RESEARCH OF THE GEOMORPHOLOGY SECTOR OF THE INSTITUTE OF GEOGRAPHY OF NAS OF UKRAINE IN THE FIRST QUARTER OF THE 21ST CENTURY
Bibliographic record
Abstract
The creation of the Ukrainian Academy of Sciences in 1918 marked the beginning of a more than a century-long period of systematic geomorphological research on the territory of Ukraine. In 1961, at the Institute of Geological Sciences of the Academy of Sciences of the Ukrainian SSR, the department of the latest movements of the earth’s crust began work, which was transformed over time into the department (since 2016 - the sector) of geomorphology of the Institute of Geography of the National Academy of Sciences of Ukraine. During the second half of the 20th century, the main areas of fundamental, regional and applied geomorphological and neotectonic research were formed in the Department of Geomorphology. At the end of the 20th century the introduction of geoinformation analysis and modeling methods into scientific research, which became an impetus for the modernization of existing and the creation of new effective methods for researching the relief, relief-forming deposits, the latest and modern dynamics of the near-surface part of the lithosphere. Among the main directions of research of the department of geomorphology in the first quarter of the 21st century should be mentioned the study of spatio-temporal regularities and factors of modern (including anthropogenic) geomorphogenesis, the study of the latest and modern dynamics of the near-surface part of the lithosphere, the development of methods for the detection, ranking and assessment of the neogeodynamic rating of linear morphostructures, applied engineering-geomorphological, ecological-geomorphological and prospecting-geomorphological studies, large-scale geomorphological and neotectonic mapping and geoinformation modeling. Armed Russian aggression, as a result of which large-scale transformations of the relief took place, made corrections in the directions of geomorphological studies of the sector. In the near future, applied geomorphological studies with the aim of post-war restoration of geomorphological systems will be relevant.
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How this classification was reachedexpand
Full frame machine prediction
Teacher imitationNot 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.
Distilled classifier scores by category (both heads)
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.002 | 0.002 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.002 | 0.005 |
| Science and technology studies | 0.002 | 0.001 |
| Scholarly communication | 0.004 | 0.002 |
| Open science | 0.000 | 0.002 |
| Research integrity | 0.000 | 0.001 |
| Insufficient payload (model declined to judge) | 0.003 | 0.001 |
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.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.
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".