Member Since 2012
Mackenzie D. Day
Assistant Professor, University of California Los Angeles
Professional Experience
University of California Los Angeles
Assistant Professor
2018 - Present
Education
University of Texas at Austin
Doctorate
2017
Honors & Awards
Ronald Greeley Early Career Award in Planetary Sciences
Received December 2022
Citation
Mackenzie Day received her B.S. from the California Institute of Technology in 2012 and her Ph.D. from the University of Texas at Austin in 2017. Mackenzie is now an assistant professor at the University of California, Los Angeles, and she is a leader at interpreting modern and ancient planetary surface systems affected by windblown sediment. Her scientific advances are built on a deep understanding of aeolian processes that is creatively applied to estimate environmental properties encoded in landforms and sedimentary deposits. Mackenzie’s careful work has demonstrated that the structure of simple dune fields and their constituent dunes are truly reflections of their formative wind regimes and sediment supplies. This has provided foundational support for Earth analogue studies and confirmed that surface conditions on planetary bodies can be accurately estimated using appropriate morphodynamic frameworks. Focusing on craters as a primary source and sink for dune sediment, her research group defined the critical crater wall slope connected to whether sediment eroded from intracrater deposits can be transported out of a crater basin and thereby be transferred to the regional sediment budget. Mackenzie’s expertise in modern aeolian systems has also benefited mission operations, including how different types of windblown deposits affect rover trafficability and identification of sites of active bedrock erosion that likely make optimal sampling locations for ancient Martian biosignatures. Mackenzie has also made significant contributions to our understanding of the early Martian environment via innovative stratigraphic analyses. These studies have helped define ancient wind fields and properties of the wet-to-dry Mars transition preserved in fluviolacustrine to aeolian sedimentary successions. Evaluating limitations in the spatial resolution of Mars imaging has allowed Mackenzie to demonstrate that many layered deposits are likely aeolianites. Working across scales, Mackenzie has contributed to a better definition of subthreshold grain saltation at particle dimensions, and a better definition of erosive, rim-generated vortices at the crater scale. Sediment transported by these vortices is commonly worked into dunes that interact with each other as they migrate and grow. Mackenzie has made fundamental contributions to understanding these dune interactions, as well as the sedimentary structures they generate. Following Ronald Greeley, Mackenzie’s considerable scientific contributions are matched by her professional services that include the training and mentoring of junior planetary scientists. Mackenzie Day has earned the Ronald Greeley Early Career Award for “innovative application of theory, field and remotely sensed data to the erosion and deposition of planetary landforms by windblown sediment.” —David Mohrig, University of Texas at Austin
Response
I feel truly honored to receive the Ronald Greeley Early Career Award in Planetary Sciences. I never had the privilege of meeting Ron Greeley during his lifetime, but I have certainly learned from him through his work. His contributions to aeolian geology in particular have been at the foundation of much of my research, and I hope my career will reflect his legacy of research and mentorship. I want to thank the many people who have mentored and supported me over the years, from John Grotzinger, who gave me my first research job as an undergraduate, to David Catling, who gave me the flexibility to explore new ideas as a postdoc. I am grateful for the community of mentors and colleagues I had during my time in Texas, including David Mohrig, Ryan Ewing, and Tim Goudge, and for the wonderful colleagues who welcomed me to my new department at University of California, Los Angeles. I am especially grateful for the support of my graduate adviser, Gary Kocurek, whose patient mentorship and guidance taught me not only how to see the puzzle in the landscape but also how to solve it. I also want to thank my students and collaborators. Their effort has contributed immensely to my career and cannot be understated. I have been incredibly fortunate to be supported and welcomed by so many people, and I hope to honor that support and Ron Greeley’s legacy by paying it forward as a supportive mentor myself. —Mackenzie Day, University of California, Los Angeles
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Current Roles
Member
Fall Meeting Program Committee
Publications
Orbital and In‐Situ Investigation of Periodic Bedrock Ridges in Glen Torridon, Gale Crater, Mars

Gale crater, the field site for NASA's Mars Science Laboratory Curiosity rover, contains a diverse and extensive record of aeolian deposition and e...

May 26, 2022
AGU Abstracts
Global Analysis of Dune Patterns on Titan
SURFACE PROCESSES ACROSS THE SOLAR SYSTEM I POSTER
earth and planetary surface processes | 13 december 2023
Colin Marvin, Wen Bo, Jani Radebaugh, Andrew Gunn,...
Fields of linear dunes dominate Titans equatorial region. Because dunes evolve in concert with the winds, the patterns they form are tied to the dune ...
View Abstract
Hydrodynamic and Sediment-Transport Controls on the Size of Eolian Dunes Across Planetary Surfaces
GRANULAR AND FLUID PHYSICS ON EARTH AND OTHER PLANETARY BODIES III ORAL
earth and planetary surface processes | 12 december 2023
Mathieu G. Lapotre, Philippe Claudin, Andrew Gunn,...
Despite vast variations in fluid and sediment properties, fields of windblown dunes have been identified well beyond Earth, including on Venus, Mars, ...
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Numerical Modeling of Recurring Slope Lineae and Slope Streak Formation through Dry Grainflow Mechanisms on Mars
GRANULAR AND FLUID PHYSICS ON EARTH AND OTHER PLANETARY BODIES I POSTER
earth and planetary surface processes | 12 december 2023
Stephanie Jarmak, David E. Stillman, Mackenzie D. ...
Recurring Slope Lineae (RSL), seasonally varying low-albedo streaks on steep slopes, remain some of the most poorly understood surface features on Mar...
View Abstract

Volunteer Experience
2024 - Present
Member
Fall Meeting Program Committee
2021 - 2022
Member
Fall Meeting Program Committee
2021 - 2022
Member
Earth and Planetary Surface Processes Fall Meeting Program Committee
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