MétaCan
Menu
← Back to cohort
Record W2528831201

Evaluation of a Soil Radar Backscatter Model with Applicability to Radar Observations of a sub-Arctic Environment

2013· dissertation· en· W2528831201 on OpenAlexaboutno aff
Ryan Ahola

Bibliographic record

VenueUWSpace (University of Waterloo) · 2013
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicClimate change and permafrost
Canadian institutionsnot available
Fundersnot available
KeywordsRadarBackscatter (email)Remote sensingArcticEnvironmental scienceGeographyGeologyComputer scienceOceanographyTelecommunications
DOInot available

Abstract

fetched live from OpenAlex

This research explores the applicability of a soil backscatter model for estimating X-band (9.35-9.85 GHz) backscatter from snow covered sub-Arctic terrain in the Hudson Bay Lowlands, Manitoba, Canada. The studied radar frequencies and model have been identified for potential use within Snow Water Equivalent (SWE) retrievals for future remote sensing missions. In open tundra environments, the predominant X-band response is controlled by soil frozen status, soil moisture and soil surface roughness. Snow in these environments is expected to have little influence on backscatter due to the transparent nature of shallow snowpacks at this frequency. Therefore, understanding a backscatter model's sensitivity to soil parameters is of primary concern for appropriate use under sub-Arctic terrain conditions. \n \nUsing measurements and estimates of soil complex relative permittivity as well as a series of soil surface roughness measurements, backscatter model estimates are compared with two X-band remote sensing datasets: 1) ground-based scatterometer measurements obtained by the University of Waterloo Scatterometer (UW-Scat), and 2) TerraSAR-X observations. Comparisons reveal mixed agreement between remote sensing measurements and backscatter model estimates, with average differences ranging from -0.76 to 11.43 dB. While TerraSAR-X VV measurements and in situ soil surface roughness observations contributed to the range of differences, overall agreement was typically ˜6 dB, indicating poor agreement for the majority of backscatter model, UW-Scat and TerraSAR-X comparisons. These results thus illustrate substantial challenges for application of the backscatter model within dual-frequency SWE retrieval frameworks, without proper incorporation of roughness, soil moisture and permittivity for the areas under observation. \n \nResults from this study reveal uncertainties in the applicability of the soil backscatter model for sub-Arctic terrain of the Hudson Bay Lowlands. While good agreement was observed for TerraSAR-X VV measurements, poor and varied agreement for the remaining ground and satellite-based measurements suggests the current modelling framework needs improvement for use in sub-Arctic terrain. By improving the characterization of the Hudson Bay Lowlands region, a better understanding of the nature of sub-Arctic terrain parameters required for this application can be achieved. This may also lead to improved modelling frameworks for representing sub-Arctic terrain within future satellite missions.

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)0.001
metaresearch head score (Gemma)0.001
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.055
Threshold uncertainty score0.109

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0010.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.001
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0010.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

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 head0.038
GPT teacher head0.208
Teacher spread0.170 · 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 designSimulation or modeling
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
Published2013
Admission routes1
Has abstractyes

Explore more

Same venueUWSpace (University of Waterloo)→Same topicClimate change and permafrost→French-language works237,207→