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Record W3016936581 · doi:10.11575/prism/37633

Aeolian Controlled Landscape Evolution at a Martian Analogue Site in Northwestern Argentina

2020· dissertation· en· W3016936581 on OpenAlexfundno aff
Elena A. Favaro

Bibliographic record

VenueOpen MIND · 2020
Typedissertation
Languageen
FieldPhysics and Astronomy
TopicPlanetary Science and Exploration
Canadian institutionsnot available
FundersKillam TrustsNatural Sciences and Engineering Research Council of CanadaDigitalGlobe Foundation
KeywordsAeolian processesMartianGeologyGeographyEarth scienceAstrobiologyPhysical geographyMars Exploration ProgramGeomorphologyPhysics

Abstract

fetched live from OpenAlex

Aeolian processes are the most pervasive agent of surficial change in the solar system. Encompassing sediment entrainment, transport, deposition, deflation, and abrasion, aeolian-driven landscape modification can affect planetary surfaces over a range of spatial and temporal scales. On Earth, aeolian processes shape the landscape across all seven continents. In our solar system, Mars is the only other planet known to have active aeolian processes. As the main geological agent of change over the past 4 billion years, wind has sculpted the Martian surface into patterns we recognize from studies of arid landscapes on Earth. Of interest to scientists is constraining the paleo- and contemporary wind regime of Mars to better understand its geologic, climatic, and erosional histories. Terrestrial aeolian research in Martian analogue environments has become an integral research practice to achieve these objectives. This thesis investigates process-form linkages between the aeolian environment and landscape on the Puna Plateau, Northwestern Argentina. A well-known Martian analogue, the Puna Plateau is ideal for conducting aeolian analogue research owing to its high altitude, low atmospheric pressure, aridity, wind regime, pyroclastic and basaltic geology, and the presence of a number of enigmatic bedrock landforms and granular bedforms known to exist on Mars, including, yardangs, periodic bedrock ridges, megaripples, and wind streaks. This research applies a diverse suite of in situ, laboratory, modelling, and remote sensing methodologies and analysis techniques to characterize sediment transport, the wind regime, abrasion dynamics, and distribution of landforms in the study area. Results from each study were used to refine and inform subsequent research questions. Among the findings of these works, we (i) identify a new abrasion feature, propose an evolutionary cycle, and highlight the diagnostic utility of this and other bedrock abraded features; (ii) identify variability of wind direction in the study area using wind re-analysis models, demonstrate the range of densities of mobilized grains using in situ sediment traps, and highlight the challenges of constraining sediment flux and abrasion rates in multimodal density environments; and (iii) use a high-resolution digital elevation model to statistically analyze yardang distribution, put forth hypotheses about initiation mechanisms, and relate the distribution of yardangs in the study area to those found elsewhere on Earth and Mars. The research in this thesis demonstrates the utility and necessity of using multiple methodologies to holistically define complex aeolian systems.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.149
Threshold uncertainty score0.295

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.017
GPT teacher head0.254
Teacher spread0.237 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2020
Admission routes1
Has abstractyes

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