Bibliographic record
Abstract
Recent changes of glacier coverage in the western Terskey-Alatoo range, Kyrgyz Republic, using Corona and Landsat ACUN ˜A, C 111 Ice volumetric changes on active volcanoes in southern Chile AGETA, Y 344 Estimation of atmospheric transmissivity of solar radiation from precipitation in the Himalaya and the Tibetan Plateau AIZEN, EM 49 Climatic and atmospheric circulation pattern variability from ice-core isotope/geochemistry records (Altai, Tien Shan and Tibet) AIZEN, EM 202 Glacier changes in the central and northern Tien Shan during the last 140 years based on surface and remote-sensing data AIZEN, VB 49 Climatic and atmospheric circulation pattern variability from ice-core isotope/geochemistry records (Altai, Tien Shan and Tibet) AIZEN, VB 202 Glacier changes in the central and northern Tien Shan during the last 140 years based on surface and remote-sensing data AIZEN, VB 378 A snow algal community on Akkem glacier in the Russian Altai mountains AN, L 160 A study on the vertical profile of bacterial DNA structure in the Puruogangri (Tibetan Plateau) ice core using denaturing gradient gel electrophoresis ARKHIPOV, S 70 Biological ice-core analysis of Sofiyskiy glacier in the Russian Altai BELO `, M 123 Glaciological characteristics of the ablation zone of Baltoro glacier, Karakoram, Pakistan BOLIUS, D 14 A first shallow firn-core record from Glaciar La Ollada, Cerro Mercedario, central Argentine Andes BOWN, F 111 Ice volumetric changes on active volcanoes in southern Chile BRAITHWAITE, RJ 329 Accumulation at the equilibrium-line altitude of glaciers inferred from a degree-day model and tested against field observations BROCK, B 111 Ice volumetric changes on active volcanoes in southern Chile BRU ¨TSH, S 8 A potential high-elevation ice-core site at Hielo Patago ´nico Sur CAN ˜ON, M 194 Fast shrinkage of tropical glaciers in Colombia CAI, D 79 Monitoring the glacier changes in the Muztag Ata and Konggur mountains, east Pamirs, based on Chinese Glacier Inventory and recent satellite imagery CASASSA, G 8 A potential high-elevation ice-core site at Hielo Patago ´nico Sur CASASSA, G 14 A first shallow firn-core record from Glaciar La Ollada, Cerro Mercedario, central Argentine Andes CASASSA, G 111 Ice volumetric changes on active volcanoes in southern Chile CEBALLOS, JL 194 Fast shrinkage of tropical glaciers in Colombia CHEN, C 275 Response of meltwater runoff to air-temperature fluctuations on Keqikaer glacier, south slope of Tuomuer mountain, western China CHEN, F 86 A comparison of tree-ring records and glacier variations over the past 700 years, northeastern Tibetan Plateau CHEN, F 385 Glacier variations in the Naimona'nyi region, western Himalaya, in the last three decades CHUTKO, K 329 Accumulation at the equilibrium-line altitude of glaciers inferred from a degree-day model and tested against field observations CLAVERO, J 111 Ice volumetric changes on active volcanoes in southern Chile DAVIS, ME 29 Strong negative correlation between dust event frequency and air temperature over the northern Tibetan Plateau reflected by the Malan ice-core record DAVIS, ME 34 An Andean ice-core record of a Middle Holocene megadrought in North Africa and Asia DAVIS, ME 61 Holocene climate variability archived in the Puruogangri ice cap on the central Tibetan Plateau DEMUTH, MN 177 Seasonal and spatial variations of snow chemistry on Mount Logan, Yukon, Canada DING, L 79 Monitoring the glacier changes in the Muztag Ata and Konggur mountains, east Pamirs, based on Chinese Glacier Inventory and recent satellite imagery DING, Y 79 Monitoring the glacier changes in the Muztag Ata and Konggur mountains, east Pamirs, based on Chinese Glacier Inventory and recent satellite imagery DING, Y 91 Glacier retreat as a result of climate warming and increased precipitation in the Tarim river basin, northwest China DING, Y 97 The retreat of glaciers in response to recent climate warming in western China DING, Y 187 Glacier changes during the past century in the Gangrigabu mountains, southeast Qinghai-Xizang (Tibetan) Plateau, China DING, Y 275 Response of meltwater runoff to air-temperature fluctuations on Keqikaer glacier, south slope of Tuomuer mountain, western China
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 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 | 0.001 | 0.008 |
| Meta-epidemiology (narrow) | 0.001 | 0.000 |
| Meta-epidemiology (broad) | 0.001 | 0.000 |
| Bibliometrics | 0.002 | 0.003 |
| Science and technology studies | 0.001 | 0.000 |
| Scholarly communication | 0.006 | 0.003 |
| Open science | 0.002 | 0.003 |
| Research integrity | 0.001 | 0.001 |
| Insufficient payload (model declined to judge) | 0.625 | 0.589 |
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".