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Record W3123568143

NASA Sees First in 2018 the Direct Proof of Ozone Hole Recovery

2018· article· en· W3123568143 on OpenAlexaboutno aff
Relly Victoria Petrescu, Raffaella Aversa, Antonio Apicella, Florian Ion Tiberiu Petrescu

Bibliographic record

VenueSSRN Electronic Journal · 2018
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicAtmospheric Ozone and Climate
Canadian institutionsnot available
Fundersnot available
KeywordsOzoneOzone layerStratosphereOzone depletionAtmosphere (unit)Atmospheric sciencesEnvironmental scienceAltitude (triangle)ChlorineAstrobiologyUltravioletMeteorologyChemistryGeologyPhysics
DOInot available

Abstract

fetched live from OpenAlex

For the first time, scientists have shown through direct observations of the ozone hole by a satellite instrument, built by NASA's Jet Propulsion Laboratory in Pasadena, California, that levels of ozone-destroying chlorine are declining, resulting in less ozone depletion. Measurements show that the decline in chlorine, resulting from an international ban on chlorine-containing human-produced chemicals called Chlorofluorocarbons (CFCs), has resulted in about 20% less ozone depletion during the Antarctic winter than there was in 2005 - the first year that measurements of chlorine and ozone during the Antarctic winter were made by NASA's Aura satellite. The ozone layer is the area of the terrestrial stratosphere, which is largely made up of ozone. This layer contains 90% of the ozone found in the atmosphere and absorbs 97-99% of high-frequency ultraviolet radiation. The ozone layer ranges from about 15 km to about 40 km altitude. Ozone is part of the gases that make up the atmosphere: It is born out of oxygen through photochemical reactions caused by solar radiation. The earth is surrounded by an ozone layer located at a very high altitude. This layer filters about two-thirds of the Ultraviolet (UV) radiation from the Sun. If all the rays reach Earth, it would be damaging to life on the planet. The ozone layer is located in the stratosphere, but the most concentrated is 20-25 km. Basically, it is ozone and not pure ozone air, with a larger number of ozone molecules in the composition than the usual air (containing mainly nitrogen and oxygen). In the ozone layer there is a continuous transformation between different forms of oxygen. The usual oxygen molecules, O2, split into oxygen atoms, O. They merge with the oxygen molecules forming ozone, O3. Over time, ozone decomposes into normal oxygen O2 and single oxygen atoms, O. Over the past 40 years, industrial production using many chlorine-containing chemicals such as chlorofluorocarbons (CFCs) in sprays, refrigerants and solvents used in the electronics industry has increased. These substances have been banned under the Montreal Protocol. In September 2014, the United Nations and the World Meteorological Organization published a report on the evolution of the ozone layer, arguing that it could be rebuilt by the middle of the century as a result of the measures adopted by the Montreal Protocol. According to the report, the ozone layer has declined globally in the 1980s and early 1990s, has remained relatively unchanged since 2000 and could revert to the 1980s before 2050.

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)0.004
metaresearch head score (Gemma)0.009
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: none
GenreCandidate signal: Empirical · Consensus signal: none
Teacher disagreement score0.072
Threshold uncertainty score0.242

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0040.009
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0010.001
Bibliometrics0.0010.000
Science and technology studies0.0020.001
Scholarly communication0.0040.004
Open science0.0010.004
Research integrity0.0040.005
Insufficient payload (model declined to judge)0.0720.025

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 head0.007
GPT teacher head0.203
Teacher spread0.195 · 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

Citations2
Published2018
Admission routes1
Has abstractyes

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