and Exploration
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