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Record W1607035973 · doi:10.1002/2013jd020502

An energetic perspective on hydrological cycle changes in the Geoengineering Model Intercomparison Project

2013· article· en· W1607035973 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.

Bibliographic record

VenueJournal of Geophysical Research Atmospheres · 2013
Typearticle
Languageen
FieldEnvironmental Science
TopicClimate Change and Geoengineering
Canadian institutionsEnvironment and Climate Change Canada
FundersPacific Northwest National LaboratoryEngineering and Physical Sciences Research CouncilGoddard Space Flight CenterOffice of ScienceGrand Équipement National De Calcul IntensifBeijing Normal UniversityU.S. Department of EnergyEuropean CommissionDivision of Chemical, Bioengineering, Environmental, and Transport SystemsBattelleMet OfficeFund for Innovative Climate and Energy ResearchNorges ForskningsrådMinistry of Education, Culture, Sports, Science and TechnologyDepartment for Environment, Food and Rural Affairs, UK GovernmentNational Aeronautics and Space AdministrationNational Science Foundation
KeywordsEnvironmental scienceLatent heatAtmosphere (unit)Coupled model intercomparison projectClimatologyPrecipitationSensible heatClimate modelAtmospheric sciencesFlux (metallurgy)Energy balanceClimate changeWater cycleEvaporationMean radiant temperatureMeteorologyChemistryGeographyThermodynamicsGeologyPhysics

Abstract

fetched live from OpenAlex

Abstract Analysis of surface and atmospheric energy budget responses to CO 2 and solar forcings can be used to reveal mechanisms of change in the hydrological cycle. We apply this energetic perspective to output from 11 fully coupled atmosphere‐ocean general circulation models simulating experiment G1 of the Geoengineering Model Intercomparison Project (GeoMIP), which achieves top‐of‐atmosphere energy balance between an abrupt quadrupling of CO 2 from preindustrial levels ( abrupt4xCO2 ) and uniform solar irradiance reduction. We divide the climate system response into a rapid adjustment , in which climate response is due to adjustment of the atmosphere and land surface on short time scales, and a feedback response , in which the climate response is predominantly due to feedback related to global mean temperature changes. Global mean temperature change is small in G1 , so the feedback response is also small. G1 shows a smaller magnitude of land sensible heat flux rapid adjustment than in abrupt4xCO2 and a larger magnitude of latent heat flux adjustment, indicating a greater reduction of evaporation and less land temperature increase than abrupt4xCO2 . The sum of surface flux changes in G1 is small, indicating little ocean heat uptake. Using an energetic perspective to assess precipitation changes, abrupt4xCO2 shows decreased mean evaporative moisture flux and increased moisture convergence, particularly over land. However, most changes in precipitation in G1 are in mean evaporative flux, suggesting that changes in mean circulation are small.

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.

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.001
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation 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 score0.099
Threshold uncertainty score0.385

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.001
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 head0.053
GPT teacher head0.344
Teacher spread0.291 · 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