Atmospheric protection and climate change
Bibliographic record
Abstract
INTRODUCTION The protection of the atmosphere was a relative latecomer to international environmental regulation but is now well established. With limited exceptions, until 1979 no treaty sought, as its primary purpose, to place limits on the right of states to allow atmospheric emissions that caused environmental damage. Some treaties had, however, called for general preventive strategies. Since 1979, numerous treaties and other international acts have addressed the protection of the atmosphere. Although there is no atmospheric equivalent to the 1982 UN Convention on the Law of the Sea, international legal instruments have been adopted at the regional and global level which address a range of issues, including: transboundary pollution by sulphur dioxide, nitrogen oxide, volatile organic compounds, heavy metals and persistent organic pollutants (POPs); the protection of the ozone layer; the prevention of climate change; and the protection of the environment of outer space. The precedents set by treaties relating to the protection of other environmental media, in particular the marine environment, have contributed to the development of these rules. Landmarks in the development of international law in this area include: the 1938 and 1941 decisions in the Trail Smelter case; the applications brought to the ICJ by Australia and New Zealand against France with respect to French atmospheric nuclear tests in the Pacific Ocean region; growing evidence in Europe and North America in the 1970s of acid rain damage from atmospheric emissions of sulphur compounds; the 1986 Chernobyl accident; growing evidence in the 1980s of depletion of the ozone layer; greater awareness of the threats posed by forest fires with transnational effects, such as those in Indonesia in 1997 which caused widespread regional problems, and, mostly recently, consolidation of scientific evidence that increased atmospheric concentrations of carbon dioxide and other greenhouse gases are likely to cause temperatures to increase worldwide with consequential adverse effects.
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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 | 0.000 | 0.001 |
| Meta-epidemiology (narrow) | 0.001 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.001 | 0.001 |
| Science and technology studies | 0.001 | 0.002 |
| Scholarly communication | 0.002 | 0.002 |
| Open science | 0.001 | 0.001 |
| Research integrity | 0.002 | 0.003 |
| Insufficient payload (model declined to judge) | 0.022 | 0.005 |
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".