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Record W1538710699 · doi:10.1002/2013jd021110

Forcings and feedbacks in the GeoMIP ensemble for a reduction in solar irradiance and increase in CO<sub>2</sub>

2014· article· en· W1538710699 on OpenAlexaff
Nicolás Huneeus, Oliviér Boucher, Kari Alterskjær, Jason N. S. Cole, Charles L. Curry, Duoying Ji, Andy Jones, Ben Kravitz, Jón Egill Kristjánsson, John C. Moore, Helene Muri, Ulrike Niemeier, Phil Rasch, Alan Robock, Balwinder Singh, Hauke Schmidt, Michael Schulz, Simone Tilmes, Shingo Watanabe, Jin‐Ho Yoon

Bibliographic record

VenueJournal of Geophysical Research Atmospheres · 2014
Typearticle
Languageen
FieldEnvironmental Science
TopicClimate Change and Geoengineering
Canadian institutionsUniversity of VictoriaEnvironment and Climate Change Canada
FundersPacific Northwest National LaboratoryGoddard Space Flight CenterOffice of ScienceGrand Équipement National De Calcul IntensifU.S. Department of EnergyEuropean CommissionMet OfficeFund for Innovative Climate and Energy ResearchDivision of Chemical, Bioengineering, Environmental, and Transport SystemsBattelleNorges ForskningsrådDepartment for Environment, Food and Rural Affairs, UK GovernmentNational Aeronautics and Space AdministrationMinistère de l'Écologie, du Développement Durable et de l'ÉnergieNational Center for Atmospheric ResearchNational Science Foundation
KeywordsShortwaveEnvironmental scienceCloud forcingRadiative forcingForcing (mathematics)IrradianceSolar irradianceAtmospheric sciencesLongwaveContext (archaeology)Energy budgetRadiative transferShortwave radiationCloud coverClimatologyClimate modelClimate changeMeteorologyCloud computingPhysicsRadiationGeographyComputer science

Abstract

fetched live from OpenAlex

Abstract The effective radiative forcings (including rapid adjustments) and feedbacks associated with an instantaneous quadrupling of the preindustrial CO2 concentration and a counterbalancing reduction of the solar constant are investigated in the context of the Geoengineering Model Intercomparison Project (GeoMIP). The forcing and feedback parameters of the net energy flux, as well as its different components at the top‐of‐atmosphere (TOA) and surface, were examined in 10 Earth System Models to better understand the impact of solar radiation management on the energy budget. In spite of their very different nature, the feedback parameter and its components at the TOA and surface are almost identical for the two forcing mechanisms, not only in the global mean but also in their geographical distributions. This conclusion holds for each of the individual models despite intermodel differences in how feedbacks affect the energy budget. This indicates that the climate sensitivity parameter is independent of the forcing (when measured as an effective radiative forcing). We also show the existence of a large contribution of the cloudy‐sky component to the shortwave effective radiative forcing at the TOA suggesting rapid cloud adjustments to a change in solar irradiance. In addition, the models present significant diversity in the spatial distribution of the shortwave feedback parameter in cloudy regions, indicating persistent uncertainties in cloud feedback mechanisms.

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)0.001
metaresearch head score (Gemma)0.002
Version: metacan-v3-hybrid-931329e0061cValidation 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 score0.040
Threshold uncertainty score0.079

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0010.002
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0010.001
Bibliometrics0.0000.001
Science and technology studies0.0010.001
Scholarly communication0.0010.001
Open science0.0010.001
Research integrity0.0020.001
Insufficient payload (model declined to judge)0.0010.000

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 head0.025
GPT teacher head0.290
Teacher spread0.266 · 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 designSimulation or modeling
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

Citations23
Published2014
Admission routes1
Has abstractyes

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