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Record W6949850089 · doi:10.5281/zenodo.15448615

Sensitivity Study of Aerosol Direct Radiative Effects on Cloudy EarthCARE Scenes Using 1D and 3D Radiative Transfer Simulations

2025· article· en· W6949850089 on OpenAlexaffabout

Bibliographic record

VenueZenodo (CERN European Organization for Nuclear Research) · 2025
Typearticle
Languageen
FieldEnvironmental Science
TopicAtmospheric aerosols and clouds
Canadian institutionsEnvironment and Climate Change Canada
FundersEuropean Commission
KeywordsRadiative transferAerosolShortwaveAtmospheric radiative transfer codesRadiometerSatelliteRadiative fluxRadiative forcingShortwave radiation

Abstract

fetched live from OpenAlex

The upcoming EarthCARE (Earth Cloud, Aerosol and Radiation Explorer) satellite mission will provide concurrent inferences of aerosol, cloud, and precipitation properties along with radiative fluxes and heating rate profiles. This is essential information to evaluate the representation of all these variables in weather forecasting and climate models and advance our knowledge about cloud and aerosol radiative effects and feedback mechanisms (Wehr et al. 2023). EarthCARE is the first mission to make “operational” use of 3D radiative transfer (RT) models, as well as conventional 1D models. These models will simulate measurements (made and inferred) by EarthCARE’s broadband radiometer (BBR) and compare them against actual BBR measurements in order to assess the quality of aerosol and cloud retrievals derive from other instruments onboard EarthCARE. The scientific goal of the EarthCARE mission is to retrieve cloud and aerosol properties well enough that when used in 3D RT models, predicted and “observed” fluxes differ, on average, by less than ±10 W/m2. This will be a continuous radiative closure assessment of the L2 products, which will be important for both L2-algorithm developers and data users. The RT models to be used, along with their official products, are described in Cole et al. (2023). As pointed out by Cole et al. (2023), the 1D and 3D RT calculations for upwelling shortwave fluxes at 20 km can be expected to differ by more than the target scientific goal in at least 50% of the cases. The assessment of aerosol direct radiative effects on cloudy atmospheres is a difficult task as their properties, which vary with altitude, impact atmospheric RT. The objective of the present study is to use RT models to quantify these effects for 1D and 3D scenes using different vertical distributions of aerosols. The libRadtran RT package (Mayer & Kylling, 2005; Emde et al., 2016) will be used along with its MYSTIC (Mayer 2009) solver for 3D RT simulations. This sensitivity study will employ data from the Halifax, Baja, and Hawaii EarthCARE test frames (~6,200 km-long). For selected cloud scenes, artificial aerosol layers (above and below clouds) will be generated. Differences in simulated shortwave and longwave fluxes and heating rate profiles, along with top of atmosphere radiances, will be evaluated and discussed for different aerosol optical properties based on different aerosol types and their varying vertical distributions. Outcomes of this study will be useful for future radiative closure assessments of EarthCARE using ground-based measurements of aerosol and cloud profiles, thus contributing to post-launch Cal/Val activities.

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)0.002
metaresearch head score (Gemma)0.005
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 score0.069
Threshold uncertainty score0.138

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0020.005
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0010.002
Bibliometrics0.0010.001
Science and technology studies0.0010.001
Scholarly communication0.0010.001
Open science0.0020.001
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 head0.019
GPT teacher head0.250
Teacher spread0.231 · 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

Citations0
Published2025
Admission routes2
Has abstractyes

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