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Record W2142345352 · doi:10.1029/2003ja009881

Ring current intensification and convection‐driven negative bays: Multisatellite studies

2003· article· en· W2142345352 on OpenAlexaff
X. Zhou, B. T. Tsurutani, G. D. Reeves, G. Rostoker, W. Sun, J. M. Ruohoniemi, Y. Kamide, A. T. Y. Lui, G. K. Parks, W. D. González, J. K. Arballo

Bibliographic record

VenueJournal of Geophysical Research Atmospheres · 2003
Typearticle
Languageen
FieldPhysics and Astronomy
TopicIonosphere and magnetosphere dynamics
Canadian institutionsUniversity of Alberta
Fundersnot available
KeywordsSubstormRing currentSolar windInterplanetary magnetic fieldGeophysicsMagnetosphereGeomagnetic stormInterplanetary spaceflightPhysicsGeosynchronous orbitPolarStormConvectionGeologyAtmospheric sciencesSatelliteMeteorologyMagnetic fieldAstronomy

Abstract

fetched live from OpenAlex

The original view on the cause of ring current intensifications was a frequent occurrence of intense substorm expansion phases. Results from many studies have supported this view. However, whether this is the only mechanism of ring current buildup has been a controversy. Kamide [1992] asserted that ring current intensification is due to “sustained, southward IMF, not because of frequent occurrence of intense substorms.” Lui et al. [2001] have shown that the ring current can be intensified during enhanced convection without substorm occurrence. Tsurutani et al. [2003] have found that there was a lack of substorm expansion phases for long periods of time (up to 7 hours) in 5 out of 11 storm main phases (in 1997) that were induced by the smoothly varying Bz component of the interplanetary magnetic field (IMF) within interplanetary magnetic clouds. In this paper, a relatively weak magnetic storm event (with minimum SYM‐H at −47 nT) that occurred on 15 July 1997 is studied using ground‐based magnetograms, polar cap potentials from Super Dual Auroral Radar Network, and Los Alamos National Laboratory (LANL) geosynchronous energetic particle data as well as the Polar UV imaging (for aurorae) and Wind (for the solar wind) data. It is shown that during the storm main phase, there was a lack of substorm expansion phase activity (from imaging and the ground‐based data) and a lack of energetic particle injections at the geostationary orbit. The most prominent auroral forms were north‐south aligned auroral patches and torches. Dawn and dusk aurorae were more intense than the aurorae near midnight, where auroral gaps occurred. In addition, this paper shows that there was a significant directly driven activity during the storm main phase when the IMF was continually southward. We argue that during this event the ring current intensification was more strongly associated with enhanced magnetospheric convection than with impulsive energy unloading. Three scenarios are suggested to explain the relatively low intensity of the magnetic storm induced by a magnetic cloud. They are (1) weak nightside auroral zone ionospheric ion outflows (due to lack of substorms), (2) choked penetration of the tail plasma flow (due to lack of substorms), and (3) retarded magnetospheric convection (due to reduced solar wind‐magnetosphere reconnection). The observed saturation of the polar cap potential drop is in support of this latter mechanism.

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)0.001
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: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.004
Threshold uncertainty score0.008

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0010.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.001
Research integrity0.0000.000
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 head0.053
GPT teacher head0.359
Teacher spread0.306 · 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

Citations11
Published2003
Admission routes1
Has abstractyes

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